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  • The Olympic Mountains is a mountain range on the Olympic Peninsula of western Washington in the United States. The mountains, part of the Pacific Coast Ranges, are not especially high - Mount Olympus is the highest at 7,962 ft (2,427 m) - but the western slopes of the Olympics rise directly out of the Pacific Ocean and are the wettest place in the 48 contiguous states. On the wetter end of the spectrum, 140 and 170 inches (3,600 and 4,300 mm) of rain falls on the Hoh Rainforest annually. Conversely, areas to the northeast of the mountains are located in a rain shadow and receive as little as 16 in (410 mm) of precipitation. Most of the mountains are protected within the bounds of the Olympic National Park. Physiographically, they are a section of the larger Pacific Border province, which is in turn a part of the larger Pacific Mountain System.
    MtOlympusWinterPan.jpg
  • The Olympic Mountains is a mountain range on the Olympic Peninsula of western Washington in the United States. The mountains, part of the Pacific Coast Ranges, are not especially high - Mount Olympus is the highest at 7,962 ft (2,427 m) - but the western slopes of the Olympics rise directly out of the Pacific Ocean and are the wettest place in the 48 contiguous states. On the wetter end of the spectrum, 140 and 170 inches (3,600 and 4,300 mm) of rain falls on the Hoh Rainforest annually. Conversely, areas to the northeast of the mountains are located in a rain shadow and receive as little as 16 in (410 mm) of precipitation. Most of the mountains are protected within the bounds of the Olympic National Park. Physiographically, they are a section of the larger Pacific Border province, which is in turn a part of the larger Pacific Mountain System.
    MtOlympusWinter3.jpg
  • The Olympic Mountains is a mountain range on the Olympic Peninsula of western Washington in the United States. The mountains, part of the Pacific Coast Ranges, are not especially high - Mount Olympus is the highest at 7,962 ft (2,427 m) - but the western slopes of the Olympics rise directly out of the Pacific Ocean and are the wettest place in the 48 contiguous states. On the wetter end of the spectrum, 140 and 170 inches (3,600 and 4,300 mm) of rain falls on the Hoh Rainforest annually. Conversely, areas to the northeast of the mountains are located in a rain shadow and receive as little as 16 in (410 mm) of precipitation. Most of the mountains are protected within the bounds of the Olympic National Park. Physiographically, they are a section of the larger Pacific Border province, which is in turn a part of the larger Pacific Mountain System.
    MtOlympusWinter3.jpg
  • The Olympic Mountains is a mountain range on the Olympic Peninsula of western Washington in the United States. The mountains, part of the Pacific Coast Ranges, are not especially high - Mount Olympus is the highest at 7,962 ft (2,427 m) - but the western slopes of the Olympics rise directly out of the Pacific Ocean and are the wettest place in the 48 contiguous states. On the wetter end of the spectrum, 140 and 170 inches (3,600 and 4,300 mm) of rain falls on the Hoh Rainforest annually. Conversely, areas to the northeast of the mountains are located in a rain shadow and receive as little as 16 in (410 mm) of precipitation. Most of the mountains are protected within the bounds of the Olympic National Park. Physiographically, they are a section of the larger Pacific Border province, which is in turn a part of the larger Pacific Mountain System.
    MtOlympusWinter3.jpg
  • The Olympic Mountains is a mountain range on the Olympic Peninsula of western Washington in the United States. The mountains, part of the Pacific Coast Ranges, are not especially high - Mount Olympus is the highest at 7,962 ft (2,427 m) - but the western slopes of the Olympics rise directly out of the Pacific Ocean and are the wettest place in the 48 contiguous states. On the wetter end of the spectrum, 140 and 170 inches (3,600 and 4,300 mm) of rain falls on the Hoh Rainforest annually. Conversely, areas to the northeast of the mountains are located in a rain shadow and receive as little as 16 in (410 mm) of precipitation. Most of the mountains are protected within the bounds of the Olympic National Park. Physiographically, they are a section of the larger Pacific Border province, which is in turn a part of the larger Pacific Mountain System.
    MtOlympusWinter3.jpg
  • The Olympic Mountains is a mountain range on the Olympic Peninsula of western Washington in the United States. The mountains, part of the Pacific Coast Ranges, are not especially high - Mount Olympus is the highest at 7,962 ft (2,427 m) - but the western slopes of the Olympics rise directly out of the Pacific Ocean and are the wettest place in the 48 contiguous states. On the wetter end of the spectrum, 140 and 170 inches (3,600 and 4,300 mm) of rain falls on the Hoh Rainforest annually. Conversely, areas to the northeast of the mountains are located in a rain shadow and receive as little as 16 in (410 mm) of precipitation. Most of the mountains are protected within the bounds of the Olympic National Park. Physiographically, they are a section of the larger Pacific Border province, which is in turn a part of the larger Pacific Mountain System.
    MtOlympusWinter1.jpg
  • Horn on western saddle
    SaddleHorn1.jpg
  • Detail on western saddle
    SaddleDetail1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    HillCountry2019-2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityMeadow2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityCreek1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop6.jpg
  • Longhorn cattle among bluebonnets in the Texas Hill Country. The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    LlanoLonghorn3.jpg
  • Natural Bridge in Yoho National Park, British Columbia, Canada. <br />
<br />
Yoho National Park is located in the Canadian Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia. Yoho NP is bordered by Kootenay National Park on the southern side and Banff National Park on the eastern side in Alberta. The name Yoho comes from the Cree word for awe and wonder.<br />
<br />
Yoho covers 1,313 km2 (507 mi2) and it is the smallest of the four contiguous national parks. Yoho, together with Jasper, Kootenay and Banff National Parks, along with three British Columbia provincial parks—Hamber Provincial Park, Mount Assiniboine Provincial Park, and Mount Robson Provincial Park—form the Canadian Rocky Mountain Parks World Heritage Site. The park's administrative and visitor centre are located in the town of Field, British Columbia, beside the Trans-Canada Highway.
    NaturalBridge3.jpg
  • The Stuart Range is a mountain range in central Washington, USA. The range lies within the eastern extent of the Cascade Range immediately southwest of Leavenworth and runs east-west. The western peaks make up a single sharp ridge. The eastern half of the range splits into two parallel ridges, the northern of which is known as the Enchantment Peaks. Between these ridges lies the Enchantment Basin, which holds the dozens of tarns known as the Enchantment Lakes. Collectively, the basin and the encircling eastern peaks of the Stuart Range make up The Enchantments, a well-known backpacking destination. The south face of the Stuart Range falls off steeply to Ingalls Creek, beyond which rise the roughly parallel Wenatchee Mountains
    EnchantmentsAnnapurna1.jpg
  • Longhorn cattle among bluebonnets in the Texas Hill Country. The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    LlanoLonghorn5.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop3.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop1.jpg
  • Longhorn cattle among bluebonnets in the Texas Hill Country. The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    LlanoLonghorn4.jpg
  • Longhorn cattle among bluebonnets in the Texas Hill Country. The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    LlanoLonghorn3.jpg
  • Longhorn cattle among bluebonnets in the Texas Hill Country. The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    LlanoLonghorn2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    HillCountry2019-4.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop5.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop3.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop1.jpg
  • Longhorn cattle among bluebonnets in the Texas Hill Country. The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    LlanoLonghorn4.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    HillCountry2019-4.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    _Y6A8814.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    _Y6A8810.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    HillCountry2019-3.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityMeadow2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    _Y6A8712-HDR.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityCreek2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop3.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence3.jpg
  • Bow Lake is a small lake in western Alberta, Canada. It is located on the Bow River, in the Canadian Rockies, at an altitude of 1920 m. The lake lies south of the Bow Summit, east of the Waputik Range (views including Wapta Icefield, Bow Glacier, Bow Peak, Mount Thompson, Crowfoot Glacier and Crowfoot Mountain) and west of the Dolomite Pass, Dolomite Peak and Cirque Peak.<br />
<br />
Bow Lake is one of the lakes that line the Icefields Parkway in Banff National Park and Jasper National Park, other such lakes being Hector Lake, Lake Louise, Peyto Lake, Mistaya Lake, Waterfowl Lakes, Chephren Lake and Sunwapta Lake.[1]<br />
<br />
Historical Simpson's Num-Ti-Jah Lodge is located on the shores of Bow Lake[2]<br />
<br />
Bow Lake is the closest lake to the headwaters of Bow River, and has a total area of 3.21 km². Water in the lake is meltwater of the Bow Glacier.
    BowLake1.jpg
  • Natural Bridge in Yoho National Park, British Columbia, Canada. <br />
<br />
Yoho National Park is located in the Canadian Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia. Yoho NP is bordered by Kootenay National Park on the southern side and Banff National Park on the eastern side in Alberta. The name Yoho comes from the Cree word for awe and wonder.<br />
<br />
Yoho covers 1,313 km2 (507 mi2) and it is the smallest of the four contiguous national parks. Yoho, together with Jasper, Kootenay and Banff National Parks, along with three British Columbia provincial parks—Hamber Provincial Park, Mount Assiniboine Provincial Park, and Mount Robson Provincial Park—form the Canadian Rocky Mountain Parks World Heritage Site. The park's administrative and visitor centre are located in the town of Field, British Columbia, beside the Trans-Canada Highway.
    NaturalBridge2.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
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The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
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The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassFalls1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierDivideCreek1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop6.jpg
  • Carpet of lupines on 1st Burroughs Mountain in Mount Rainier National Park in Western Washington, USA<br />
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Mount Rainier National Park is a United States National Park located in southeast Pierce County and northeast Lewis County in Washington state. It was established on March 2, 1899 as the fifth national park in the United States. The park encompasses 236,381 acres including all of Mount Rainier, a 14,411-foot stratovolcano. The mountain rises abruptly from the surrounding land with elevations in the park ranging from 1,600 feet to over 14,000 feet. The highest point in the Cascade Range, around it are valleys, waterfalls, subalpine meadows, old-growth forest and more than 25 glaciers. The volcano is often shrouded in clouds that dump enormous amounts of rain and snow on the peak every year and hide it from the crowds that head to the park on weekends.<br />
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Mount Rainier is circled by the Wonderland Trail and is covered by several glaciers and snowfields totaling some 35 square miles. Carbon Glacier is the largest glacier by volume in the contiguous United States, while Emmons Glacier is the largest glacier by area. About 1.8 million people visit Mount Rainier National Park each year. Mount Rainier is a popular peak for mountaineering with some 10,000 attempts per year with approximately 50% making it to the summit.
    MountRainierSunrise1stBurrough2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop5.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    BluebonnetCow1.jpg
  • Carpet of lupines on 1st Burroughs Mountain in Mount Rainier National Park in Western Washington, USA
    MountRainierSunrise1stBurrough2.jpg
  • Carpet of lupines on 1st Burroughs Mountain in Mount Rainier National Park in Western Washington, USA<br />
.....<br />
Mount Rainier National Park is a United States National Park located in southeast Pierce County and northeast Lewis County in Washington state. It was established on March 2, 1899 as the fifth national park in the United States. The park encompasses 236,381 acres including all of Mount Rainier, a 14,411-foot stratovolcano. The mountain rises abruptly from the surrounding land with elevations in the park ranging from 1,600 feet to over 14,000 feet. The highest point in the Cascade Range, around it are valleys, waterfalls, subalpine meadows, old-growth forest and more than 25 glaciers. The volcano is often shrouded in clouds that dump enormous amounts of rain and snow on the peak every year and hide it from the crowds that head to the park on weekends.<br />
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Mount Rainier is circled by the Wonderland Trail and is covered by several glaciers and snowfields totaling some 35 square miles. Carbon Glacier is the largest glacier by volume in the contiguous United States, while Emmons Glacier is the largest glacier by area. About 1.8 million people visit Mount Rainier National Park each year. Mount Rainier is a popular peak for mountaineering with some 10,000 attempts per year with approximately 50% making it to the summit.
    MountRainierSunriseMeadow1.jpg
  • The Stuart Range is a mountain range in central Washington, USA. The range lies within the eastern extent of the Cascade Range immediately southwest of Leavenworth and runs east-west. The western peaks make up a single sharp ridge. The eastern half of the range splits into two parallel ridges, the northern of which is known as the Enchantment Peaks. Between these ridges lies the Enchantment Basin, which holds the dozens of tarns known as the Enchantment Lakes. Collectively, the basin and the encircling eastern peaks of the Stuart Range make up The Enchantments, a well-known backpacking destination. The south face of the Stuart Range falls off steeply to Ingalls Creek, beyond which rise the roughly parallel Wenatchee Mountains
    EnchantmentsAnnapurna1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop5.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop6.jpg
  • Longhorn cattle among bluebonnets in the Texas Hill Country. The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    LlanoLonghorn1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence3.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    _Y6A8714-HDR.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    BluebonnetCow1.jpg
  • Longhorn cattle among bluebonnets in the Texas Hill Country. The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    LlanoLonghorn2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    HillCountry2019-5.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    _Y6A8854-Edit-2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    _Y6A8809.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    HillCountry2019-2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence1-2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityMeadow1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityCreek1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    HillCountry2019-1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop5.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop6.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassFalls1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierDivideCreek1.jpg
  • Emerald Lake in Yoho National Park, British Columbia, Canada. <br />
<br />
Yoho National Park is located in the Canadian Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia. Yoho NP is bordered by Kootenay National Park on the southern side and Banff National Park on the eastern side in Alberta. The name Yoho comes from the Cree word for awe and wonder.<br />
<br />
Yoho covers 1,313 km2 (507 mi2) and it is the smallest of the four contiguous national parks. Yoho, together with Jasper, Kootenay and Banff National Parks, along with three British Columbia provincial parks—Hamber Provincial Park, Mount Assiniboine Provincial Park, and Mount Robson Provincial Park—form the Canadian Rocky Mountain Parks World Heritage Site. The park's administrative and visitor centre are located in the town of Field, British Columbia, beside the Trans-Canada Highway.
    EmeraldLake1.jpg
  • Natural Bridge in Yoho National Park, British Columbia, Canada. <br />
<br />
Yoho National Park is located in the Canadian Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia. Yoho NP is bordered by Kootenay National Park on the southern side and Banff National Park on the eastern side in Alberta. The name Yoho comes from the Cree word for awe and wonder.<br />
<br />
Yoho covers 1,313 km2 (507 mi2) and it is the smallest of the four contiguous national parks. Yoho, together with Jasper, Kootenay and Banff National Parks, along with three British Columbia provincial parks—Hamber Provincial Park, Mount Assiniboine Provincial Park, and Mount Robson Provincial Park—form the Canadian Rocky Mountain Parks World Heritage Site. The park's administrative and visitor centre are located in the town of Field, British Columbia, beside the Trans-Canada Highway.
    NaturalBridge1.jpg
  • The rowans or mountain-ashes are shrubs or trees in the genus Sorbus of the rose family, Rosaceae. They are native throughout the cool temperate regions of the Northern Hemisphere, with the highest species diversity in the mountains of western China and the Himalaya, where numerous apomictic microspecies occur. The name rowan was originally applied to the species Sorbus aucuparia and is also used for other species in Sorbus subgenus Sorbus.<br />
<br />
Formerly, when a wider variety of fruits were commonly eaten in Europe and North America, Sorbus was a domestically used fruit throughout these regions. It is still used in some countries, but Sorbus domestica, for example, is now all but extinct in Britain, where it was traditionally revered. Natural hybrids, often including Sorbus aucuparia and the whitebeam, Sorbus aria, give rise to many endemic variants in the UK.
    LakeLouiseRowan1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassFalls1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop3.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    HillCountry2019-5.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    HillCountry2019-3.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    HillCountry2019-1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    _Y6A8712-HDR.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityMeadow1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityCreek2.jpg
  • Longhorn cattle among bluebonnets in the Texas Hill Country. The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    LlanoLonghorn1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    _Y6A8714-HDR.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop2.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassFalls1.jpg
  • Carpet of lupines on 1st Burroughs Mountain in Mount Rainier National Park in Western Washington, USA<br />
.....<br />
Mount Rainier National Park is a United States National Park located in southeast Pierce County and northeast Lewis County in Washington state. It was established on March 2, 1899 as the fifth national park in the United States. The park encompasses 236,381 acres including all of Mount Rainier, a 14,411-foot stratovolcano. The mountain rises abruptly from the surrounding land with elevations in the park ranging from 1,600 feet to over 14,000 feet. The highest point in the Cascade Range, around it are valleys, waterfalls, subalpine meadows, old-growth forest and more than 25 glaciers. The volcano is often shrouded in clouds that dump enormous amounts of rain and snow on the peak every year and hide it from the crowds that head to the park on weekends.<br />
<br />
Mount Rainier is circled by the Wonderland Trail and is covered by several glaciers and snowfields totaling some 35 square miles. Carbon Glacier is the largest glacier by volume in the contiguous United States, while Emmons Glacier is the largest glacier by area. About 1.8 million people visit Mount Rainier National Park each year. Mount Rainier is a popular peak for mountaineering with some 10,000 attempts per year with approximately 50% making it to the summit.
    MountRainierSunrise1stBurrough2-2.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassFalls1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassFalls1.jpg
  • Carpet of lupines on 1st Burroughs Mountain in Mount Rainier National Park in Western Washington, USA<br />
.....<br />
Mount Rainier National Park is a United States National Park located in southeast Pierce County and northeast Lewis County in Washington state. It was established on March 2, 1899 as the fifth national park in the United States. The park encompasses 236,381 acres including all of Mount Rainier, a 14,411-foot stratovolcano. The mountain rises abruptly from the surrounding land with elevations in the park ranging from 1,600 feet to over 14,000 feet. The highest point in the Cascade Range, around it are valleys, waterfalls, subalpine meadows, old-growth forest and more than 25 glaciers. The volcano is often shrouded in clouds that dump enormous amounts of rain and snow on the peak every year and hide it from the crowds that head to the park on weekends.<br />
<br />
Mount Rainier is circled by the Wonderland Trail and is covered by several glaciers and snowfields totaling some 35 square miles. Carbon Glacier is the largest glacier by volume in the contiguous United States, while Emmons Glacier is the largest glacier by area. About 1.8 million people visit Mount Rainier National Park each year. Mount Rainier is a popular peak for mountaineering with some 10,000 attempts per year with approximately 50% making it to the summit.
    MountRainierSunriseMeadow1.jpg
  • Emerald Lake in Yoho National Park, British Columbia, Canada. <br />
<br />
Yoho National Park is located in the Canadian Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia. Yoho NP is bordered by Kootenay National Park on the southern side and Banff National Park on the eastern side in Alberta. The name Yoho comes from the Cree word for awe and wonder.<br />
<br />
Yoho covers 1,313 km2 (507 mi2) and it is the smallest of the four contiguous national parks. Yoho, together with Jasper, Kootenay and Banff National Parks, along with three British Columbia provincial parks—Hamber Provincial Park, Mount Assiniboine Provincial Park, and Mount Robson Provincial Park—form the Canadian Rocky Mountain Parks World Heritage Site. The park's administrative and visitor centre are located in the town of Field, British Columbia, beside the Trans-Canada Highway.
    EmeraldLake1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassFalls1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierDivideCreek1.jpg
  • Wichita Mountains Wildlife Refuge, located in southwestern Oklahoma near Lawton, has protected unique wildlife habitats since 1901 and is the oldest managed wildlife facility in the United States Fish and Wildlife Service system. Measuring about 59,020 acres (238.8 km2), the Refuge hosts a great diversity of species: 806 plant species, 240 species of birds, 36 fish, and 64 reptiles and amphibians are present. The refuge's location in the geologically unique Wichita Mountains and its areas of undisturbed mixed grass prairie make it an important conservation area. The Wichitas are approximately 500 million years old.
    WichitaBison9.jpg
  • Gnome Tarn and Prusik Peak in the Enchantment Lakes area of Alpine Lakes Wilderness, Washington
    EnchantmentsPrussikSunset2.jpg
  • Sunrise at Gnome Tarn in the Enchantments Lakes wilderness
    EnchantmentsGnomeTarnPink4.jpg
  • Sunrise at Gnome Tarn in the Enchantments Lakes wilderness
    EnchantmentsGnomeTarnPink6.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    WaveColorfulStripes2.jpg
  • Sunrise at Gnome Tarn in the Enchantments Lakes wilderness
    EnchantmentsGnomeTarnPink3.jpg
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