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Møns Klint, English: the Cliffs of Møn.
The chalk forming the cliffs consists of the remains of shells from millions of microscopic creatures (coccolithophores) which lived on the seabed over 70 million years ago. As a result of huge pressure from glaciers moving west, the terrain was compacted and pushed upwards, forming a number of hills and folds. When the ice melted at the end of the last ice age about 11,000 years ago, the cliffs emerged. They form part of the same deposits as the cliffs of Rügen, Germany, on the other side of the Baltic. Today, it is possible to find fossils of various types of shellfish as the sea continues to erode the chalk. Erosion also caused one of the highest points on the cliffs, the Sommerspir, to fall into the sea in 1998, and in January 2007, there was an even larger landslide around the Store Taler, in the northern part of the cliffs, creating a 300-m long peninsula of chalk and fallen trees stretching out into the sea below.
source: en.wikipedia.org/wiki/M%C3%B8ns_Klint
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© René Eriksen.
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IG: @iamevanclark
located at the southwestern edge of the Burren region in County Clare, Ireland. They rise 120 metres (390 ft) above the Atlantic Ocean at Hag's Head and reach their maximum height of 214 metres (702 ft) just north of O'Brien's Tower, eight kilometres to the north. A round stone tower near the midpoint of the cliffs was built in 1835 by Sir Cornelius O'Brien. From the cliffs and from atop the tower, visitors can see the Aran Islands in Galway Bay, the Maumturks and Twelve Pins mountain ranges to the north in County Galway, and Loop Head to the south.
Cliff jumper in Bruce Peninsula National Park, Ontario Canada.
9 Photo's used, stitched in Photoshop.
Suisun Marsh was beautiful this morning. A walk at sunrise on the little Hill Slough trail provided views of Suisun Hill, Hill Slough and the surrounding area bathed in glorious sparkling light. I also took particular note of a colony of Cliff Swallows nesting under the bridge. I have yet to capture a sharp image of one of these swift little creatures, but I did manage this somewhat blurry shot taken from an awkward angle of a single bird perched on one of their interesting nests. I’d like a better view -- I wonder if I should invest in some hip waders?
Petrochelidon pyrrhonota
www.ipm.ucdavis.edu/PMG/PESTNOTES/pn7482.html
Barn and cliff swallows build mud nests attached to buildings and other structures, a habit that sometimes puts them into conflict with people. This is particularly true of the cliff swallow—the swallow of San Juan Capistrano—which nests in large colonies of up to several hundred pairs.
Swallows feed on insects and spend a large part of each day in the air catching flies, beetles, and mosquitoes. Their long, pointed wings give them great speed and maneuverability. Cliff swallows are found throughout California, except in high mountains and the dry southeastern desert. Four basic conditions are found at all cliff swallow colonies: (1) an open habitat for foraging; (2) a vertical surface beneath an overhang for attaching the nest; (3) a supply of mud that has the proper consistency for nest building; and (4) a body of fresh water for drinking.
Cliff swallows arrive at nest colonies in successive waves. A definite homing tendency exists among adults that previously nested at a colony. These birds are the first to return, followed by adults who bred at other colonies in previous years and by young birds who have not yet bred. The younger birds include individuals not born at the selected colony. In addition to their homing tendency, breeding swallows are attracted to old nests. Under suitable conditions, a nest is quite durable and can be used in successive years. Old nests are usually claimed on the first day of arrival, although probably not by the original makers. Dilapidated nests are quickly occupied and repaired.
Cliff swallow nests are gourd-shaped enclosed structures built of mud pellets, consisting primarily of sand with smaller amounts of silt and clay. The nest is cemented with mud under the eave of a building, bridge, or other vertical surface. Usually the first nests are located at the highest point possible with subsequent nests attached below it, forming a dense cluster. Both sexes construct the nest, proceeding slowly to allow the mud to dry and harden. Depending on mud supply and weather, nest construction takes 1 to 2 weeks. Mud is collected at ponds, puddles, ditches, and other sites up to one-half mile away, with many birds using the same mud source. A typical nest contains 1,000 to 1,400 mud pellets, each representing one trip to and from the nest.
About 2/3 of the way down the 400 steps to South Stack Lighthouse in Holyhead, Wales - There was a hole in one side of the cliff. When I looked through this is what I saw.
On the western side of the peninsula, from the headland above the shore in the previous shot and looking north-east rather than south.
Early Bronze Age flint arrowheads.
For more information visit www.wessexarch.co.uk/projects/kent/ramsgate/cliffs_end/
The conversion of the color photo I took makes me wish I had had the presence of mind to shoot this in Sepia in the first place. A large storm had just passed over and the clouds were thick and dark making a cool effect but dulling the colors of the area, so when I converted it just for the sake of doing it I liked the results better.
Best viewed large
Located on the Colorado Plateau in northern Arizona, Vermilion Cliffs National Monument includes the Paria Canyon-Vermilion Cliffs Wilderness. The Monument borders Kaibab National Forest to the west and Glen Canyon National Recreation Area to the east.
This remote and unspoiled, 280,000-acre Monument is a geologic treasure, containing a variety of diverse landscapes from the Paria Plateau, Vermilion Cliffs, Coyote Buttes, and Paria Canyon. Elevations range from 3,100 to 7,100 feet.
Visitors will enjoy scenic views of towering cliffs and deep canyons. Paria Canyon offers an outstanding three to five day wilderness backpacking experience. The colorful swirls of cross-bedded sandstone in Coyote Buttes are an international hiking destination. There are also opportunities to view wildlife, including California condors. There are two developed campgrounds just outside the Monument: Stateline and White House. Dispersed camping is allowed outside the wilderness area in previously disturbed areas.
A permit is required for hiking in Coyote Buttes North (the Wave), Coyote Buttes South, and for overnight trips within Paria Canyon.
Learn more at: www.blm.gov/az/st/en/prog/blm_special_areas/natmon/vermil...
Photo: Bob Wick, BLM California
Some rocks at the edge of the cliff at the Butt of Lewis, with the opposite cliff face in the background.
The Cliffs of Moher are one of Ireland's top Visitor attractions. The Cliffs are 214m high at the highest point and range for 8 kilometres over the Atlantic Ocean on the western seaboard of County Clare. O'Brien's Tower stands proudly on a headland of the majestic Cliffs. From the Cliffs one can see the Aran Islands, Galway Bay, as well as The Twelve Pins, the Maum Turk Mountains in Connemara and Loop Head to the South. The Cliffs of Moher take their name from a ruined promontory fort “Mothar” which was demolished during the Napoleonic wars to make room for a signal tower.
The Cliffs of Moher are home to one of the major colonies of cliff nesting seabirds in Ireland. The area was designated as a Special Protection Area (SPA) for Birds under the EU Birds Directive in 1986 and as a Refuge for Fauna in 1988. Included within the designated site are the cliffs, the cliff-top maritime grassland and heath, and a 200 metre zone of open water, directly in front of the cliffs to protect part of the birds' feeding area. The designation covers 200 hectares and highlights the area's importance for wildlife.