Wild Turkeys
Nederland – Dwingelderveld
Base camp at 7,200 feet
The beginnings of a glacier
Avalanche warning
The Cuckmere valley from Ewe Down - 11.1.2016
Clouds over Cuckmere Haven - 11.01.2016
Hoodoos & arches
Water Canyon waterfall
Glacial flow (Explored)
Blue and white
Crags and shadows
Nore Down, north of Newhaven, from Seaford Road -…
A Teal drake on the Ouse Estuary Nature Reserve -…
Cuckmere Haven from the A259, coast road in Sussex…
Outhouse with a view
Rough surface
Blue ice melts
Twilight on the Alaska range
Budding barrel cactus
The Great Unconformity
Probably not an issue today--
Osceola Ditch
Where glaciers begin
Spring cover
The Great Arch
View of a glacier
Above the mountains (Explored)
Snow Bowl
Northern Snake Range and Mt. Moriah
Wheeler Peak
Great Basin Bristlecone Pine
Travertine Dams
San Rafael River
Chipmunks playing
Paragliding above the Cuckmere valley - Sussex - 2…
Spain - Barbate, Torre del Tajo
Old Boathouse, Piddinghoe, 2.1.2012
Piddinghoe from the SE - Newhaven - 6.7.2015
Coombe Farm from Telscombe Tye - 20.10.2015
Telscombe Village - East Sussex - 20.10.2015
Canyon View
Black Legged Kittiwake
Cow parsley by the Cuckmere - 9.10.2015
Checking out the boaters
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Crevasse Field
Talkeetna Air Taxi - Denali Flight and Glacier Landing
"A crevasse is a deep crack, or fracture, found in an ice sheet or glacier, as opposed to a crevice that forms in rock. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces.
Crevasses often have vertical or near-vertical walls, which can then melt and create seracs, arches, and other ice formations.[1] These walls sometimes expose layers that represent the glacier's stratigraphy. Crevasse size often depends upon the amount of liquid water present in the glacier. A crevasse may be as deep as 45 metres, as wide as 20 metres, and up to several hundred metres long"
en.wikipedia.org/wiki/Crevasse
AIMG 5562
"A crevasse is a deep crack, or fracture, found in an ice sheet or glacier, as opposed to a crevice that forms in rock. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces.
Crevasses often have vertical or near-vertical walls, which can then melt and create seracs, arches, and other ice formations.[1] These walls sometimes expose layers that represent the glacier's stratigraphy. Crevasse size often depends upon the amount of liquid water present in the glacier. A crevasse may be as deep as 45 metres, as wide as 20 metres, and up to several hundred metres long"
en.wikipedia.org/wiki/Crevasse
AIMG 5562
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