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  • Bamboo forest along the Pipiwai trail to Waimoku Fall in the Kipahulu area of Haleakala National Park in Maui, Hawaii<br />
.....<br />
Haleakalā National Park was established as a separate unit of the National Park System in 1960 (it was previously joined with Hawaiʻi National Park on Hawaiʻi Island). At the time, the park only consisted of the crater area of Haleakalā. On March 26, 1951, Kīpahulu Valley was added to Haleakalā National Park (HNP) as the Kīpahulu Biological Reserve to insure protection of endangered ecosystems within the sanctuary. Eighteen years later on January 10, 1969, the HNP boundaries were expanded to include the Kīpahulu coastal area of ʻOheʻo. Although access in the Kīpahulu Biological Reserve is strictly limited to researchers and managers, the ʻOheʻo region of the park is open for recreation. Attractions include the ʻOheʻo Pools, often called the "Seven Sacred Pools" (a name created by tourism proponents), a car-accessible campground, and several maintained trails, such as the four-mile Pipiwai Loop Trail to Waimoku waterfall. The Kīpahulu ʻOhana, a non-profit community organization established in 1995 through a co-operative agreement with Haleakalā National Park to revive, restore, and share the practices of traditional Native Hawaiian culture, also conducts community-based cultural tours in the area.
    HaleakalaBambooForest1-Texture.jpg
  • Bamboo forest along the Pipiwai trail to Waimoku Fall in the Kipahulu area of Haleakala National Park in Maui, Hawaii<br />
.....<br />
Haleakalā National Park was established as a separate unit of the National Park System in 1960 (it was previously joined with Hawaiʻi National Park on Hawaiʻi Island). At the time, the park only consisted of the crater area of Haleakalā. On March 26, 1951, Kīpahulu Valley was added to Haleakalā National Park (HNP) as the Kīpahulu Biological Reserve to insure protection of endangered ecosystems within the sanctuary. Eighteen years later on January 10, 1969, the HNP boundaries were expanded to include the Kīpahulu coastal area of ʻOheʻo. Although access in the Kīpahulu Biological Reserve is strictly limited to researchers and managers, the ʻOheʻo region of the park is open for recreation. Attractions include the ʻOheʻo Pools, often called the "Seven Sacred Pools" (a name created by tourism proponents), a car-accessible campground, and several maintained trails, such as the four-mile Pipiwai Loop Trail to Waimoku waterfall. The Kīpahulu ʻOhana, a non-profit community organization established in 1995 through a co-operative agreement with Haleakalā National Park to revive, restore, and share the practices of traditional Native Hawaiian culture, also conducts community-based cultural tours in the area.
    HaleakalaBambooForest2.jpg
  • Sunrise in Mount Rainier National Park in Natches Peak trail area near Tipsoo Lake<br />
.....<br />
Tipsoo Lake, at an elevation of 5299 ft (1615 m) above sea level, is an alpine lake within the Northern Cascade Range located near the summit of Chinook Pass in Pierce County, Washington. The area is popular with photographers as the shores and surrounding area abound with the vibrant yellow, orange and purple colors of huckleberry, lupine, Indian paintbrush, and Partridgefoot. There are several hiking trails near the lake that vary in degrees of difficulty and share spectacular views of Mount Rainier and the surrounding landscape.
    MtRainierTipsooPeak1.jpg
  • Sunrise in Mount Rainier National Park in Natches Peak trail area near Tipsoo Lake<br />
.....<br />
Tipsoo Lake, at an elevation of 5299 ft (1615 m) above sea level, is an alpine lake within the Northern Cascade Range located near the summit of Chinook Pass in Pierce County, Washington. The area is popular with photographers as the shores and surrounding area abound with the vibrant yellow, orange and purple colors of huckleberry, lupine, Indian paintbrush, and Partridgefoot. There are several hiking trails near the lake that vary in degrees of difficulty and share spectacular views of Mount Rainier and the surrounding landscape.
    MtRainierTipsooPeak3.jpg
  • Sunrise in Mount Rainier National Park in Natches Peak trail area near Tipsoo Lake<br />
.....<br />
Tipsoo Lake, at an elevation of 5299 ft (1615 m) above sea level, is an alpine lake within the Northern Cascade Range located near the summit of Chinook Pass in Pierce County, Washington. The area is popular with photographers as the shores and surrounding area abound with the vibrant yellow, orange and purple colors of huckleberry, lupine, Indian paintbrush, and Partridgefoot. There are several hiking trails near the lake that vary in degrees of difficulty and share spectacular views of Mount Rainier and the surrounding landscape.
    MtRainierTipsooPeak3.jpg
  • Sunrise in Mount Rainier National Park in Natches Peak trail area near Tipsoo Lake<br />
.....<br />
Tipsoo Lake, at an elevation of 5299 ft (1615 m) above sea level, is an alpine lake within the Northern Cascade Range located near the summit of Chinook Pass in Pierce County, Washington. The area is popular with photographers as the shores and surrounding area abound with the vibrant yellow, orange and purple colors of huckleberry, lupine, Indian paintbrush, and Partridgefoot. There are several hiking trails near the lake that vary in degrees of difficulty and share spectacular views of Mount Rainier and the surrounding landscape.
    MtRainierTipsooPeak3.jpg
  • Sunrise in Mount Rainier National Park in Natches Peak trail area near Tipsoo Lake<br />
.....<br />
Tipsoo Lake, at an elevation of 5299 ft (1615 m) above sea level, is an alpine lake within the Northern Cascade Range located near the summit of Chinook Pass in Pierce County, Washington. The area is popular with photographers as the shores and surrounding area abound with the vibrant yellow, orange and purple colors of huckleberry, lupine, Indian paintbrush, and Partridgefoot. There are several hiking trails near the lake that vary in degrees of difficulty and share spectacular views of Mount Rainier and the surrounding landscape.
    MtRainierTipsooPeak3.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    HohHallMossesTrail2.jpg
  • The Pipiwai trail to Waimoku Fall in the Kipahulu area of Haleakala National Park in Maui, Hawaii
    MauiWaimokuFalls.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    HohHallMossesTrail2.jpg
  • Sunrise in Mount Rainier National Park in Natches Peak trail area near Tipsoo Lake<br />
.....<br />
Tipsoo Lake, at an elevation of 5299 ft (1615 m) above sea level, is an alpine lake within the Northern Cascade Range located near the summit of Chinook Pass in Pierce County, Washington. The area is popular with photographers as the shores and surrounding area abound with the vibrant yellow, orange and purple colors of huckleberry, lupine, Indian paintbrush, and Partridgefoot. There are several hiking trails near the lake that vary in degrees of difficulty and share spectacular views of Mount Rainier and the surrounding landscape.
    MtRainierTipsooPeak1.jpg
  • Sunrise in Mount Rainier National Park in Natches Peak trail area near Tipsoo Lake<br />
.....<br />
Tipsoo Lake, at an elevation of 5299 ft (1615 m) above sea level, is an alpine lake within the Northern Cascade Range located near the summit of Chinook Pass in Pierce County, Washington. The area is popular with photographers as the shores and surrounding area abound with the vibrant yellow, orange and purple colors of huckleberry, lupine, Indian paintbrush, and Partridgefoot. There are several hiking trails near the lake that vary in degrees of difficulty and share spectacular views of Mount Rainier and the surrounding landscape.
    MtRainierTipsooPeak1.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    HohHallMossesTrail2.jpg
  • Banyan trees and roots along the Pipiwai trail in Maui's Haleakala national park
    HaleakalaBanyanRoots1.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers1.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • The sun is setting behind Mount Rainier from Naches Peak loop trail
    MountRainierNachesSunburst1.jpg
  • Snowshoers on the Mazama Ridge snowshoe trail on Mount Rainier in Washington state
    Rainier Snowshoers.jpg
  • The sun is setting behind Mount Rainier from Naches Peak loop trail
    MountRainierNachesSunburst1.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    CascadePassHiker1.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    CascadePassHiker1.jpg
  • View of Dewey Lake and distant mountain ridges from Naches Peak trail in Mount Rainier National Park in Washington state.
    MtRainierDeweyLake.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • Stevie Ray Vaughan Memorial is a bronze sculpture of Stevie Ray Vaughan by Ralph Helmick, located at the intersection of Town Lake Hike and Bike Trail (South Bank at South 1st and Riverside Drive) in Austin, Texas, in the United States. The work was installed in 1994 and is maintained by Austin Parks & Recreation. It has become a popular tourist attraction, and often has flowers and other devotions at its base.
    AustinSRV4.jpg
  • Stevie Ray Vaughan Memorial is a bronze sculpture of Stevie Ray Vaughan by Ralph Helmick, located at the intersection of Town Lake Hike and Bike Trail (South Bank at South 1st and Riverside Drive) in Austin, Texas, in the United States. The work was installed in 1994 and is maintained by Austin Parks & Recreation. It has become a popular tourist attraction, and often has flowers and other devotions at its base.
    AustinSRV4.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    CascadePassHiker1-2.jpg
  • The Old State House is an historic government building located at the intersection of Washington and State Streets in Boston, Massachusetts, USA. Built in 1713, it is the oldest surviving public building in Boston, and the seat of the state's legislature until 1798. It is now a history museum operated by the Bostonian Society, a nonprofit whose primary focus is the museum. It is one of many historic landmarks that can be visited along the Freedom Trail.
    BostonOldStateHouse1.jpg
  • The sun is setting behind Mount Rainier from Naches Peak loop trail
    MountRainierNachesSunburst1.jpg
  • Snowshoers on the Mazama Ridge snowshoe trail on Mount Rainier in Washington state
    Rainier Snowshoers.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers1.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • Snowshoers on the Mazama Ridge snowshoe trail on Mount Rainier in Washington state
    Rainier Snowshoers.jpg
  • View of Dewey Lake and distant mountain ridges from Naches Peak trail in Mount Rainier National Park in Washington state.
    MtRainierDeweyLake.jpg
  • Dallas is the ninth most populous city in the United States of America and the third most populous city in the state of Texas. The Dallas-Fort Worth metroplex is the largest metropolitan area in the South and fourth-largest metropolitan area in the United States. Divided among Collin, Dallas, Denton, Kaufman, and Rockwall counties, the city had a population of 1,197,816 in 2010, according to the United States Census Bureau.<br />
The city is the largest economic center of the 12-county Dallas–Fort Worth–Arlington metropolitan area (the DFW MSA) that according to the March 2010 U.S. Census Bureau release, had a population of 3,371,773. The metroplex economy is the sixth largest in the United States, with a 2010 gross metropolitan product of $374 billion. Its 2010 Real GDP amounted to $325 billion according to ‘Urban America: US cities in the global economy,’ which was published by the McKinsey Global Institute in April 2012.<br />
Dallas was founded in 1841 and was formally incorporated as a city in February 1856. The city's economy is primarily based on banking, commerce, telecommunications, computer technology, energy, healthcare and medical research, transportation and logistics. The city is home to the third largest concentration of Fortune 500 companies in the nation. Located in North Texas and a major city in the American South, Dallas is the main core of the largest inland metropolitan area in the United States that lacks any navigable link to the sea.
    DallasReunionTower2.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    CascadePassHiker1.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    CascadePassHiker1.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers1.jpg
  • Snowshoers on the Mazama Ridge snowshoe trail on Mount Rainier in Washington state
    Rainier Snowshoers.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    CascadePassHiker1.jpg
  • Cascade Pass (formerly also known as Skagit Pass) is a 5,392-foot (1,643 m) mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S.  It  provides the easiest connection from the Cascade River to the head of Lake Chelan, and is now inside North Cascades National Park, and crossed by only a hiking trail.
    CascadePassHiker1.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers1.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers1.jpg
  • Snowshoers on the Mazama Ridge snowshoe trail on Mount Rainier in Washington state
    Rainier Snowshoers.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • View of Dewey Lake and distant mountain ridges from Naches Peak trail in Mount Rainier National Park in Washington state.
    MtRainierDeweyLake.jpg
  • Bluebonnets at Grapevine Lake in North Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    FlowerMound1.jpg
  • Bluebonnets at Grapevine Lake in North Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    FlowerMound1.jpg
  • Bluebonnets at Grapevine Lake in North Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    FlowerMound1.jpg
  • Bluebonnets at Grapevine Lake in North Texas
    _D3_3697.jpg
  • Bluebonnets at Grapevine Lake in North Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    FlowerMound1.jpg
  • Bluebonnets at Grapevine Lake in North Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    FlowerMound1.jpg
  • Bluebonnets at Grapevine Lake in North Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    FlowerMound1.jpg
  • Bluebonnets at Grapevine Lake in North Texas
    _D3_3725-Edit.jpg
  • The Gardens of Marqueyssac are located in the town of Vézac, in the French area of Dordogne, in the region of Nouvelle-Aquitaine. It is on the list of "jardins remarquables de France" (remarkable gardens in France). The park of Château de Marqueyssac is a private estate of twenty-two hectares built around an 18th century castle. Its facilities are typical of what was done in France under Napoleon III.<br />
<br />
Built on a rocky spur 130 meters above the river, the park offers a view of the valley, castles and nearby villages, including Beynac-et-Cazenac, Fayrac, Castelnaud, La Roque-Gageac and Domme.<br />
<br />
In 2011, it was the third most visited tourist site in the Dordogne with 190,000 visitors.
    JardinsDeMarqueyssac9.jpg
  • Bluebonnets at Grapevine Lake in North Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    FlowerMound1.jpg
  • Bluebonnets at Grapevine Lake in North Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    FlowerMound1.jpg
  • The Talimena Scenic Drive is a National Scenic Byway in southeastern Oklahoma and extreme western Arkansas spanning a 54.0-mile (86.9 km) stretch of Oklahoma State Highway 1 (SH-1) and Arkansas Highway 88 (Hwy 88) from Talihina, Oklahoma, to Mena, Arkansas. Designated a National Scenic Byway by the America's Byway Program in 2005, the road travels within the Ouachita National Forest along the highest peaks of the Winding Stair Mountains, part of the Ouachita Mountain chain, including the second tallest peak in Arkansas, Rich Mountain, 2,681 feet in elevation. Many of the forests along these ridges, stunted and of little commercial value, were never logged and are old growth. The two-lane road features hiking trails beginning at various points along its stretch and 22 scenic vista pull-outs. There are at least 13% hill grades along the route.
    TalimenaVista2.jpg
  • Griffith Park is a large municipal park at the eastern end of the Santa Monica Mountains, in the Los Feliz neighborhood of Los Angeles, California. The park covers 4,310 acres of land, making it one of the largest urban parks in North America. It is the second-largest city park in California, after Mission Trails Preserve in San Diego, and the 11th largest municipally-owned park in the United States. It has also been referred to as the Central Park of Los Angeles but is much larger, more untamed, and rugged than its New York City counterpart.
    HollywoodHills1.jpg
  • Bighorn sheep along the Colorado River in the interior of the Grand Canyon
    GrandCanyonBighorns1.jpg
  • Mountain goat in the Enchantment Lakes Wilderness in Washington state
    EnchantmentsMountainGoats2.jpg
  • The Margaret Hunt Hill Bridge is a bridge in Dallas, Texas which spans the Trinity River and was built as part of the Trinity River Project. Designed by Santiago Calatrava, it is one of three such bridges planned to be built over the Trinity; the second, the Margaret McDermott Bridge, is currently under construction. The span parallels the Continental Avenue Bridge, a walking bridge.<br />
<br />
The bridge is named for Margaret Hunt Hill, an heiress and philanthropist.<br />
<br />
Dallas is the ninth most populous city in the United States of America and the third most populous city in the state of Texas. The Dallas-Fort Worth metroplex is the largest metropolitan area in the South and fourth-largest metropolitan area in the United States. Divided among Collin, Dallas, Denton, Kaufman, and Rockwall counties, the city had a population of 1,197,816 in 2010, according to the United States Census Bureau.
    DallasMHHBridge6.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon1.jpg
  • Dallas is the ninth most populous city in the United States of America and the third most populous city in the state of Texas. The Dallas-Fort Worth metroplex is the largest metropolitan area in the South and fourth-largest metropolitan area in the United States. Divided among Collin, Dallas, Denton, Kaufman, and Rockwall counties, the city had a population of 1,197,816 in 2010, according to the United States Census Bureau.<br />
The city is the largest economic center of the 12-county Dallas–Fort Worth–Arlington metropolitan area (the DFW MSA) that according to the March 2010 U.S. Census Bureau release, had a population of 3,371,773. The metroplex economy is the sixth largest in the United States, with a 2010 gross metropolitan product of $374 billion. Its 2010 Real GDP amounted to $325 billion according to ‘Urban America: US cities in the global economy,’ which was published by the McKinsey Global Institute in April 2012.<br />
Dallas was founded in 1841 and was formally incorporated as a city in February 1856. The city's economy is primarily based on banking, commerce, telecommunications, computer technology, energy, healthcare and medical research, transportation and logistics. The city is home to the third largest concentration of Fortune 500 companies in the nation. Located in North Texas and a major city in the American South, Dallas is the main core of the largest inland metropolitan area in the United States that lacks any navigable link to the sea.
    DallasDealyPlaza1.jpg
  • Footbridge across pond surrounded by maples in fall color, at Kubota Japanese Gardens, Seattle, Washington
    KubotaRedRailing2.jpg
  • Dallas is the ninth most populous city in the United States of America and the third most populous city in the state of Texas. The Dallas-Fort Worth metroplex is the largest metropolitan area in the South and fourth-largest metropolitan area in the United States. Divided among Collin, Dallas, Denton, Kaufman, and Rockwall counties, the city had a population of 1,197,816 in 2010, according to the United States Census Bureau.<br />
The city is the largest economic center of the 12-county Dallas–Fort Worth–Arlington metropolitan area (the DFW MSA) that according to the March 2010 U.S. Census Bureau release, had a population of 3,371,773. The metroplex economy is the sixth largest in the United States, with a 2010 gross metropolitan product of $374 billion. Its 2010 Real GDP amounted to $325 billion according to ‘Urban America: US cities in the global economy,’ which was published by the McKinsey Global Institute in April 2012.<br />
Dallas was founded in 1841 and was formally incorporated as a city in February 1856. The city's economy is primarily based on banking, commerce, telecommunications, computer technology, energy, healthcare and medical research, transportation and logistics. The city is home to the third largest concentration of Fortune 500 companies in the nation. Located in North Texas and a major city in the American South, Dallas is the main core of the largest inland metropolitan area in the United States that lacks any navigable link to the sea.
    DallasLights2.jpg
  • Footbridge across pond surrounded by maples in fall color, at Kubota Japanese Gardens, Seattle, Washington
    KubotaFallScene2.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon1.jpg
  • Reflection in the Colorado River at Lava Falls, in the Grand Canyon National Park<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    _MG_9398.jpg
  • Prickly Pear cactus at the mouth of Havasu Canyon, Grand Canyon National Park<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonHavasuCactus.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon3.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon2.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park with barrel cacti in foreground
    NankoweapCactus.jpg
  • Rafts at dawn on the Colorado River in the interior of the Grand Canyon
    GrandCanyonDawnRafts1.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon1.jpg
  • Footbridge across pond surrounded by maples in fall color, at Kubota Japanese Gardens, Seattle, Washington
    KubotaGardensBridge2.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollSteam6.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollSteam5.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollSteam2.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll2.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    _A1A7917.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollRiver1.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll1.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll7.jpg
  • Reflection in the Colorado River at Lava Falls, in the Grand Canyon National Park<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    _MG_9397.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park with barrel cacti in foreground
    NankoweapCactus.jpg
  • Saddle Canyon Small Tree
    GrandCanyonSaddleCanyonTree1.jpg
  • The Margaret Hunt Hill Bridge is a bridge in Dallas, Texas which spans the Trinity River and was built as part of the Trinity River Project. Designed by Santiago Calatrava, it is one of three such bridges planned to be built over the Trinity; the second, the Margaret McDermott Bridge, is currently under construction. The span parallels the Continental Avenue Bridge, a walking bridge.<br />
<br />
The bridge is named for Margaret Hunt Hill, an heiress and philanthropist.<br />
<br />
Dallas is the ninth most populous city in the United States of America and the third most populous city in the state of Texas. The Dallas-Fort Worth metroplex is the largest metropolitan area in the South and fourth-largest metropolitan area in the United States. Divided among Collin, Dallas, Denton, Kaufman, and Rockwall counties, the city had a population of 1,197,816 in 2010, according to the United States Census Bureau.
    DallasMHHBridge9.jpg
  • The Margaret Hunt Hill Bridge is a bridge in Dallas, Texas which spans the Trinity River and was built as part of the Trinity River Project. Designed by Santiago Calatrava, it is one of three such bridges planned to be built over the Trinity; the second, the Margaret McDermott Bridge, is currently under construction. The span parallels the Continental Avenue Bridge, a walking bridge.<br />
<br />
The bridge is named for Margaret Hunt Hill, an heiress and philanthropist.<br />
<br />
Dallas is the ninth most populous city in the United States of America and the third most populous city in the state of Texas. The Dallas-Fort Worth metroplex is the largest metropolitan area in the South and fourth-largest metropolitan area in the United States. Divided among Collin, Dallas, Denton, Kaufman, and Rockwall counties, the city had a population of 1,197,816 in 2010, according to the United States Census Bureau.
    DallasMHHBridge3.jpg
  • The Margaret Hunt Hill Bridge is a bridge in Dallas, Texas which spans the Trinity River and was built as part of the Trinity River Project. Designed by Santiago Calatrava, it is one of three such bridges planned to be built over the Trinity; the second, the Margaret McDermott Bridge, is currently under construction. The span parallels the Continental Avenue Bridge, a walking bridge.<br />
<br />
The bridge is named for Margaret Hunt Hill, an heiress and philanthropist.<br />
<br />
Dallas is the ninth most populous city in the United States of America and the third most populous city in the state of Texas. The Dallas-Fort Worth metroplex is the largest metropolitan area in the South and fourth-largest metropolitan area in the United States. Divided among Collin, Dallas, Denton, Kaufman, and Rockwall counties, the city had a population of 1,197,816 in 2010, according to the United States Census Bureau.
    DallasMHHBridge4.jpg
  • Dallas is the ninth most populous city in the United States of America and the third most populous city in the state of Texas. The Dallas-Fort Worth metroplex is the largest metropolitan area in the South and fourth-largest metropolitan area in the United States. Divided among Collin, Dallas, Denton, Kaufman, and Rockwall counties, the city had a population of 1,197,816 in 2010, according to the United States Census Bureau.<br />
The city is the largest economic center of the 12-county Dallas–Fort Worth–Arlington metropolitan area (the DFW MSA) that according to the March 2010 U.S. Census Bureau release, had a population of 3,371,773. The metroplex economy is the sixth largest in the United States, with a 2010 gross metropolitan product of $374 billion. Its 2010 Real GDP amounted to $325 billion according to ‘Urban America: US cities in the global economy,’ which was published by the McKinsey Global Institute in April 2012.<br />
Dallas was founded in 1841 and was formally incorporated as a city in February 1856. The city's economy is primarily based on banking, commerce, telecommunications, computer technology, energy, healthcare and medical research, transportation and logistics. The city is home to the third largest concentration of Fortune 500 companies in the nation. Located in North Texas and a major city in the American South, Dallas is the main core of the largest inland metropolitan area in the United States that lacks any navigable link to the sea.
    DallasTrinityRiver1.jpg
  • Dallas is the ninth most populous city in the United States of America and the third most populous city in the state of Texas. The Dallas-Fort Worth metroplex is the largest metropolitan area in the South and fourth-largest metropolitan area in the United States. Divided among Collin, Dallas, Denton, Kaufman, and Rockwall counties, the city had a population of 1,197,816 in 2010, according to the United States Census Bureau.<br />
The city is the largest economic center of the 12-county Dallas–Fort Worth–Arlington metropolitan area (the DFW MSA) that according to the March 2010 U.S. Census Bureau release, had a population of 3,371,773. The metroplex economy is the sixth largest in the United States, with a 2010 gross metropolitan product of $374 billion. Its 2010 Real GDP amounted to $325 billion according to ‘Urban America: US cities in the global economy,’ which was published by the McKinsey Global Institute in April 2012.<br />
Dallas was founded in 1841 and was formally incorporated as a city in February 1856. The city's economy is primarily based on banking, commerce, telecommunications, computer technology, energy, healthcare and medical research, transportation and logistics. The city is home to the third largest concentration of Fortune 500 companies in the nation. Located in North Texas and a major city in the American South, Dallas is the main core of the largest inland metropolitan area in the United States that lacks any navigable link to the sea.
    DallasLights1.jpg
  • Seattle skyline at dawn on a winter day in February
    SeattleDowntownSunrise3.jpg
  • Anchorage (officially called the Municipality of Anchorage) is a unified home rule municipality in the southcentral part of the U.S. state of Alaska. It is the northernmost city in the United States with more than 100,000 residents and the largest community in North America north of the 60th parallel. With an estimated 298,610 residents in 2012 (and 380,821 residents within its Metropolitan Statistical Area, which combines Anchorage with the neighboring Matanuska-Susitna Borough), it is Alaska's most populous city and constitutes more than 40 percent of the state's total population; among the 50 states, only New York has a higher percentage of residents who live in the state's most populous city.
    AnchorageAutumn2.jpg
  • Footbridge across pond surrounded by maples in fall color, at Kubota Japanese Gardens, Seattle, Washington
    SeattleKubota1.jpg
  • Footbridge across pond surrounded by maples in fall color, at Kubota Japanese Gardens, Seattle, Washington
    _MG_3259.jpg
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