Show Navigation

Search Results

Refine Search
Match all words
Match any word
Prints
Personal Use
Royalty-Free
Rights-Managed
(leave unchecked to
search all images)
{ 1302 images found }

Loading ()...

  • Abstract pattern in Caverns of Sonora, Sutton County, Texas, USA. The world-class Caverns of Sonora have a stunning and sparkling array of speleothems (helictites, stalactites, stalagmites, flowstone, coral trees, and other calcite crystal formations). National Speleological Society co-founder, Bill Stephenson said, after seeing it for the first time, "The beauty of Caverns of Sonora cannot be exaggerated...not even by a Texan!" Geologically, the cave formed between 1.5 to 5 million years ago within 100-million-year-old (Cretaceous) Segovia limestone, of the Edward limestone group. A fault allowed gases to rise up to mix with aquifer water, making acid which dissolved the limestone, leaving the cave. Between 1 and 3 million years ago, the water drained from the cave, after which speleothems begain forming. It is one of the most active caves in the world, with over 95% of its formations still growing. Sonora Caves are on Interstate 10, about half-way between Big Bend National Park and San Antonio, Texas.
    1403TX-412_Caverns-of-Sonora_Texas.jpg
  • Tides have shaped sea sand into scalloped abstract patterns at Seaside, on the Oregon coast, USA
    08ORC-701.jpg
  • Abstract pattern in Caverns of Sonora, Sutton County, Texas, USA. The world-class Caverns of Sonora have a stunning and sparkling array of speleothems (helictites, stalactites, stalagmites, flowstone, coral trees, and other calcite crystal formations). National Speleological Society co-founder, Bill Stephenson said, after seeing it for the first time, "The beauty of Caverns of Sonora cannot be exaggerated...not even by a Texan!" Geologically, the cave formed between 1.5 to 5 million years ago within 100-million-year-old (Cretaceous) Segovia limestone, of the Edward limestone group. A fault allowed gases to rise up to mix with aquifer water, making acid which dissolved the limestone, leaving the cave. Between 1 and 3 million years ago, the water drained from the cave, after which speleothems begain forming. It is one of the most active caves in the world, with over 95% of its formations still growing. Sonora Caves are on Interstate 10, about half-way between Big Bend National Park and San Antonio, Texas.
    1403TX-357_Caverns-of-Sonora_Texas.jpg
  • Tides have shaped sea sand into scalloped abstract patterns at Seaside, on the Oregon coast, USA
    08ORC-700.jpg
  • An abstract pattern of orange-yellow sandstone decorates Crack Canyon, on federal BLM land in San Rafael Swell, near Goblin Valley State Park, Utah, USA. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW3-098_Crack-Canyon_pattern.jpg
  • Abstract: A car hood reflects a lined pattern of a fiberglass roof, in Lima, Peru, South America.
    14PER2-010.jpg
  • Abstract flowstone pattern, Carlsbad Caverns National Park, in the Guadalupe Mountains, Chihuahuan Desert, southeast New Mexico, USA. Hike in on your own via the natural entrance or take an elevator from the visitor center. Geology: 4 to 6 million years ago, an acid bath in the water table slowly dissolved the underground rooms of Carlsbad Caverns, which then drained along with the uplift of the Guadalupe Mountains. The Guadalupe Mountains are the uplifted part of the ancient Capitan Reef which thrived along the edge of an inland sea more than 250 million years ago during Permian time. Carlsbad Caverns National Park protects part of the Capitan Reef, one of the best-preserved, exposed Permian-age fossil reefs in the world. The park's magnificent speleothems (cave formations) are due to rain and snowmelt soaking through soil and limestone rock, dripping into a cave, evaporating and depositing dissolved minerals. Drip-by-drip, over the past million years or so, Carlsbad Cavern has slowly been decorating itself. The slowest drips tend to stay on the ceiling (as stalactites, soda straws, draperies, ribbons or curtains). The faster drips are more likely to decorate the floor (with stalagmites, totem poles, flowstone, rim stone dams, lily pads, shelves, and cave pools). Today, due to the dry desert climate, few speleothems inside any Guadalupe Mountains caves are wet enough to actively grow. Most speleothems inside Carlsbad Cavern would have been much more active during the last ice age-up to around 10,000 years ago, but are now mostly inactive.
    1404NM-5031_Carlsbad-Caverns-NP.jpg
  • Abstract white ceiling pattern marbled with yellow in Caverns of Sonora, Sutton County, Texas, USA. The world-class Caverns of Sonora have a stunning and sparkling array of speleothems (helictites, stalactites, stalagmites, flowstone, coral trees, and other calcite crystal formations). National Speleological Society co-founder, Bill Stephenson said, after seeing it for the first time, "The beauty of Caverns of Sonora cannot be exaggerated...not even by a Texan!" Geologically, the cave formed between 1.5 to 5 million years ago within 100-million-year-old (Cretaceous) Segovia limestone, of the Edward limestone group. A fault allowed gases to rise up to mix with aquifer water, making acid which dissolved the limestone, leaving the cave. Between 1 and 3 million years ago, the water drained from the cave, after which speleothems begain forming. It is one of the most active caves in the world, with over 95% of its formations still growing. Sonora Caves are on Interstate 10, about half-way between Big Bend National Park and San Antonio, Texas.
    1403TX-439_Caverns-of-Sonora_Texas.jpg
  • Abstract white ceiling pattern marbled with yellow in Caverns of Sonora, Sutton County, Texas, USA. The world-class Caverns of Sonora have a stunning and sparkling array of speleothems (helictites, stalactites, stalagmites, flowstone, coral trees, and other calcite crystal formations). National Speleological Society co-founder, Bill Stephenson said, after seeing it for the first time, "The beauty of Caverns of Sonora cannot be exaggerated...not even by a Texan!" Geologically, the cave formed between 1.5 to 5 million years ago within 100-million-year-old (Cretaceous) Segovia limestone, of the Edward limestone group. A fault allowed gases to rise up to mix with aquifer water, making acid which dissolved the limestone, leaving the cave. Between 1 and 3 million years ago, the water drained from the cave, after which speleothems begain forming. It is one of the most active caves in the world, with over 95% of its formations still growing. Sonora Caves are on Interstate 10, about half-way between Big Bend National Park and San Antonio, Texas.
    1403TX-438_Caverns-of-Sonora_Texas.jpg
  • Abstract wall pattern in Caverns of Sonora, Sutton County, Texas, USA. The world-class Caverns of Sonora have a stunning and sparkling array of speleothems (helictites, stalactites, stalagmites, flowstone, coral trees, and other calcite crystal formations). National Speleological Society co-founder, Bill Stephenson said, after seeing it for the first time, "The beauty of Caverns of Sonora cannot be exaggerated...not even by a Texan!" Geologically, the cave formed between 1.5 to 5 million years ago within 100-million-year-old (Cretaceous) Segovia limestone, of the Edward limestone group. A fault allowed gases to rise up to mix with aquifer water, making acid which dissolved the limestone, leaving the cave. Between 1 and 3 million years ago, the water drained from the cave, after which speleothems begain forming. It is one of the most active caves in the world, with over 95% of its formations still growing. Sonora Caves are on Interstate 10, about half-way between Big Bend National Park and San Antonio, Texas.
    1403TX-400_Caverns-of-Sonora_Texas.jpg
  • Abstract ceiling pattern in Caverns of Sonora, Sutton County, Texas, USA. The world-class Caverns of Sonora have a stunning and sparkling array of speleothems (helictites, stalactites, stalagmites, flowstone, coral trees, and other calcite crystal formations). National Speleological Society co-founder, Bill Stephenson said, after seeing it for the first time, "The beauty of Caverns of Sonora cannot be exaggerated...not even by a Texan!" Geologically, the cave formed between 1.5 to 5 million years ago within 100-million-year-old (Cretaceous) Segovia limestone, of the Edward limestone group. A fault allowed gases to rise up to mix with aquifer water, making acid which dissolved the limestone, leaving the cave. Between 1 and 3 million years ago, the water drained from the cave, after which speleothems begain forming. It is one of the most active caves in the world, with over 95% of its formations still growing. Sonora Caves are on Interstate 10, about half-way between Big Bend National Park and San Antonio, Texas.
    1403TX-378_Caverns-of-Sonora_Texas.jpg
  • Abstract pattern in Caverns of Sonora, Sutton County, Texas, USA. The world-class Caverns of Sonora have a stunning and sparkling array of speleothems (helictites, stalactites, stalagmites, flowstone, coral trees, and other calcite crystal formations). National Speleological Society co-founder, Bill Stephenson said, after seeing it for the first time, "The beauty of Caverns of Sonora cannot be exaggerated...not even by a Texan!" Geologically, the cave formed between 1.5 to 5 million years ago within 100-million-year-old (Cretaceous) Segovia limestone, of the Edward limestone group. A fault allowed gases to rise up to mix with aquifer water, making acid which dissolved the limestone, leaving the cave. Between 1 and 3 million years ago, the water drained from the cave, after which speleothems begain forming. It is one of the most active caves in the world, with over 95% of its formations still growing. Sonora Caves are on Interstate 10, about half-way between Big Bend National Park and San Antonio, Texas.
    1403TX-334_Caverns-of-Sonora_Texas.jpg
  • Abstract helictite pattern in Caverns of Sonora, Sutton County, Texas, USA. The world-class Caverns of Sonora have a stunning and sparkling array of speleothems (helictites, stalactites, stalagmites, flowstone, coral trees, and other calcite crystal formations). National Speleological Society co-founder, Bill Stephenson said, after seeing it for the first time, "The beauty of Caverns of Sonora cannot be exaggerated...not even by a Texan!" Geologically, the cave formed between 1.5 to 5 million years ago within 100-million-year-old (Cretaceous) Segovia limestone, of the Edward limestone group. A fault allowed gases to rise up to mix with aquifer water, making acid which dissolved the limestone, leaving the cave. Between 1 and 3 million years ago, the water drained from the cave, after which speleothems begain forming. It is one of the most active caves in the world, with over 95% of its formations still growing. Sonora Caves are on Interstate 10, about half-way between Big Bend National Park and San Antonio, Texas.
    1403TX-305_Caverns-of-Sonora_Texas.jpg
  • Abstract helictite pattern in Caverns of Sonora, Sutton County, Texas, USA. The world-class Caverns of Sonora have a stunning and sparkling array of speleothems (helictites, stalactites, stalagmites, flowstone, coral trees, and other calcite crystal formations). National Speleological Society co-founder, Bill Stephenson said, after seeing it for the first time, "The beauty of Caverns of Sonora cannot be exaggerated...not even by a Texan!" Geologically, the cave formed between 1.5 to 5 million years ago within 100-million-year-old (Cretaceous) Segovia limestone, of the Edward limestone group. A fault allowed gases to rise up to mix with aquifer water, making acid which dissolved the limestone, leaving the cave. Between 1 and 3 million years ago, the water drained from the cave, after which speleothems begain forming. It is one of the most active caves in the world, with over 95% of its formations still growing. Sonora Caves are on Interstate 10, about half-way between Big Bend National Park and San Antonio, Texas.
    1403TX-417_Caverns-of-Sonora_Texas.jpg
  • Abstract puff-ball pattern in Caverns of Sonora, Sutton County, Texas, USA. The world-class Caverns of Sonora have a stunning and sparkling array of speleothems (helictites, stalactites, stalagmites, flowstone, coral trees, and other calcite crystal formations). National Speleological Society co-founder, Bill Stephenson said, after seeing it for the first time, "The beauty of Caverns of Sonora cannot be exaggerated...not even by a Texan!" Geologically, the cave formed between 1.5 to 5 million years ago within 100-million-year-old (Cretaceous) Segovia limestone, of the Edward limestone group. A fault allowed gases to rise up to mix with aquifer water, making acid which dissolved the limestone, leaving the cave. Between 1 and 3 million years ago, the water drained from the cave, after which speleothems begain forming. It is one of the most active caves in the world, with over 95% of its formations still growing. Sonora Caves are on Interstate 10, about half-way between Big Bend National Park and San Antonio, Texas.
    1403TX-383_Caverns-of-Sonora_Texas.jpg
  • Orange and white sandstone erodes into abstract patterns in Zion National Park adjoins Springdale, Utah, USA.
    11UT1-2170_Zion-NP-Utah.jpg
  • Flowstone forms abstract shapes in Mammoth Cave National Park, which was established in 1941 in Edmonson County, Kentucky, USA and was declared a UNESCO World Heritage Site in 1981 and international Biosphere Reserve 1990. With over 390 miles (630 km) of passageways, the Mammoth-Flint Ridge Cave System is the longest known in the world. Mammoth Cave developed in thick Mississippian-aged limestone strata capped by a layer of Big Clifty Sandstone. Descending limestone layers include the Girkin Formation, Saint Genevieve Limestone, and Saint Louis Limestone.
    10MAM-062.jpg
  • Abstract concrete: broken cement and rebar skeleton of former industry decays in Anacortes, on Fidalgo Island in Skagit County, Washington, USA. From 1892-1930s, the site hosted sawmills and a box factory, followed by the Anacortes Veneer mill in 1939, becoming Custom Plywood from 1962-1990s, until destroyed by fire. A few years after this 2005 photo was taken, a clean-up from 2011-2013 ecologically restored the site back to coastal marsh. Changing economic cycles have brought the area back to nature.
    05WHI-20105.jpg
  • A colorful abstract pattern of 250 million-year-old Grindelwald limestone is exposed in a tunnel of the boardwalk within Gletscherschlucht along the White Lütschine river gorge, in Grindelwald, Switzerland, Europe. The Lower Grindelwald Glacier last extended through Gletscherschlucht gorge in 1855 and has receded very rapidly, melting back more than 3.75 kilometers as of 2014. Consistent with a pattern global warming, the glacier may entirely disappear by 2100. From Gletscherschlucht hotel restaurant, a wooden walkway leads over raging water through galleries and rocky tunnels over 1000 meters into the ravine, under 100-meter-high cliffs. You can walk to Gletscherschlucht in 35 minutes from the center of Grindelwald or take the bus.
    16SWIC-607.jpg
  • Explore the beautiful slot of Ding Canyon on BLM land in the San Rafael Swell, near Goblin Valley State Park, Utah, USA. As part of the Colorado Plateau, the San Rafael Swell is a giant dome-shaped anticline of sandstone, shale, and limestone (160-175 million years old) that was pushed up during the Paleocene Laramide Orogeny 60-40 million years ago. Since then, infrequent but powerful flash floods have eroded the sedimentary rocks into valleys, canyons, gorges, mesas, and buttes. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0780_Ding-Canyon.jpg
  • Explore the beautiful slot of Ding Canyon on BLM land in the San Rafael Swell, near Goblin Valley State Park, Utah, USA. As part of the Colorado Plateau, the San Rafael Swell is a giant dome-shaped anticline of sandstone, shale, and limestone (160-175 million years old) that was pushed up during the Paleocene Laramide Orogeny 60-40 million years ago. Since then, infrequent but powerful flash floods have eroded the sedimentary rocks into valleys, canyons, gorges, mesas, and buttes. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0777_Ding-Canyon.jpg
  • A colorful abstract pattern of 250 million-year-old Grindelwald limestone is exposed along the boardwalk within Gletscherschlucht in the White Lütschine river gorge, in Grindelwald, Switzerland, Europe. The Lower Grindelwald Glacier last extended through Gletscherschlucht gorge in 1855 and has receded very rapidly, melting back more than 3.75 kilometers as of 2014. Consistent with a pattern global warming, the glacier may entirely disappear by 2100. From Gletscherschlucht hotel restaurant, a wooden walkway leads over raging water and through galleries and rocky tunnels over a kilometer into the cool ravine, beneath 100-meter-high cliffs. You can walk to Gletscherschlucht in 35 minutes from the center of Grindelwald or take the bus.
    16SWIC-592.jpg
  • A colorful abstract pattern of 250 million-year-old Grindelwald limestone is exposed along the boardwalk within Gletscherschlucht in the White Lütschine river gorge, in Grindelwald, Switzerland, Europe. The Lower Grindelwald Glacier last extended through Gletscherschlucht gorge in 1855 and has receded very rapidly, melting back more than 3.75 kilometers as of 2014. Consistent with a pattern global warming, the glacier may entirely disappear by 2100. From Gletscherschlucht hotel restaurant, a wooden walkway leads over raging water and through galleries and rocky tunnels over a kilometer into the cool ravine, beneath 100-meter-high cliffs. You can walk to Gletscherschlucht in 35 minutes from the center of Grindelwald or take the bus.
    16SWI-6246.jpg
  • Scottish Parliament Building was opened 2004 in the Holyrood area of the capital city of Scotland, Edinburgh, in the United Kingdom, Europe. The abstract modernist structure was designed by Catalan architect Enric Miralles (1955–2000). Scottish Parliament had previously dropped out of existence from 1707 through 1999. The original Parliament of Scotland was the national legislature of the independent Kingdom of Scotland, existing from the early 1200s until the Kingdom of Scotland merged with the Kingdom of England under the Acts of Union 1707 to form the Kingdom of Great Britain. Scottish Parliament disappeared with the creation of the Parliament of Great Britain at Westminster in London. Following a Scottish referendum in 1997, the current Parliament was convened by the Scotland Act 1998, which sets out its powers as a devolved legislature, which first met in 1999. The Scottish Parliament has the power to legislate in all areas that are not explicitly reserved to Westminster.
    17SC1-4453_Scotland.jpg
  • Scottish Parliament Building was opened 2004 in the Holyrood area of the capital city of Scotland, Edinburgh, in the United Kingdom, Europe. The abstract modernist structure was designed by Catalan architect Enric Miralles (1955–2000). Scottish Parliament had previously dropped out of existence from 1707 through 1999. The original Parliament of Scotland was the national legislature of the independent Kingdom of Scotland, existing from the early 1200s until the Kingdom of Scotland merged with the Kingdom of England under the Acts of Union 1707 to form the Kingdom of Great Britain. Scottish Parliament disappeared with the creation of the Parliament of Great Britain at Westminster in London. Following a Scottish referendum in 1997, the current Parliament was convened by the Scotland Act 1998, which sets out its powers as a devolved legislature, which first met in 1999. The Scottish Parliament has the power to legislate in all areas that are not explicitly reserved to Westminster.
    17SC1-4445_Scotland.jpg
  • A colorful abstract pattern of 250 million-year-old Grindelwald limestone is exposed along the boardwalk within Gletscherschlucht in the White Lütschine river gorge, in Grindelwald, Switzerland, Europe. The Lower Grindelwald Glacier last extended through Gletscherschlucht gorge in 1855 and has receded very rapidly, melting back more than 3.75 kilometers as of 2014. Consistent with a pattern global warming, the glacier may entirely disappear by 2100. From Gletscherschlucht hotel restaurant, a wooden walkway leads over raging water and through galleries and rocky tunnels over a kilometer into the cool ravine, beneath 100-meter-high cliffs. You can walk to Gletscherschlucht in 35 minutes from the center of Grindelwald or take the bus.
    16SWIC-606.jpg
  • A colorful abstract pattern of 250 million-year-old Grindelwald limestone is exposed along the boardwalk within Gletscherschlucht in the White Lütschine river gorge, in Grindelwald, Switzerland, Europe. The Lower Grindelwald Glacier last extended through Gletscherschlucht gorge in 1855 and has receded very rapidly, melting back more than 3.75 kilometers as of 2014. Consistent with a pattern global warming, the glacier may entirely disappear by 2100. From Gletscherschlucht hotel restaurant, a wooden walkway leads over raging water and through galleries and rocky tunnels over a kilometer into the cool ravine, beneath 100-meter-high cliffs. You can walk to Gletscherschlucht in 35 minutes from the center of Grindelwald or take the bus.
    16SWIC-595.jpg
  • A colorful abstract pattern of 250 million-year-old Grindelwald limestone is exposed along the boardwalk within Gletscherschlucht in the White Lütschine river gorge, in Grindelwald, Switzerland, Europe. The Lower Grindelwald Glacier last extended through Gletscherschlucht gorge in 1855 and has receded very rapidly, melting back more than 3.75 kilometers as of 2014. Consistent with a pattern global warming, the glacier may entirely disappear by 2100. From Gletscherschlucht hotel restaurant, a wooden walkway leads over raging water and through galleries and rocky tunnels over a kilometer into the cool ravine, beneath 100-meter-high cliffs. You can walk to Gletscherschlucht in 35 minutes from the center of Grindelwald or take the bus.
    16SWIC-594.jpg
  • A colorful abstract pattern of 250 million-year-old Grindelwald limestone is exposed along the boardwalk within Gletscherschlucht in the White Lütschine river gorge, in Grindelwald, Switzerland, Europe. The Lower Grindelwald Glacier last extended through Gletscherschlucht gorge in 1855 and has receded very rapidly, melting back more than 3.75 kilometers as of 2014. Consistent with a pattern global warming, the glacier may entirely disappear by 2100. From Gletscherschlucht hotel restaurant, a wooden walkway leads over raging water and through galleries and rocky tunnels over a kilometer into the cool ravine, beneath 100-meter-high cliffs. You can walk to Gletscherschlucht in 35 minutes from the center of Grindelwald or take the bus.
    16SWI-6245.jpg
  • A white dike intrudes into blue-gray rock forming an abstract tree shape with yellow lichen suggesting leaves. My favorite hike in the Bishop Creek watershed goes from South Lake to Long Lake and Saddlerock Lake, looping back via a steeper, poorly marked route to Ruwau Lake, Chocolate Lakes, and Bull Lake, in John Muir Wilderness, Inyo National Forest, Sierra Nevada, California, USA. The rewarding semi-loop is 9 miles with 2220 feet cumulative gain. An easier walk is 7.2 miles round trip with 1500 feet gain to Saddlerock Lake, out and back via beautiful Long Lake.
    1507CAL-5106.jpg
  • Glass reflecting an abstract pattern of cumulus clouds obscures rows of bottles seen behind. These prominent windows front the finest home in Bodie, owned by James Stuart Cain from the 1890s - 1940s. Bodie is now California's official state gold rush ghost town. Jessie McGath originally built this house for his new wife in 1879, and JS Cain bought it in the 1890s. Cain moved to Bodie when he was 25 and built an empire starting with putting lumber barges on Mono Lake and transporting timber to support mine shafts, stoke boilers for machinery, build & heat buildings, and cook food. Cain eventually took control of the Stamp Mill though court action and went on to be the principal property owner and one of the richest men in town. Bodie State Historic Park lies in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, near Bridgeport, California, USA. After W. S. Bodey's original gold discovery in 1859, profitable gold ore discoveries in 1876 and 1878 transformed "Bodie" from an isolated mining camp to a Wild West boomtown. By 1879, Bodie had a population of 5000-7000 people with 2000 buildings. At its peak, 65 saloons lined Main Street, which was a mile long. Bodie declined rapidly 1912-1917 and the last mine closed in 1942. Bodie became a National Historic Landmark in 1961 and Bodie State Historic Park in 1962. This image was stitched from two photos to increase pixel count and potential print size.
    1507CAL-2563-64pan_Bodie-CA.jpg
  • A white salt crust forms an abstract pattern over orange-red sandstone in Crack Canyon, in San Rafael Swell, near Goblin Valley State Park, Utah, USA.
    1503SW3-055_Crack-Canyon_pattern.jpg
  • Scottish Parliament Building was opened 2004 in the Holyrood area of the capital city of Scotland, Edinburgh, in the United Kingdom, Europe. The abstract modernist structure was designed by Catalan architect Enric Miralles (1955–2000). Scottish Parliament had previously dropped out of existence from 1707 through 1999. The original Parliament of Scotland was the national legislature of the independent Kingdom of Scotland, existing from the early 1200s until the Kingdom of Scotland merged with the Kingdom of England under the Acts of Union 1707 to form the Kingdom of Great Britain. Scottish Parliament disappeared with the creation of the Parliament of Great Britain at Westminster in London. Following a Scottish referendum in 1997, the current Parliament was convened by the Scotland Act 1998, which sets out its powers as a devolved legislature, which first met in 1999. The Scottish Parliament has the power to legislate in all areas that are not explicitly reserved to Westminster.
    17SC1-4443_Scotland.jpg
  • A colorful abstract pattern of 250 million-year-old Grindelwald limestone is exposed along the boardwalk within Gletscherschlucht in the White Lütschine river gorge, in Grindelwald, Switzerland, Europe. The Lower Grindelwald Glacier last extended through Gletscherschlucht gorge in 1855 and has receded very rapidly, melting back more than 3.75 kilometers as of 2014. Consistent with a pattern global warming, the glacier may entirely disappear by 2100. From Gletscherschlucht hotel restaurant, a wooden walkway leads over raging water and through galleries and rocky tunnels over a kilometer into the cool ravine, beneath 100-meter-high cliffs. You can walk to Gletscherschlucht in 35 minutes from the center of Grindelwald or take the bus.
    16SWIC-596.jpg
  • A colorful abstract pattern of 250 million-year-old Grindelwald limestone is exposed along the boardwalk within Gletscherschlucht in the White Lütschine river gorge, in Grindelwald, Switzerland, Europe. The Lower Grindelwald Glacier last extended through Gletscherschlucht gorge in 1855 and has receded very rapidly, melting back more than 3.75 kilometers as of 2014. Consistent with a pattern global warming, the glacier may entirely disappear by 2100. From Gletscherschlucht hotel restaurant, a wooden walkway leads over raging water and through galleries and rocky tunnels over a kilometer into the cool ravine, beneath 100-meter-high cliffs. You can walk to Gletscherschlucht in 35 minutes from the center of Grindelwald or take the bus. (This image has been rotated 90 degrees counterclockwise for artistic effect.)
    16SWIC-593.jpg
  • Flash floods have eroded a slot of Navajo sandstone into a natural cathedral at Lower Antelope Canyon, in Antelope Canyon Navajo Tribal Park, near Page, Arizona, USA. (The older spelling "Navaho" is no longer used by the Navajo, an American Indian group who call themselves Diné, or Dineh, "The People.") For licensing options, please inquire.
    06AZ_5073-Lower_Antelope_Canyon.jpg
  • Lower Antelope Canyon (or "the Corkscrew") is a beautiful slot canyon in Antelope Canyon Navajo Tribal Park, near Page, Arizona, USA. Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. Flash floods and other erosion have carved Navajo Sandstone into this natural rock cathedral.
    11AZ1-2245_Lower-Antelope-Canyon.jpg
  • The Wave, Coyote Buttes, located on the Arizona side of Paria Canyon-Vermilion Cliffs Wilderness Area, which is public land managed by the United States BLM. Over 190 million years, ancient sand dune layers calcified into rock and created "The Wave." Iron oxides bled through this Jurassic-age Navajo sandstone to create the salmon color. Hematite and goethite added yellows, oranges, browns and purples. Over thousands of years, water cut through the ridge above and exposed a channel that was further scoured by windblown sand into the smooth curves that today look like ocean swells and waves. For the permit required to hike to "The Wave", contact the US Bureau of Land Management (BLM), who limits access to protect this fragile geologic formation. Image was published in 2009 for a surgeon's book on the intersection of science and faith. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    03AZ-05-25-The-Wave_Coyote-Buttes.jpg
  • Explore colorful fossilized sand dunes in the Paw Hole section of South Coyote Buttes, in Vermilion Cliffs National Monument, Arizona, USA. The Coyote Buttes area exposes cross-bedded aeolian Jurassic Navajo Sandstone. Various iron oxides bled through the sandstone layers to create a salmon color; hematite and goethite added yellows, oranges, browns, and purples. For the required hiking permit, contact the US Bureau of Land Management (BLM, in Kanab, Utah). Access to this Federal public land is regulated to protect fragile geologic formations. Coyote Buttes are within Vermilion Cliffs National Monument (established in 2000 within Arizona), which is within Paria Canyon-Vermilion Cliffs Wilderness Area (established in 1984 spanning across the borders of Utah and Arizona). Stitched from two photos to increase depth of focus. The image was stitched from 2 overlapping photos to increase depth of focus.
    1303AZ-1361-1362stit.jpg
  • Hikers walk a dog along a rock face near Northgate Peaks trail, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1053.jpg
  • Dunes rise up to 750 feet tall in Great Sand Dunes National Park and Preserve, on the eastern edge of San Luis Valley, Sangre de Cristo Range, south-central Colorado, USA.
    1909US1-2482.jpg
  • Flash floods have eroded a slot of Navajo sandstone into a natural cathedral at Lower Antelope Canyon, in Antelope Canyon Navajo Tribal Park, near Page, Arizona, USA. (The older spelling "Navaho" is no longer used by the Navajo, an American Indian group who call themselves Diné, or Dineh, "The People.")
    06AZ_4138-Lower_Antelope_Canyon.jpg
  • Lower Antelope Canyon (or "the Corkscrew") is a beautiful slot canyon in Antelope Canyon Navajo Tribal Park, near Page, Arizona, USA. Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. Flash floods and other erosion have carved Navajo Sandstone into this natural rock cathedral.
    11AZ1-2236-37pan_Lower-Antelope-Cany...jpg
  • Lower Antelope Canyon (or "the Corkscrew") is a beautiful slot canyon in Antelope Canyon Navajo Tribal Park, near Page, Arizona, USA. Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. Flash floods and other erosion have carved Navajo Sandstone into this natural rock cathedral.
    11AZ3C-5042_Lower-Antelope-Canyon.jpg
  • Exterior facade, glass window patttern. Seattle Public Library, designed by Dutch architect Rem Koolhaas, finished in 2004. Address: 1000 Fourth Ave, Seattle, Washington 98164, USA.
    04LIB-015-outside-tree-wall-pattern.jpg
  • Lower Antelope Canyon (or "the Corkscrew") is a beautiful slot canyon in Antelope Canyon Navajo Tribal Park, near Page, Arizona, USA. Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. Flash floods and other erosion have carved Navajo Sandstone into this natural rock cathedral.
    11AZ3C-5071_Lower-Antelope-Canyon.jpg
  • Lower Antelope Canyon (or "the Corkscrew") is a beautiful slot canyon in Antelope Canyon Navajo Tribal Park, near Page, Arizona, USA. Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. Flash floods and other erosion have carved Navajo Sandstone into this natural rock cathedral.
    11AZ1-2202_Lower-Antelope-Canyon.jpg
  • Lower Antelope Canyon (or "the Corkscrew") is a beautiful slot canyon in Antelope Canyon Navajo Tribal Park, near Page, Arizona, USA. Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. Flash floods and other erosion have carved Navajo Sandstone into this natural rock cathedral.
    11AZ1-2190_Lower-Antelope-Canyon.jpg
  • Copper pattern in a rock. The Arizona-Sonora Desert Museum is a 98-acre zoo, aquarium, botanical garden, natural history museum, publisher, and art gallery founded in 1952. It's just west of Tucson, Arizona, USA.
    23AZ-502.jpg
  • Red and orange alpine moonscape on Akamina Ridge, in Akamina-Kishinena Provincial Park, British Columbia, Canada. The loop hike to Forum and Wall Lakes via Akamina Ridge is 12 miles with 3440 feet ascent & descent. The trailhead is in Alberta, accessible by road from Waterton Park.
    2209RV-1123.jpg
  • Rock pattern vista at Comeau Pass, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0563.jpg
  • Rock pattern. Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0546.jpg
  • Refuge du Requin, Mer de Glace, Mont Blanc Massif, seen from Télécabine Panoramic Mont-Blanc cable car in France, Europe. The "Télécabine Panoramic Mont-Blanc" cable car crosses 5 kilometers of the Mont Blanc Massif in France from Aiguille du Midi to Pointe Helbronner. To reach Pointe Helbronner, we used Skyway Monte Bianco cable car, where the top platform splits the border between Italy & France, and the bottom station is in La Palud village just north of Courmayeur in the Aosta Valley, Italy.
    22ALP-04281.jpg
  • Invasive iceplant at Leffingwell Landing Park, part of Hearst San Simeon State Park, Cambria, California, USA. Iceplant was introduced to California in the early 1900s as an erosion stabilization tool beside railroad tracks, and later used by Caltrans on roadsides. Iceplant is bad for a number of reasons. It’s invasive and releases salt into the soil, raising the salt level high enough to inhibit other plant seeds, especially grasses.  It doesn't serve as a food source for animals and can out-compete the native plants for water, light, and space. It's actually bad for erosion control. Having weak root systems, these heavy plants can cause the hill to start sliding, taking existing topsoil from the slope. Although the soft succulent new growth has a high water content which doesn't burn, the slow-to-decompose dead leaves layered underneath create a fire hazard.
    2203CA-0451.jpg
  • Copper pattern in a rock. The Arizona-Sonora Desert Museum is a 98-acre zoo, aquarium, botanical garden, natural history museum, publisher, and art gallery founded in 1952. It's just west of Tucson, Arizona, USA.
    23AZ-504.jpg
  • Orange breast feathers of an endangered masked bobwhite quail. Arizona-Sonora Desert Museum, Tucson, Arizona, USA. The Arizona-Sonora Desert Museum is a 98-acre zoo, aquarium, botanical garden, natural history museum, publisher, and art gallery founded in 1952.
    23AZ-425.jpg
  • Octopus agave (Agave vilmoriniana). Arizona-Sonora Desert Museum, Tucson, Arizona, USA. The Arizona-Sonora Desert Museum is a 98-acre zoo, aquarium, botanical garden, natural history museum, publisher, and art gallery founded in 1952.
    23AZ-287.jpg
  • Garden Wall hike at Logan Pass, Glacier National Park, Montana, USA
    2209RV-0008.jpg
  • From Akamina Ridge in Canada, see blue ridges of Glacier National Park located in the United States. The loop hike to Forum and Wall Lakes via Akamina Ridge in Akamina-Kishinena Provincial Park (British Columbia, Canada) is 12 miles with 3440 feet ascent & descent. The trailhead is in Alberta, accessible by road from Waterton Park.
    2209RV-1021.jpg
  • Ancient seabed ripples in Akamina-Kishinena Provincial Park, British Columbia, Canada. The loop hike to Forum and Wall Lakes via Akamina Ridge is 12 miles with 3440 feet ascent & descent. The trailhead is in Alberta, accessible by road from Waterton Park.
    2209RV-1003.jpg
  • Orange rock pattern with yellow lichen. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0894.jpg
  • Orange rock pattern with yellow lichen. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0892.jpg
  • Orange & blue rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0867.jpg
  • Orange and blue striped rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0837.jpg
  • Red, orange, & white rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0767.jpg
  • Red, orange, & white rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0766.jpg
  • Yellow lichen pattern on orange rock. Gunsight Pass Trail, Glacier National Park, Montana, USA
    2209RV-0724.jpg
  • Broken purple boulders, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0646.jpg
  • Ancient fossilized orange & purple seabed ripples at Comeau Pass, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0582.jpg
  • Rock pattern vista at Comeau Pass, Sperry Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0572.jpg
  • Rock pattern, Gunsight Pass, Glacier National Park, Montana, USA
    2209RV-0411.jpg
  • Rime ice on pine needles at Gunsight Pass, Glacier National Park, Montana, USA
    2209RV-0404.jpg
  • A stream descends strikingly striated rock layers above Gunsight Lake, in Glacier National Park, Montana, USA
    2209RV-0376.jpg
  • Borer beetle tracks, Gunsight Pass Trail, Glacier National Park, Montana, USA
    2209RV-0324.jpg
  • Rock pattern, seen on the hike to Dragon's Tail ridge, starting from Hidden Lake Traihead at Logan Pass, in Glacier National Park, Montana, USA
    2209RV-0243.jpg
  • Rock pattern, seen on the hike to Dragon's Tail ridge, starting from Hidden Lake Traihead at Logan Pass, in Glacier National Park, Montana, USA
    2209RV-0224.jpg
  • Rock pattern, seen on the hike to Dragon's Tail ridge, starting from Hidden Lake Traihead at Logan Pass, in Glacier National Park, Montana, USA
    2209RV-0208.jpg
  • Rock pattern, seen on the hike to Dragon's Tail ridge, starting from Hidden Lake Traihead at Logan Pass, in Glacier National Park, Montana, USA
    2209RV-0205.jpg
  • Rock pattern, seen on the hike to Dragon's Tail ridge, starting from Hidden Lake Traihead at Logan Pass, in Glacier National Park, Montana, USA
    2209RV-0193.jpg
  • Rock pattern, seen on the hike to Dragon's Tail ridge, starting from Hidden Lake Traihead at Logan Pass, in Glacier National Park, Montana, USA
    2209RV-0184.jpg
  • Rock pattern, Logan Pass, Glacier National Park, Montana, USA
    2209RV-0065.jpg
  • Green rock pattern, Logan Pass, Glacier National Park, Montana, USA
    2209RV-0054.jpg
  • Trümmelbach Falls (German: Trümmelbachfälle) are a series of ten glacier-fed waterfalls inside the mountain made accessible by a tunnel-funicular (built in 1913), stairs, and illumination, in Lauterbrunnen, Switzerland, Europe. In the Lauterbrunnen Valley, the creek called Trümmelbach drains the northerly glaciers of the Eiger (3967 m), Mönch (4099 m), and Jungfrau (4158 m) peaks.
    22ALP-11430.jpg
  • The Eiger at sunset seen from Hotel Gletschergarten in Grindelwald, Switzerland, Europe.
    22ALP-10133.jpg
  • Swiss Via Alpina 1: sharp blue ridges of the Alps seen from atop Mt. Titlis, near Engelberg, Switzerland, Europe. In Engelberg, we rode the Titlis lift, the world's first rotating cable car. The Titlis cable car system connects Engelberg (996 m or 3,268 ft) to the summit of Klein Titlis (3,028 m or 9,934 ft) via stations at Trübsee and Stand. At Klein Titlis, we visited the illuminated Glacier Cave and Titlis Cliff Walk, the highest elevation suspension bridge in Europe, opened in December 2012, giving views across the Alps. We enjoyed walking 2 miles around scenic Trübsee, a circuit where six play stations for kids make an ideal family excursion, suitable for strollers. Scheduling 3 nights in Engelberg provided a well-needed rest break in the middle of hiking the first ten stages of the Swiss Via Alpina (National Route 1).
    22ALP-08598.jpg
  • Swiss Via Alpina 1, Day 5: views on descent from Surenenpass to Fürenalp, near Engelberg, Switzerland, Europe. Swiss Via Alpina (National Route 1), Day 5: From Altdorf, we rode the PostBus to Attinghausen Seilbahn, a cable car which ascends to Brüsti, from where we hiked over Surenenpass to Fürenalp cable car (8.8 miles, 3360 feet up, 2340 ft down), which we rode plus PostBus to reach Hotel Sonnwendhof in Engelberg.
    22ALP-08411.jpg
  • Anemone seed head. TMB trek Day 6: hike from Bonatti Refuge in Italy > La Fouly, Switzerland, Europe
    20220710_082813.jpg
  • Sunset at Bonatti Refuge in Val Ferret, Italy, the Alps, Europe. Tour du Mont Blanc (TMB) trek Day 5: I hiked from Courmayeur via the Mont de la Saxe option to Walter Bonatti Refuge (10 miles with 5200 feet ascent, 2700 ft descent) (whereas the standard TMB route hiked separately by Carol was 8 miles with 3300 ft up, 700 ft down).
    22ALP-05006.jpg
  • Rock pattern below Col de la Seigne, Val Veny, Italy, Europe. Tour du Mont Blanc (TMB) trek Day 3: hike from Les Chapieux in France via Col de la Seigne to Elisabetta Refuge in Val Veny, Italy (8.8 miles miles with 3450 feet ascent, 1440 ft descent).
    22ALP-03020.jpg
  • Lichen pattern. Hike the Grand North Balcony from Plan de l'Aiguille to Montenvers, above Chamonix, in France, Europe (4.3 miles one way with 2000 feet vertical ascent and 700 ft descent).
    22ALP-02168.jpg
  • Eroded sandstone. Leffingwell Landing Park, part of Hearst San Simeon State Park, Cambria, California, USA
    2203CA-0467.jpg
  • Rock pattern. Estero Bluffs State Park, Cayucos, California.
    2203CA-0420.jpg
  • Turkey feathers reflect a rainbow of colors. Pinnacles Campground, Pinnacles National Park, California, USA
    2203CA-0370.jpg
  • Atop Pinnacles National Park on the High Peaks loop (5.4 miles, 1650 ft gain). California, USA
    2203CA-0198.jpg
  • Bear Gulch Cave Trail. Pinnacles National Park, California, USA
    2203CA-0046.jpg
  • Bear Gulch Cave Trail. Pinnacles National Park, California, USA
    2203CA-0044.jpg
  • Sycamore tree bark. Madera Canyon, Santa Rita Mountains, Coronado National Forest, near Green Valley, Arizona, USA.
    23AZ-071.jpg
  • Fungus on a log. Madera Canyon, Santa Rita Mountains, Coronado National Forest, near Green Valley, Arizona, USA.
    23AZ-063.jpg
  • Orange rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0897.jpg
  • Orange rock pattern. Grinnell Glacier Trail, Glacier National Park, Montana, USA
    2209RV-0889.jpg
Next
  • Facebook
  • Twitter
x

Portfolio of Tom Dempsey / PhotoSeek.com

  • Portfolio
  • BLOG — PhotoSeek HOME
  • ALL IMAGES + captions
    • Worldwide favorites
    • ALL GALLERIES
    • Lightbox
  • SEARCH
  • CART
  • How to buy my images
  • Camera reviews
  • ABOUT