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)
{ 1296 images found }

Loading ()...

  • Wavy greenish rock pattern, Logan Pass, Glacier National Park, Montana, USA
    2209RV-0033.jpg
  • Pfeiffer Falls. Pfeiffer Big Sur State Park, California, USA. On the western slope of the Santa Lucia Mountains, the peaks of Pfeiffer Big Sur State Park tower high above the Big Sur River Gorge, where the Big Sur River enters this popular park. Walk along the banks of the river and among the redwoods, conifers, oaks, sycamores, cottonwoods, maples, alders and willows. Big Sur is the southern limit of Coastal Redwoods in North America.
    2203CA-0754.jpg
  • Orange sunset along the Big Sur coast, California, USA
    2203CA-0653.jpg
  • In Saas-Fee, we enjoyed sightseeing on the Spielboden-Längfluh lift. Saas-Fee is the main village in the Saastal, (Saas Valley), in the district of Visp, canton of Valais, in Switzerland, Europe. The village perches on a high mountain plateau at 1,800 meters (5,900 feet) elevation, surrounded by 13 peaks above 4,000 meters (13,123 feet). This classic ski resort features a car-free city center and well-preserved Swiss wood architecture.
    22ALP-06931.jpg
  • Wood pattern. Ancient Bristlecone Pine Forest, Inyo National Forest, California, USA. The fascinating Methuselah Walk is a loop of 4.1 miles with 705 feet gain.
    2108CA1-569.jpg
  • Smoky blue ridges seen from Palisades Lakes Trail in Mountain Rainier National Park, Washington, USA. We hiked 6.2 miles with 1630 feet gain to Hidden Lake.
    2107WA-062.jpg
  • Petrified red sand ripples along Hance Rapid scouting trail. Day 6 of 16 days rafting 226 miles down the Colorado River in Grand Canyon National Park, Arizona, USA.
    2103SW-C1091.jpg
  • Conglomerate rock pattern in Two Hundred and Twenty Mile Canyon, where we stayed at Middle Camp at Colorado River Mile 220.1. Day 15 of 16 days rafting 226 miles down the Colorado River in Grand Canyon National Park, Arizona, USA.
    2103SW-B1377.jpg
  • Scalloped rock pattern. Day 11 of 16 days rafting 226 miles down the Colorado River in Grand Canyon National Park, Arizona, USA.
    2103SW-C2278.jpg
  • Million-year-old lake sediments have eroded into fantastic mud castles at Cathedral Gorge State Park, Panaca, Nevada, USA.
    2103SW-A1576.jpg
  • Rock patterns along the White Domes Loop Trail in Valley of Fire State Park, near the town of Moapa Valley, Nevada, USA. A great 3.5-mile "spectacle loop" (with 450 feet of gain and loss) starts at Park Turnout #3, goes to the Fire Wave, proceeds along the Seven Wonders Trail through Kaolin Wash, completes the White Domes Trail Loop back to the movie set remains, repeats a quarter mile of Kaolin Wash, turns north on Seven Wonders Trail past Thunderstorm Arch, and returns to Park Turnout #3. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations.
    2103SW-A1318.jpg
  • Rock patterns in Kaolin Wash, Valley of Fire State Park, near Moapa Valley, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations.
    2103SW-A1309.jpg
  • Sandstone rock patterns in Kaolin Wash, Valley of Fire State Park, near Moapa Valley, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations.
    2103SW-A1303.jpg
  • Sandstone rock patterns in Kaolin Wash, Valley of Fire State Park, near Moapa Valley, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations.
    2103SW-A1254.jpg
  • Sandstone rock patterns in Kaolin Wash, Valley of Fire State Park, near Moapa Valley, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations.
    2103SW-A1236.jpg
  • Sandstone rock patterns in Kaolin Wash, Valley of Fire State Park, near Moapa Valley, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations.
    2103SW-A1223.jpg
  • The Fire Wave in Valley of Fire State Park, Moapa Valley, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations.
    2103SW-A1183.jpg
  • A concrete spiral stairwell at Battery Russell in Fort Stevens State Park, on the Oregon coast, USA. Fort Stevens operated from 1863–1947 as part of a three-fort American military system defending the Columbia River Mouth. Built near the end of the American Civil War, this American military installation was named for a slain Civil War general and former Washington Territory governor, Isaac I. Stevens. In June 1942 during World War II, a Japanese submarine fired 17 rounds upon Fort Stevens (luckily causing causing no real damage), making it the only military base on the Continental United States to be fired upon by an enemy since the War of 1812.
    2102OR2-037.jpg
  • Colorful seaside rock patterns near Seal Rock State Recreation Site, on the Oregon coast, USA. We stayed at the adjacent Seal Rocks RV Cove.
    2102OR2-923.jpg
  • Glacier-scoured rock pattern near Burro Pass, in Hoover Wilderness of Humboldt-Toiyabe National Forest, Eastern Sierra Nevada, Mono County, California, USA.
    2007CA-2753.jpg
  • Sky and mountains lit by sunset reflect in a wavy pond south of Nutter Lake in Hoover Wilderness of Humboldt-Toiyabe National Forest, Eastern Sierra Nevada, Mono County, California, USA.
    2007CA-2418.jpg
  • Yellow green and purple rock pattern along the trail to Shadow Lake (7.5 miles, 1200 ft gain) in Ansel Adams Wilderness, Inyo National Forest, Sierra Nevada, Mammoth Lakes village, California, USA.
    2007CA-1208.jpg
  • Cracked pattern mud near Ben Reifel Visitor Center in Badlands National Park, South Dakota, USA. The intricately carved cliff of the Badlands Wall constantly retreats as it erodes and washes into the White River Valley below.
    20.10US1-0600.jpg
  • Colorful wavy sandstone layers are revealed in the slot of Little Wild Horse Canyon. San Rafael Swell Recreation Area, Utah, USA. Hike a classic loop from Little Wild Horse Canyon to Bell Canyon, in the San Rafael Reef. This great walk (an 8.6-mile circuit with 900 feet gain) is a short drive on a paved road from Goblin Valley State Park. The hike via fascinating narrow slot canyons and open mesas requires some scrambling over rocks, possibly through shallow water holes (which were dry for us on Sept 20, 2020 but wet in April 2006). Thanks to the greatest legislative victory in the history of SUWA (Southern Utah Wilderness Alliance), in 2019, Congress passed the Emery County Public Land Management Act, which declared 663,000 acres of wilderness, including Little Wild Horse Canyon Wilderness, in San Rafael Swell Recreation Area, Utah, USA. The Navajo and Wingate sandstone of the San Rafael Reef was uplifted fifty million years ago into a striking bluff which now runs from Price to Hanksville, bisected by Interstate 70 at a breach fifteen miles west of the town of Green River.
    20.10US1-0424.jpg
  • Zebra Slot Canyon, Grand Staircase-Escalante National Monument, Utah, USA. From Hole-in-the-Rock Road, hike east on a well-trodden but unmarked path, 5 miles round trip with 450 feet total gain to Zebra Slot.
    20.10US1-0230.jpg
  • A water-carved hole in Peekaboo Gulch in Grand Staircase-Escalante National Monument, Utah, USA. This image was stitched from multiple overlapping photos.
    20.10US1-0064-66-Pano.jpg
  • Scalloped sandstone in Peekaboo Gulch in Grand Staircase-Escalante National Monument, Utah, USA. This image was stitched from multiple overlapping photos.
    20.10US1-0052-54-Pano.jpg
  • Lago Pollone reflects the Pollone Glacier, near El Chalten, in Santa Cruz Province, Argentina, Patagonia, South America. We hiked the scenic Rio Electrico Valley to Refugio Piedra del Fraile ("Stone of the Friar", 14.5 km round trip). From the refuge, a rewarding day hike visits Lago Pollone (8.5 km round trip with 320 m gain).
    2002PAT-3883.jpg
  • The icy blue face of Perito Moreno Glacier melts into Lake Argentino, in Los Glaciares National Park, near El Calafate, Argentina, Patagonia, South America. The spectacular Perito Moreno Glacier is one of 48 glaciers fed by the Southern Patagonian Ice Field (the world's third largest reserve of fresh water). Lago Argentino is the biggest freshwater lake in Argentina and reaches as deep as 500 meters (1640 feet). Its outlet, the Santa Cruz River, flows into the Atlantic Ocean. Despite most glaciers worldwide retreating due to global warming, Perito Moreno Glacier has been a relatively stable exception for the past hundred years. Located 78 kilometers (48 mi) from El Calafate, the glacier was named after explorer Francisco Moreno, a pioneer who studied the region in the 1800s and defended the territory of Argentina in the conflict surrounding the international border dispute with Chile. Los Glaciares National Park is honored on UNESCO's World Heritage List.
    2002PAT-1769.jpg
  • Visit the impressive Marble Chapel Nature Sanctuary (Capillas de Mármol) via popular boat tours from Bahía Manso on General Carrera Lake, near Puerto Rio Tranquilo, Chile, Patagonia, South America. This beautiful Chilean Nature Sanctuary sculpted by water and wind has three main geological formations: the Cathedral, the Chapel, and the Cave. You can join a Marble Caves tour in Puerto Río Tranquilo; or save money and time by driving directly 8 km south to Bahía Manso, via a pot-holed very steep side road, where we spontaneously joined a 2-hour tour boat on short notice. The best time is a sunny summer morning in calmer waters. The side road to Bahía Manso was nervously passable with our 2-wheel-drive compact car, but 4WD might be required to return back up if wet.
    2002PAT-1245.jpg
  • Sandstone rock pattern. In Capitol Reef National Park, we hiked impressive sandstone gorges from Chimney Rock Trailhead over to Spring Canyon and down to a car shuttle at Highway 24 (10 miles one way with 1100 ft descent and 370 ft gain), Torrey, Utah, USA.
    1909US1-8609.jpg
  • Sandstone walls reflect in Spring Canyon in Capitol Reef NP, Torrey, Utah, USA. In Capitol Reef National Park, we hiked impressive sandstone gorges from Chimney Rock Trailhead over to Spring Canyon and down to a car shuttle at Highway 24 (10 miles one way with 1100 ft descent and 370 ft gain).
    1909US1-8863.jpg
  • Aerial view of Carroll Glacier, in Glacier Bay National Park, Alaska, USA. Flightseeing from Skagway or Haines is a spectacular way to see Glacier Bay. We were bedazzled by Mountain Flying Service's 1.3-hour West Arm tour from Skagway. Glacier Bay is honored by UNESCO as part of a huge Biosphere Reserve and World Heritage site shared between Canada and the United States. In 1750-80, Glacier Bay was totally covered by ice, which has since radically melted away. In 1794, Captain George Vancover found Icy Strait on the Gulf of Alaska choked with ice, and all but a 3-mile indentation of Glacier Bay was filled by a huge tongue of the Grand Pacific Glacier, 4000 feet deep and 20 miles wide. By 1879, naturalist John Muir reported that the ice had retreated 48 miles up the bay. In 1890, "Glacier Bay" was named by Captain Beardslee of the U.S. Navy. Over the last 200 years, melting glaciers have exposed 65 miles of ocean. As of 2019, glaciers cover only 27% of the Park area. Since the mid 1900s, Alaska has warmed 3 degrees Fahrenheit and its winters have warmed nearly 6 degrees. Human-caused climate change induced by emissions of greenhouse gases continues to accelerate warming at an unprecedented rate. Climate change is having disproportionate effects in the Arctic, which is heating up twice as fast as the rest of Earth.
    1906AKH-5514.jpg
  • Aerial view of fast-melting Carroll Glacier, in Glacier Bay National Park, Alaska, USA. Flightseeing from Skagway or Haines is a spectacular way to see Glacier Bay. We were bedazzled by Mountain Flying Service's 1.3-hour West Arm tour from Skagway. Glacier Bay is honored by UNESCO as part of a huge Biosphere Reserve and World Heritage site shared between Canada and the United States. In 1750-80, Glacier Bay was totally covered by ice, which has since radically melted away. In 1794, Captain George Vancover found Icy Strait on the Gulf of Alaska choked with ice, and all but a 3-mile indentation of Glacier Bay was filled by a huge tongue of the Grand Pacific Glacier, 4000 feet deep and 20 miles wide. By 1879, naturalist John Muir reported that the ice had retreated 48 miles up the bay. In 1890, "Glacier Bay" was named by Captain Beardslee of the U.S. Navy. Over the last 200 years, melting glaciers have exposed 65 miles of ocean. As of 2019, glaciers cover only 27% of the Park area. Since the mid 1900s, Alaska has warmed 3 degrees Fahrenheit and its winters have warmed nearly 6 degrees. Human-caused climate change induced by emissions of greenhouse gases continues to accelerate warming at an unprecedented rate. Climate change is having disproportionate effects in the Arctic, which is heating up twice as fast as the rest of Earth.
    1906AKH-5371.jpg
  • Crevasses in Mendenhall Glacier. Juneau, Alaska, USA. For spectacular views over Mendenhall Glacier, hike the West Glacier (Mt. McGinnis) Trail 6-9.5 miles round trip, 1000-3200 feet gain, best late May-September. The Trailhead is a half mile from Mendenhall Campground entrance by road. A good trail skirts the northwest side of Mendenhall Lake then climbs through forest to the bare rock along the glacier's west side, where some scrambling and route finding skills are required. Mendenhall Glacier flows 12 miles from downtown Juneau. Mendenhall Glacier Recreation Area is a unit of Tongass National Forest. Mendenhall Glacier has retreated 1.75 miles since 1929, when Mendenhall Lake was created, and over 2.5 miles (4.0 km) since 1500. Since the mid 1900s, Alaska has warmed 3 degrees Fahrenheit and its winters have warmed nearly 6 degrees. Human-caused climate change induced by emissions of greenhouse gases continues to accelerate the warming of Alaska at an unprecedented rate. Climate change is having disproportionate effects in the Arctic, which is heating up twice as fast as the rest of Earth.
    1906AKH-3670.jpg
  • Decaying wood strip pattern on a cabin window shutter. Chicken, Alaska, USA. Chicken is one of the few surviving gold rush towns in Alaska. Mining and tourism keep it alive in the summer, and about 17 people stay through the winter. Gold miners settling here in the late 1800s wanted to name it after the local ptarmigan birds, but couldn't agree on the spelling, so instead called it Chicken to avoid embarrassment. A portion of Chicken including early 1900s buildings and the F.E. Company Dredge No. 4 (Pedro Dredge) is listed as the Chicken Historic District on the National Register of Historical Places. Chicken can be reached via Chicken Airport or Alaska Route 5, the Taylor Highway, which is not maintained from mid-October through mid-March.
    1906AKH-1518.jpg
  • Old rust pattern. Paddlewheel graveyard, Yukon River Campground, Dawson City, Yukon, Canada. Explore the ruins of seven historic paddlewheel boats discarded in the woods along the banks of the Yukon River. Directions: On foot or auto, take the free George Black Ferry to West Dawson and the Top of the World Highway. Turn right into Yukon River campground and park at its northern end. Walk through the yellow gate, turn left, and walk downstream a few minutes to the Paddlewheel graveyard. Please respect this site, which is protected under the Yukon Historic Resources Act. Dawson City was the center of the Klondike Gold Rush (1896–99), after which population rapidly declined, in Yukon, Canada. Dawson City shrank further during World War II after the Alaska Highway bypassed it 300 miles (480 km) to the south using Whitehorse as a hub. In 1953, Whitehorse replaced Dawson City as Yukon Territory's capital. Dawson City's population dropped to 600–900 through the 1960s-1970s, but later increased as high gold prices made modern placer mining operations profitable and tourism was promoted. In Yukon, the Klondike Highway is marked as Yukon Highway 2 to Dawson City.
    1906AK2-073.jpg
  • Rock patterns from Siberia Valley side streams. The Gillespie Pass Circuit follows the Young and Wilkin Rivers in Mount Aspiring National Park, in the Southern Alps. Makarora, Otago region, South Island of New Zealand. UNESCO lists Mount Aspiring as part of Wahipounamu - South West New Zealand World Heritage Area.
    1901NZ1-4104.jpg
  • Sand dune pattern. Sunrise on Mesquite Flat Dunes, near Stovepipe Wells in Death Valley National Park, California, USA. This dune field includes three types of dunes: crescent, linear, and star shaped. Polygon-cracked clay of an ancient lakebed forms the floor. Mesquite trees have created large hummocks that provide stable habitats for wildlife.
    1804SW-3022.jpg
  • Sunrise on Mesquite Flat Dunes, near Stovepipe Wells in Death Valley National Park, California, USA. This dune field includes three types of dunes: crescent, linear, and star shaped. Polygon-cracked clay of an ancient lakebed forms the floor. Mesquite trees have created large hummocks that provide stable habitats for wildlife.
    1804SW-2935.jpg
  • Polygon-cracked clay of an ancient lakebed forms the floor of Mesquite Flat Dunes, near Stovepipe Wells in Death Valley National Park, California, USA.
    1804SW2-180.jpg
  • Sunrise seen from Zabriskie Point in Death Valley National Park, California, USA.
    1804SW2-152.jpg
  • Sunrise seen from Zabriskie Point in Death Valley National Park, California, USA.
    1804SW2-132.jpg
  • Artist's Palette geologic formation on Artists Drive, Death Valley National Park, California, USA. More than 5 million years ago, multiple volcanic eruptions deposited ash and minerals across the landscape, which chemically altered over time into a colorful paint pot of elements: iron, aluminum, magnesium, and titanium.
    1804SW-2306.jpg
  • The Raplee Anticline (Lime Ridge), along San Juan River, Mexican Hat, Utah, USA.
    1804SW-1108.jpg
  • Sandstone rock pattern. Courthouse Towers, Park Avenue Trail, in Arches National Park, Moab, Utah, USA.
    1804SW2-042.jpg
  • Palette Spring, Mammoth Hot Springs. Yellowstone National Park, Wyoming, USA.
    1709US1-4623_Yellowstone-NP-WY.jpg
  • Climbers ascend Devils Tower National Monument. Bear Lodge Mountains, Black Hills, Wyoming, USA. Devils Tower is a butte of intrusive igneous rock exposed by erosion in the Bear Lodge Mountains, part of the Black Hills, near Hulett and Sundance in Crook County. Devils Tower (aka Bear Lodge Butte) rises dramatically 1267 feet above the Belle Fourche River, standing 867 feet from base to summit, at 5112 feet above sea level. Devils Tower was the first United States National Monument, established on September 24, 1906 by President Theodore Roosevelt.
    1709US1-3314_Devils-Tower-WY.jpg
  • The 1893 wood stake ladder for the first ascent of Devils Tower (by Willard Ripley) was restored 1972. The last known use of the ladder was in 1927 by daredevil Babe "The Fly" White. In 1972, the Park Service removed what was left of the bottom section, and restored the top 140 feet of the ladder, shown here. Devils Tower is a butte of intrusive igneous rock exposed by erosion in the Bear Lodge Mountains, part of the Black Hills, in Devils Tower National Monument, near Hulett and Sundance in Crook County, Wyoming, USA. Devils Tower (aka Bear Lodge Butte) rises dramatically 1267 feet above the Belle Fourche River, standing 867 feet from base to summit, at 5112 feet above sea level. Devils Tower was the first United States National Monument, established on September 24, 1906 by President Theodore Roosevelt.
    1709US1-3339_Devils-Tower-WY.jpg
  • Gateway Arch in St. Louis, Missouri, USA. Clad in stainless steel and built in the form of a weighted catenary arch, Gateway Arch is the world's tallest arch (630 feet high), the tallest man-made monument in the Western Hemisphere and Missouri's tallest accessible building. Built as a monument to the westward expansion of the United States, and officially dedicated to the American people, it is the centerpiece of the Jefferson National Expansion Memorial. The Arch was designed by Finnish-American architect Eero Saarinen in 1947. It was built 1963-1965 at the site of St. Louis' founding on the west bank of the Mississippi River and opened to the public in 1967. (Although built to last for ages, it is eventually susceptible to a tornado impact which could rip off the upper two-thirds.)
    1709US1-2191_Gateway-Arch_MO.jpg
  • Rock pattern in Callanish Standing Stones. Erected 4600 years ago, the Callanish Standing Stones are one of the most spectacular megalithic monuments in Scotland. The main site known as "Callanish I" forms a cross with a central stone circle erected circa 2900-2600 BC. More lines of stones were added by 2000 BC (the close of the Neolithic era), and it become a focus for rituals during the Bronze Age. From 1500-1000 BC, farmers emptied the burials and ploughed the area. After from 800 BC, peat accumulated 1.5 meters deep and buried the stones until removed in 1857. Visit this spectacular ancient site near the village of Callanish (Gaelic: Calanais), on the Isle of Lewis, Outer Hebrides (Western Isles), Scotland, United Kingdom, Europe.
    17SC4-098_Scotland.jpg
  • The Culloden Battlefield visitor center is run by the National Trust for Scotland, near Inverness, United Kingdom, Europe. The Battle of Culloden on 16 April 1746 was part of a religious civil war in Britain and was the final confrontation of the Jacobite rising of 1745. It was the last pitched battle on British soil, and in less than an hour about 1500 men were slain – more than 1000 of them Jacobites. After an unsuccessful Highland charge against the government lines, the Jacobites were routed and driven from the field. Today, strong feelings are still aroused by the battle and the brutal aftermath of weakening Gaelic culture and undermining the Scottish clan system. Three miles south of Culloden village is Drumossie Moor, often called Culloden Moor, site of the battle. Culloden is in Scotland 5 miles east of Inverness, off the A9/B9006, directed by brown signs.
    17SC1-4177_Scotland.jpg
  • Decaying walls grow grass. The formidable red sandstone walls of Caerlaverock Castle have a triangular shape, unique in Britain. First built in 1295 to to control trade, its wide moat, twin-towered gatehouse and lofty battlements give Caerlaverock a fairtale appearance, the epitome of a medieval stronghold. In the castle courtyard, walk through Nithsdale Lodging, a remarkable residence built in 1635, "the most ambitious early classical domestic architecture in Scotland." Caerlaverock is near Dumfries, on the edge of Caerlaverock National Nature Reserve, in southwest Scotland, United Kingdom, Europe. This stronghold defended the Maxwell family from the 1200s-1640, then was abandoned. It was besieged by the English during the Wars of Scottish Independence, and underwent several partial demolitions and reconstructions from the 1300s-1400s.
    17SC1-1352_Scotland.jpg
  • Fountains Abbey is one of the largest and best preserved ruined Cistercian monasteries in England. Visit it near Ripon and Aldfield, in North Yorkshire, England, UK, Europe. The adjacent Studley Royal Park features striking 1700s landscaping, gardens and canal. Founded in 1132, the abbey operated for 407 years becoming one of the wealthiest monasteries in England until its dissolution in 1539 under the order of Henry VIII. Studley Royal Park including the Ruins of Fountains Abbey is honored as a UNESCO World Heritage Site. The abbey is a Grade I listed building owned by the National Trust.
    17UK2-5504.jpg
  • A palm tree silhouette against blue sky with wispy currus clouds. Kaipalaoa Landing County Park, Hilo Bay, on the Big Island, Hawaii, USA.
    1701HAW-2973.jpg
  • Kalalau Valley cliffs seen from Pihea Trail, Na Pali Coast, Kauai, Hawaii, USA. The potholed Pihea Trail traverses a spectacular cliff edge of Na Pali-Kona Forest Reserve, overlooking the Kalalau Valley in Na Pali Coast State Park down to the Pacific Ocean, a breathtaking 4000 feet below, on the island of Kauai. Slippery wet clay makes this a challenging hike of 2.6 miles round trip with 500 feet gain to Pihea Peak. (Optionally continue past Pihea Peak to Alaka'i Swamp Trail.) Pihea Trail begins at Pu'u O Kila Lookout at the end of the road in Koke'e State Park.
    1701HAW-1513.jpg
  • Tall tropical tree canopy. Waimea Valley is a historical nature park with botanical gardens, at 59-864 Kamehameha Highway, Haleiwa, on the North Shore of island of Oahu, Hawaii, USA. Formerly known as "Waimea Valley Audubon Center," since 2008 the garden has been managed by Hi'ipaka LLC, a non-profit company created by the Office of Hawaiian Affairs. Hawaii is the northernmost island group in Polynesia.
    1701HAW-0382.jpg
  • Ancient wood at Glacier Pass. Backback to Mirror Lake in Eagle Cap Wilderness,  Wallowa–Whitman National Forest, Wallowa Mountains, Columbia Plateau, northeastern Oregon, USA. Hike 7.3 miles from Two Pan Trailhead (5600 ft) up East Lostine River to camp at popular Mirror Lake (7606 ft). Day hike to Glacier Lake via Glacier Pass (6 miles round trip, 1200 ft gain). Backpack out 8.7 miles via Carper Pass, Minam Lake and West Fork Lostine. From September 11-13, 2016 Carol and I walked 22 miles in 3 days.
    1609WAL-241.jpg
  • Evergreen & deciduous tree canopy. Deception Pass State Park, Whidbey Island, Washington, USA
    1604WHI-395.jpg
  • Tidal sand pattern. Double Bluff State Park (Useless Bay Tidelands), Whidbey Island, Washington, USA. While the tidelands are a State Park, the upland portion is Double Bluff Park, operated by the Friends of Double Bluff and Island County, including an off-leash dog park.
    1604WHI-191.jpg
  • A reflection of a great blue heron (in the Ardeidae family of birds) hunting for fish from a boat along the Cheshiahud Lake Union Loop in Seattle, Washington, USA.
    1604CHE-157_Cheshiahud_Lake-Union.jpg
  • Lichen pattern. Hike from Pontresina up Roseg Valley to Fuorcla Surlej for stunning views of Piz Bernina and Piz Rosegg, finishing at Corvatsch Mittelstation Murtel lift. Walking 14 km, we went up 1100 meters and down 150 m. Optionally shorten the hike to an easy 4 km via round trip lift. Pontresina is in Upper Engadine, in Graubünden (Grisons) canton, Switzerland, the Alps, Europe. The Swiss valley of Engadine translates as the "garden of the En (or Inn) River" (Engadin in German, Engiadina in Romansh, Engadina in Italian).
    16SWI-9070.jpg
  • In Findeln (formerly called Findelen), admire authentic Walser houses, barns, and stores built of larch timber blackened by the sun, above Zermatt, in the Pennine Alps, Switzerland, Europe. The Walser people are named after Wallis (Valais), the uppermost Rhône valley, where they settled from the 900s in the late phase of the migration of the Alamanni (confederation of Germanic tribes) crossing from the Bernese Oberland. From Zermatt, a popular walk is the Five Lakes Trail from Sunnegga Express funicular. Although especially nice for families, the 5-Seenweg loop hike is aesthetically marred with ski slope infrastructure throughout (5 dammed artificial lakes, power lines, lifts, dusty roads, snow-making sprinklers, etc). Visually, the most aesthetic features are the old wood buildings in upper Findeln, and the reflecting lakes of Grindjisee and Stellisee.
    16SWI-8460.jpg
  • The Matterhorn (4478 m/14,692 ft) rises above Zmutt Valley. From Zermatt, hike the scenic Höhbalmen Höhenweg loop via Bergrestaurant Edelweiss, Trift Hut and Zmutt, in the Pennine Alps, Switzerland, Europe. With delightful views of alpine meadows, peaks and glaciers, this strenuous walk went up and down 1200 meters over 21.6 km (13.4 miles).
    16SWI-8227.jpg
  • Kandersteg is a great base for hiking in Switzerland. For example: an epic hike from Selden in Bern canton traverses Lötsch glacier and Lötschen Pass (German: Lötschenpass, Swiss German: Lötschepass) to neighboring Lötschental in Valais canton; hiking poles recommended. The walk starts with a reserved Postbus ride from Kandersteg to Selden (in Gasterntal / Gasteretal / Gasterental), climbs 1350 meters, descends 925 m, and ends 13 km later at Lauchernalp lift station, which descends to Wiler in Lötschental, to reach Goppenstein via Postbus, back to Kandersteg via train. You can also reverse the route or stay overnight in dorms at Lötschepass hut.
    16SWI-2686.jpg
  • Bark of a Pacific Madrone or Madrona (Arbutus menziesii) tree grows in an unusually bumpy yellow and red pattern. Photographed along the lovely Goose Rock Perimeter Trail, in Deception Pass State Park, on Whidbey Island, Washington, USA.
    1505WHI-070_Arbutus-menziesii.jpg
  • Prehistoric pictograph,<br />
Cave Spring Trail, Needles District of Canyonlands National Park, Utah, USA.
    1503SW-1261_pictograph_Canyonlands.jpg
  • Explore the elegant subway and slot of Leprechaun Canyon in North Wash, between Hanksville & Hite, Utah, USA. Desert varnish coats the Triassic-Jurassic sandstone. Directions: from Hanksville, drive 26 miles south on Highway 95 to the junction with Utah 276 and stay left on H95 for another 2.0 miles across a wash, then park on the left (east) along a short road within the first 100 feet before its sandtrap end. Walk up the wash of Leprechaun Canyon 2 miles round trip to a subway which narrows to a tight squeeze called Belfast Boulevard. Manganese-rich desert varnish requires thousands of years to coat a rock face that is protected from precipitation and wind erosion. The varnish likely originates from airborne dust and external surface runoff, including: clay minerals, oxides and hydroxides of manganese (Mn) and/or iron (Fe), sand grains, trace elements, and usually organic matter. Streaks of black varnish often occur where water cascades over cliffs protected from wind. Varnish color varies from shades of brown to black. Manganese-poor, iron-rich varnishes are red to orange, and intermediate concentrations are shaded brown. Manganese-oxidizing microbes may explain the unusually high concentration of manganese in black desert varnish, which can be smooth and shiny where densest. Nearby, Glen Canyon National Recreation Area is just 8 miles south on H95.
    1503SW-0837-p2_Leprechaun-Canyon.jpg
  • Admire fanciful hoodoos, mushroom shapes, and rock pinnacles in Goblin Valley State Park, in Emery County between the towns of Green River and Hanksville, in central Utah, USA. The Goblin rocks eroded from Entrada Sandstone, which is comprised of alternating layers of sandstone (cross-bedded by former tides), siltstone, and shale debris which were eroded from former highlands and redeposited in beds on a former tidal flat. As part of the Colorado Plateau, the San Rafael Swell is a giant dome-shaped anticline of rock (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.
    1503SW-0571_Goblin-Valley.jpg
  • Admire fanciful hoodoos, mushroom shapes, and rock pinnacles in Goblin Valley State Park, in Emery County between the towns of Green River and Hanksville, in central Utah, USA. The Goblin rocks eroded from Entrada Sandstone, which is comprised of alternating layers of sandstone (cross-bedded by former tides), siltstone, and shale debris which were eroded from former highlands and redeposited in beds on a former tidal flat. As part of the Colorado Plateau, the San Rafael Swell is a giant dome-shaped anticline of rock (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.
    1503SW-0547_Goblin-Valley.jpg
  • Find fascinating Jurassic sandstone rock patterns in Wild Horse Canyon on federal BLM land in the San Rafael Swell (160-175 million years old), Utah, USA. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0748_Jurassic-sandstone-patte...jpg
  • Find fascinating Jurassic sandstone rock patterns in Wild Horse Canyon on federal BLM land in the San Rafael Swell (160-175 million years old), Utah, USA. The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior that administers American public lands.
    1503SW-0739_Jurassic-sandstone-patte...jpg
  • A limb of driftwood lodges high in the slot of 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.
    1503SW-0675_slot-driftwood_Crack-Can...jpg
  • Hike through Grand Wash, in Capitol Reef National Park, Utah, USA. Capitol Reef National Park is centered upon the 100-mile-long Waterpocket Fold, the steep eastern limb of the Circle Cliffs Uplift, formed in Late Cretaceous time, during the Laramide Orogeny. Pressure caused by the subduction of the Farallon Plate beneath the North American Plate along the west coast caused several huge folds like this in southeast Utah, USA. Steeply tilted Triassic and Jurassic rocks form the hogbacks of the Waterpocket Fold and Capitol Reef, which is built of dark-red dune-formed Wingate Sandstone, thinly bedded river deposits of the Kayenta Formation, crested by the massive, white, dune-formed Navajo Sandstone. Honeycomb weathering: rainwater soaks into sandstone, dissolves its cement, and redeposits it near the surface as the water evaporates, forming a resistant outer layer, pockmarked with holes into the soft inner layers enlarged by wind and moisture.
    1503SW-0493_sandstone-pattern.jpg
  • Navajo Sandstone (fossilized cross-bedded sand dune of the Jurassic period) exfoliates into a pattern along Rim Overlook Trail in Capitol Reef National Park, Utah, USA. Iron oxides (hematite and goethite) bled through the Navajo sandstone layers to paint the rock yellow, orange, and brown. Capitol Reef National Park is centered upon the 100-mile-long Waterpocket Fold, the steep eastern limb of the Circle Cliffs Uplift, raised in Late Cretaceous time, during the Laramide Orogeny. Pressure caused by the subduction of the Farallon Plate beneath the North American Plate along the west coast caused several huge folds like this in southeast Utah, USA.
    1503SW-0364_Navajo-sandstone-pattern.jpg
  • Swirling sandstone rock pattern, Capitol Gorge, Capitol Reef National Park, Utah, USA.
    1503SW-0116_sandstone-pattern.jpg
  • Burney Falls is a beautiful National Natural Landmark on Burney Creek in McArthur-Burney Falls Memorial State Park, Shasta County, California, USA. The water comes from underground springs above and at the falls, which plunges 129 feet. The waterfall was named after pioneer settler Samuel Burney who lived nearby in the 1850s. The McArthurs settled nearby in the late 1800s and their descendants saved the waterfall from development, bought the property and gifted it to the state in the 1920s. The park is northeast of Redding, six miles north of Highway 299 on Highway 89 near Burney. The Pacific Crest Trail passes through the park.
    1412CA-012_Burney-Falls.jpg
  • A California Sycamore (Platanus racemosa) trunk has grown twisted after being undercut by Big Chico Creek in Upper Bidwell Park, Chico, Butte County, California, USA.
    1311CA-025_California-Sycamore-tree.jpg
  • Lichen polygon pattern on rock. White Mountains, NH, USA. Kancamagus Highway (NH Route 112) is in White Mountain National Forest. The White Mountains (a range in the northern Appalachian Mountains) cover a quarter of the state of New Hampshire.
    1410NH-402_White-Mountains.jpg
  • Foam swirls. Enjoy a short walk along the Swift River in Rocky Gorge Scenic Area on Kancamagus Highway (NH Route 112), in White Mountain National Forest, New Hampshire, USA. The White Mountains (a range in the northern Appalachian Mountains) cover a quarter of the state of New Hampshire. Leaf peepers love the peak of autumn foliage around the first week of October.
    1410NH-152_White-Mountains.jpg
  • Peeling trunks of white birch trees grow in front of fall foliage colors reflected in Upper Hadlock Pond, in Acadia National Park, on Mount Desert Island, near Bar Harbor, Maine, USA. Hike granite peaks and enjoy Atlantic coastal scenery. Originally created as Lafayette National Park in 1919, the oldest National Park east of the Mississippi River, it was renamed Acadia in 1929. During the last glacial maximum 21,000 years ago, glaciers measuring up to 9,000 feet thick cut into granite ridges, sculpting the fjord-like Somes Sound.
    1410ME-573-p1_Acadia-NP-Maine.jpg
  • Imnaha River Trail, Hells Canyon National Recreation Area, Wallowa-Whitman National Forest, Imnaha, Oregon, USA
    1405OR-223.jpg
  • Moss drapery on branches. Lynn Canyon is a municipal park established in 1912 at 3663 Park Road, in North Vancouver, British Columbia, V7J 3G3, Canada. Phone 604-990-3755.
    1402VAN-524.jpg
  • Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-133.jpg
  • Large columns, in 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-5178_Carlsbad-Caverns-NP.jpg
  • Bottle-brush shape, 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-385-p1_Caverns-of-Sonora_Texa...jpg
  • Puff-ball speleothem panorama 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. This panorama was stitched from 6 overlapping photos.
    1403TX-385-90pan_Caverns-of-Sonora_T...jpg
  • Coral-like speleothems. 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-348_Caverns-of-Sonora_Texas.jpg
  • Hikers explore atop a large pink granite dome at Enchanted Rock State Natural Area, between Fredericksburg and Llano, Texas, USA. Enchanted Rock is a fascinating exfoliation dome (with layers like an onion), rising 425 feet (130 m) above its surroundings to elevation of 1825 feet (556 m) above sea level, in the Llano Uplift. Geologically, the exposed rock (monadnock or inselberg, "island mountain") is part of a pluton (bubble of rock slowly crystallized from magma) within the billion-year-old igneous batholith, Town Mountain Granite (covering 62 square miles mostly underground), which intruded from a deep pool of hot magma 7 miles upwards into the older metamorphic Packsaddle Schist. The overlying sedimentary rock (Cretaceous Edwards limestone) eroded away to expose the prominent domes seen today: Enchanted Rock, Little Rock, Turkey Peak, Freshman Mountain, and Buzzard's Roost.
    1403TX-154_Enchanted-Rock_Texas.jpg
  • Support timbers decay in stone wall at Pueblo Bonito, Chaco Culture National Historical Park, New Mexico, USA. Pueblo Bonito is a monumental public building (Puebloan Great House) occupied from around 828 to 1126 AD, now preserved in Chaco Canyon. The huge D-shaped complex of Pueblo Bonito enclosed two plazas with dozens of ceremonial kivas, plus 600 rooms towering 4 and 5 stories above the valley floor. The functions of this building included ceremony, administration, trading, storage, hospitality, communications, astronomy, and burial, but few living quarters. Chaco Culture NHP hosts the densest and most exceptional concentration of pueblos in the American Southwest and is a UNESCO World Heritage Site, located in remote northwestern New Mexico, between Albuquerque and Farmington. From 850 AD to 1250 AD, Chaco Canyon advanced then declined as a major center of culture for the Ancient Pueblo Peoples. Chacoans quarried sandstone blocks and hauled timber from great distances, assembling fifteen major complexes that remained the largest buildings in North America until the 1800s. Climate change may have led to its abandonment, beginning with a 50-year drought starting in 1130.
    1403NM-0557_Pueblo-Bonito_Chaco-Cult...jpg
  • Bisti/De-Na-Zin Wilderness, eroded sediment layers, south of Farmington, in San Juan County, New Mexico, USA. This fantasy world of strange rock formations is made of interbedded sandstone, shale, mudstone, coal, and silt. These rock layers have weathered into eerie hoodoos (pinnacles, spires, and cap rocks). This was once a riverine delta west of an ancient sea, the Western Interior Seaway, which covered much of New Mexico 70 million years ago. Swamps built up organic material which became beds of lignite. Water disappeared and left behind a 1400-foot (430 m) layer of jumbled sandstone, mudstone, shale, and coal. The ancient sedimentary deposits were uplifted with the rest of the Colorado Plateau, starting about 25 million years ago. Waters of the last ice age eroded the hoodoos now visible. The high desert widerness of Bisti is managed by the US Bureau of Land Management (BLM).
    1403NM-0102_Bisti_De-Na-Zin-Wilderne...jpg
  • Eroded badlands of Bisti/De-Na-Zin Wilderness, south of Farmington, in San Juan County, New Mexico, USA. This fantasy world of strange rock formations is made of interbedded sandstone, shale, mudstone, coal, and silt. These rock layers have weathered into eerie hoodoos (pinnacles, spires, and cap rocks). This was once a riverine delta west of an ancient sea, the Western Interior Seaway, which covered much of New Mexico 70 million years ago. Swamps built up organic material which became beds of lignite. Water disappeared and left behind a 1400-foot (430 m) layer of jumbled sandstone, mudstone, shale, and coal. The ancient sedimentary deposits were uplifted with the rest of the Colorado Plateau, starting about 25 million years ago. Waters of the last ice age eroded the hoodoos now visible. The high desert widerness of Bisti is managed by the US Bureau of Land Management (BLM).
    1403NM-0035_Bisti_De-Na-Zin-Wilderne...jpg
  • Icicles freeze over a splashing stream in Cougar Mountain Regional Wildland Park, Washington, USA.
    1301COU-003.jpg
  • A duck swims across an intricate pattern of leaves reflected in the emerald and blue waters of Lake Bled (Blejsko jezero), in the Julian Alps, Slovenia, Europe. Lake Bled hosted the World Rowing Championships in 1966, 1979, 1989, and 2011. The lake is 35 kilometers from Ljubljana International Airport.
    13SLO-1372_Lake-Bled-Slovenia.jpg
  • Sandstone pattern on the Cockscomb, a striking monocline (geologic fold) in Grand Staircase-Escalante National Monument, Utah, USA. The Cockscomb is the northern extension of the East Kaibab Monocline, a major feature of the Colorado Plateau stretching over 100 miles north from the Grand Canyon. Directions to the easiest Cockscomb ascent: On Highway 89, drive 10 miles west of Big Water. Between mileposts 17-18 on H89, turn north on Cottonwood Canyon Road (#400) and drive 12 miles to where a side road turns east over the Cockscomb (a quarter mile south of Hackberry Canyon parking lot). Park at the bottom of the steep road and walk 3 miles round trip to the crest, gaining 950 feet.
    1303UT-1478.jpg
  • Green and purple-tinged prickly pear cactus / Opuntia genus forms a thorny pattern along Lower Calf Creek Falls trail, in Grand Staircase Escalante National Monument, Utah, USA.
    1303UT-2132.jpg
  • Wavy red, white, and black sandstone patterns decorate Tunnel Slot Canyon in Grand Staircase-Escalante National Monument, Utah, USA. Directions to unmarked trailhead for Zebra and Tunnel Slot Canyons: From Escalante town, drive 6 miles east on Highway 12, turn right on Hole-in-the-Rock Road, drive 7.8 miles to the third cattle guard and park on west side of road. Hike east on well-trodden but unmarked path, 5 miles round trip to Zebra Slot, plus an optional 3 miles round trip to Tunnel Slot (750 feet gain over 8 miles), using map from GSENM Visitor Center or canyoneeringusa.com.
    1303UT-2077.jpg
  • The Remarkable Rocks form fantastic shapes in Flinders Chase National Park, Kangaroo Island, South Australia. The Remarkable Rocks began as magma injected into a sedimentary rock layer and crystallized into a single granite monolith a few kilometers below the earths surface. Subsurface weathering cracked the granite along joint planes and created corestones. Erosion peeled away the surface and revealed the corestones, which were sculpted asymmetrically by the affects of rain and prevailing southerly winds.
    04AUS-20248_Remarkable-Rocks.jpg
  • Underwater orange and green algae grows in bright patterns in Gardner Bay, a wet landing location on Española (Hood) Island, the oldest of the Galapagos Islands (formed 3 million years ago), a province of Ecuador, South America. The English named it Hood Island after Viscount Samuel Hood. Two spots are especially popular with visitors: Bahía Gardner, which has a lovely beach; and Punta Suárez, of interest because of its varied bird-life. In 1959, Ecuador declared 97% of the land area of the Galápagos Islands to be Galápagos National Park, which UNESCO registered as a World Heritage Site in 1978. Ecuador created the Galápagos Marine Reserve in 1998, which UNESCO appended in 2001.
    09EQUCIMG_3979_Galapagos.jpg
  • Ancient brown and blue rock pattern, Mount Robson Provincial Park, British Columbia, Canada. This is part of the Canadian Rocky Mountain Parks World Heritage Site honored by UNESCO in 1984.
    08CAN-2227_Mt-Robson-rock-pattern.jpg
Prev Next
  • Facebook
  • Twitter
x

Portfolio of Tom Dempsey / PhotoSeek.com

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