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  • Mountain Larches at Lake Ann in the North Cascades National Park
    LakeAnnLarches3.jpg
  • Waterfall along Asgaard pass route to the Enchantment Lakes in Washington with Dragontail Peak in the background
    EnchantmentsAsgaardPassTree.jpg
  • Prusik Peak from Gnome Tarn in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnSunrise1.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierSnowshoers2.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
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • The Border Peaks between USA and Canada in North Cascades national park in the midst of a very cold winter.
    MtBakerCascadesWinterMorning1.jpg
  • The rising sun casts its first rays on the Border Peaks between USA and Canada in North Cascades national park in the midst of a very cold winter.
    MtBakerCascades1.jpg
  • Mountain Larches at Blue Lake
    Blue Lake and Spires 2.jpg
  • Blue Lake shoreline, North Cascades
    BlueLakeLog.jpg
  • Sol Duc Falls in Olympic National Park, The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucFallsBridge1.jpg
  • Small creek near Sol Duc Falls.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucCascades6.jpg
  • Sol Duc Falls in Olympic National Park.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucFallSide.jpg
  • Little red bloodstar starfish on kelp in Washington state's Salt Creek County Park
    LittleRedStarfish-LAB.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona
    HorseshoeBendLeft.jpg
  • Slickrock ridges at South Coyote Buttes, Arizona
    RainbowRocksStriations4.jpg
  • Swirl in the sandstone at White Pocket, AZ
    WhitePocketsSwirl1.jpg
  • Canyon wall in Buckskin Gulch, Paria Canyon Wilderness. The Buckskin Gulch, a canyon in southern Utah, is one of the main tributaries of the Paria River, which is itself a minor tributary of the Colorado River. It is the longest and deepest slot canyon in the southwest United States and may very well be the longest in the world. As such it is one of the premier destinations for slot canyon hikers, and receives a high amount of foot traffic.<br />
At over 13 miles (21 km) in length it is often visited in conjunction with the longer Paria Canyon, although some prefer to make a long day trip out of the hike. With a distance of 20 miles (32 km), hiking this canyon in one day is possible. Wire Pass, a short tributary to the Buckskin, is an ideal alternative for a short day hike that still takes hikers through the narrow, curving features that are the hallmark of slot canyons
    BuckskinRoughSea.jpg
  • Abstract patterns in Lower Antelope Canyon, Page, Arizona
    AntelopeAbstractCurve1.jpg
  • Cracked earth and bushes in Valley of the Gods, Utah
    ValleyOfTheGods2.jpg
  • Mystery Valley in the Monument Valley Navajo tribal park.  Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the southern border of Utah with northern Arizona near the Four Corners area.
    MysteryValleyPancake1.jpg
  • Sand dunes near Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles2.jpg
  • First light at Yei-bi-Chai rocks in Monument Valley
    MonumentValleyYeibicheiSunrise2.jpg
  • Vishnu Schist, Grand Canyon National Park.  This is the bottommost and oldest layer of rock exposed in the canyon, around 2 billion years old!
    GrandCanyonVishnuSchist1-B&W.jpg
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon<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.
    GrandCanyonHavasuCreek2.jpg
  • Slot canyon in Deer Creek patio.  Deer Creek is a side stream to the Colorado River in the interior of the Grand Canyon.
    GrandCanyonDeerCreekSlot3.jpg
  • Blacktail Canyon, a side canyon to the Grand Canyon.
    GrandCanyonBlacktail2.jpg
  • Small waterfall on Clear Creek, a side stream to the Colorado River in the interior of the Grand Canyon
    GrandCanyonClearCreek1.jpg
  • The Colorado River from Cardenas in the interior of the canyon in the interior of the canyon
    GrandCanyonCardenas4.jpg
  • Ruin on a hilltop at Cardenas Creek in the interior of the Grand Canyon
    GrandCanyonCardenasHilltopRuin3.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon2.jpg
  • Ancient Anaszi ruins high above the Colorado River in the Marble Canyon section of Grand Canyon National Park
    NankoweapRuins3.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon1.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapHoodoos2.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSingleHoodoo1.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSingleHoodoo2.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSky3.jpg
  • Sandstone patterns in Lower Antelope Canyon near Page, Arizona
    AntelopeSandstonePatterns2.jpg
  • View of the canyon walls ofthe Grand Canyon seen from a raft on the Colorado River
    GrandCanyonRiver1.jpg
  • Vishnu Schist, Grand Canyon National Park.  This is the bottommost and oldest layer of rock exposed in the canyon, around 2 billion years old!
    GrandCanyonVishnuSchist2-B&W.jpg
  • Vishnu Schist, Grand Canyon National Park.  This is the bottommost and oldest layer of rock exposed in the canyon, around 2 billion years old!
    GrandCanyonVishnuSchist1-B&W.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
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon<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.
    GrandCanyonHavasuCreek3.jpg
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon
    GrandCanyonHavasuCreekPool1.jpg
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon
    _MG_9325.jpg
  • Slot canyon in Deer Creek patio.  Deer Creek is a side stream to the Colorado River in the interior of the Grand Canyon.
    GrandCanyonDeerCreekSlot1.jpg
  • Waterfall on Thunder River, a tributary to the Colorado River in Grand Canyon National Park
    GrandCanyonThunderRiver1.jpg
  • Elves Chasm waterfall in the interior of the Grand Canyon.
    GrandCanyonElvesChasm1.jpg
  • The Colorado River from Cardines in the interior of the canyon
    GrandCanyonCardenas1.jpg
  • Little Colorado River confluence with the Colorado River
    GrandCanyonLittleColorado3.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
    GrandCanyonMarbleCanyon4.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
    GrandCanyonMarbleCanyon1.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
  • Dawn at the south rim of the Grand Canyon
    GrandCanyonDawn.jpg
  • _A1A5125.jpg
  • _A1A5108.jpg
  • Billy Bob's honky tonk in the Fort Worth Stockyards in Texas
    BillyBobsGate1.jpg
  • Billy Bob's honky tonk in the Fort Worth Stockyards in Texas
    BillyBobs4-Edit.jpg
  • Flamingos are a type of wading bird in the genus Phoenicopterus, the only genus in the family Phoenicopteridae. There are four flamingo species in the Americas and two species in the Old World. Flamingos often stand on one leg, the other leg tucked beneath the body. The reason for this behaviour is not fully understood. Recent research indicates that standing on one leg may allow the birds to conserve more body heat, given that they spend a significant amount of time wading in cold water. However, the behaviour also takes place in warm water. As well as standing in the water, flamingos may stamp their webbed feet in the mud to stir up food from the bottom.
    ArguingFlamingos1.jpg
  • Flamingos are a type of wading bird in the genus Phoenicopterus, the only genus in the family Phoenicopteridae. There are four flamingo species in the Americas and two species in the Old World. Flamingos often stand on one leg, the other leg tucked beneath the body. The reason for this behaviour is not fully understood. Recent research indicates that standing on one leg may allow the birds to conserve more body heat, given that they spend a significant amount of time wading in cold water. However, the behaviour also takes place in warm water. As well as standing in the water, flamingos may stamp their webbed feet in the mud to stir up food from the bottom.
    FlamingoPanorama-5.jpg
  • Mount Baker reflecting in tarn near Park Butte in the Mount Baker Wilderness <br />
..... <br />
Mount Baker, also known as Koma Kulshan or simply Kulshan, is an active glaciated andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington State in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount Saint Helens. About 31 miles due east of the city of Bellingham, Whatcom County, Mount Baker is the youngest volcano in the Mount Baker volcanic field. While volcanism has persisted here for some 1.5 million years, the current glaciated cone is likely no more than 140,000 years old, and possibly no older than 80-90,000 years. <br />
After Mount Rainier, Mount Baker is the most heavily glaciated of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, 0.43 cu mi is greater than that of all the other Cascades volcanoes (except Rainier) combined. At 10,781 ft, it is the third-highest mountain in Washington State and the fifth-highest in the Cascade Range, if Little Tahoma Peak, a subpeak of Mount Rainier, and Shastina, a subpeak of Mount Shasta, are not counted. Located in the Mount Baker Wilderness, it is visible from much of Greater Victoria, Greater Vancouver, and, to the south, from Seattle (and on clear days Tacoma) in Washington. <br />
Indigenous natives have known the mountain for thousands of years, but the first written record of the mountain is from the Spanish. Spanish explorer Gonzalo Lopez de Haro mapped it in 1790 as the Gran Montana del Carmelo, "Great Mount Carmel". The explorer George Vancouver renamed the mountain for 3rd Lieutenant Joseph Baker of HMS Discovery, who saw it on April 30, 1792.
    MountBakerParkButteTarn2.jpg
  • Summer wildflowers at Tipsoo Lake in Mount Rainier National Park
    MountRainierTipsooFlowers2.jpg
  • Boulders along lake in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnRocks1.jpg
  • Creek entering Perfection Lake in the Enchantment Lakes area of Alpine Lakes Wilderness, Washington
    EnchantmentsPerfectionLake1.jpg
  • Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the Arizona–Utah border, near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation and is accessible from U.S. Highway 163.<br />
<br />
Monument Valley has been featured in many forms of media since the 1930s. Director John Ford used the location for a number of his best-known films and thus, in the words of critic Keith Phipps, "its five square miles have defined what decades of moviegoers think of when they imagine the American West
    MonumentValleyStagecoach1.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.jpg
  • Arches National Park is a US National Park in eastern Utah. The park is located on the Colorado River 4 miles (6.4 km) north of Moab, Utah. It is known for containing over 2,000 natural sandstone arches, including the world-famous Delicate Arch, in addition to a variety of unique geological resources and formations.<br />
<br />
The park is located just outside of Moab, Utah, and is 76,359 acres in area.<br />
<br />
Administered by the National Park Service, the area was originally named a National Monument on April 12, 1929. It was redesignated as a National Park on November 12, 1971.
    ArchesWindow3.jpg
  • Mt Rainier at Reflection Lakes in Winter
    RainierFaceWinter.jpg
  • Misty Reflection at Mount Rainier's Reflection Lakes
    MountRainierReflectionLakes1.jpg
  • The sun is setting behind Mount Rainier from Naches Peak loop trail
    MountRainierNachesSunburst1.jpg
  • Mount Rainier National Park wilderness near Panhandle Gap along the Wonderland trail in winter
    SummerlandFryingpanMoon1.jpg
  • Mount Rainier National Park wilderness near Panhandle Gap along the Wonderland trail in winter
    SummerlandCamp.jpg
  • Wildflowers at rim of Crater Lake, Oregon, at sunset
    CraterLakeFlowers.jpg
  • Trees at rim of Crater Lake, Oregon, at sunrise
    CraterLakeTrees.jpg
  • Crater Lake National Park in Oregon
    CraterLakeRim.jpg
  • Wizard Island in Crater Lake, Oregon
    CraterLakeWizardIsland1.jpg
  • Sequoia and King Canyon National Park, California
    SequoiaCrescentMeadowsGrove2.jpg
  • Mt Rainier at Reflection Lakes in Winter
    MtRainierHallwayTrees1.jpg
  • Mt Rainier at Reflection Lakes with three small trees
    MtRainierThreeTrees1.jpg
  • Mt Rainier and waves in the snow
    MtRainierWavySnow.jpg
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon
    GrandCanyonHavasuCreekPool2.jpg
  • Matkatamiba Canyon is a side canyon to the Grand Canyon accessible from the Colorado River<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.
    GrandCanyonMatkatamiba2.jpg
  • Stone Creek is a side stream to the Grand Canyon accessible only from the Colorado River
    _MG_9154.jpg
  • River Runners on the Colorado River
    GrandCanyonGraniteRaft1.jpg
  • Small waterfall on Clear Creek, a side stream to the Colorado River in the interior of the Grand Canyon
    GrandCanyonClearCreek4.jpg
  • The Colorado River from Cardenas in the interior of the canyon
    GrandCanyonCardenas1.jpg
  • Ruin on a hilltop at Cardenas Creek in the interior of the Grand Canyon
    GrandCanyonCardenasHilltopRuin3.jpg
  • Ancient Anaszi ruins high above the Colorado River in the Marble Canyon section of Grand Canyon National Park
    NankoweapRuins3.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon1.jpg
  • Paradise River cascading over granite rocks in Mt Rainier National Park
    MtRainierParadiseRiverRocks3.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierTipsoo9.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • Sunset at Mount Rainier's Spray Park area
    MrRainerSprayParkPan1.jpg
  • The Window in Arches National Park
    ArchesTheWindow.jpg
  • Boy and a giant Sequoia tree.  Sequoia National Park, California.
    SequoiaMartin1.jpg
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