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Periglacial Collection

Periglacial environments are characterized by extreme cold temperatures and the presence of frozen ground, known as permafrost

Background imagePeriglacial Collection: DDE-90028882

DDE-90028882
The water of the creek Gschloessbach. The Gschloessbach has its source in the glacier Viltragenkees which is the reason for its sediment load and its yellow white color

Background imagePeriglacial Collection: DDE-90028881

DDE-90028881
The glacier snout with ice cave of Viltragenkees in the National Park Hohen Tauern. Viltragenkees is showing signs of rapid retreat. The glacier foreland shows fresh moraine till

Background imagePeriglacial Collection: DDE-90028864

DDE-90028864
Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: DDE-90028863

DDE-90028863
Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: DDE-90028860

DDE-90028860
Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: DDE-90028859

DDE-90028859
Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: DDE-90028858

DDE-90028858
Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: DDE-90028857

DDE-90028857
Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: DDE-90028856

DDE-90028856
Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: DDE-90028855

DDE-90028855
Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: DDE-90028854

DDE-90028854
Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: DDE-90028853

DDE-90028853
Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: Norway, Svalbard, Billefjorden

Norway, Svalbard, Billefjorden
Norway, Svalbard Lateral rock strata, scree slopes, band of Gysum near the base at fjordside

Background imagePeriglacial Collection: Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach

Ice cave and glacier snout of Schlatenkees, source of the creek Schlatenbach. Parts of the have collapsed and melted away. Therefore an ice cave with two openings exists. Austria, East Tyrol

Background imagePeriglacial Collection: The glacier snout with ice cave of Viltragenkees in the National Park Hohen Tauern

The glacier snout with ice cave of Viltragenkees in the National Park Hohen Tauern. Viltragenkees is showing signs of rapid retreat. The glacier foreland shows fresh moraine till

Background imagePeriglacial Collection: Picture No. 10886810

Picture No. 10886810
Dwarfed Norway Spruce - on Vitosha stone river - (also called stone run / stone stream or stone sea) peculiar geomorphological phenomenon formed from granite in periglacial conditions Date:

Background imagePeriglacial Collection: Lowland Point - Periglacial Ram Cliffs - Cornwall - UK

Lowland Point - Periglacial Ram Cliffs - Cornwall - UK
DAC-1146 Lowland Point - Periglacial Ram Cliffs Cornwall - UK David Chapman Please note that prints are for personal display purposes only and may not be reproduced in any way

Background imagePeriglacial Collection: Vitosha stone river - (also called stone run - stone stream or stone sea)

Vitosha stone river - (also called stone run - stone stream or stone sea) peculiar geomorphological phenomenon formed
ROG-14299 Vitosha stone river - (also called stone run - stone stream or stone sea) peculiar geomorphological phenomenon formed from granite in periglacial conditions Mount Vitosha - Bulgaria

Background imagePeriglacial Collection: Norway Spruce (Picea abies) dwarfed habit, growing amongst granite boulders in stone run

Norway Spruce (Picea abies) dwarfed habit, growing amongst granite boulders in stone run, peculiar geomorphological phenomenon formed from granite in periglacial conditions, Vitosha Stone River

Background imagePeriglacial Collection: Granite boulders in stone run, peculiar geomorphological phenomenon formed from granite in

Granite boulders in stone run, peculiar geomorphological phenomenon formed from granite in periglacial conditions, Vitosha Stone River, Mount Vitosha, Bulgaria, may

Background imagePeriglacial Collection: Glacial sand deposit

Glacial sand deposit. Sand is composed of small grains of rock. Its composition and grain size varies depending on the location


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Periglacial environments are characterized by extreme cold temperatures and the presence of frozen ground, known as permafrost. These unique landscapes can be found in regions near the Earth's poles and high mountain ranges, where freezing temperatures persist for extended periods. In these frigid terrains, ice wedges (DDE-90028882) form intricate patterns within the frozen ground, creating a mesmerizing sight. These wedges result from repeated cycles of freezing and thawing, causing cracks to widen over time. They not only add an aesthetic appeal but also play a crucial role in shaping the landscape. The periglacial zone is home to various landforms shaped by frost action. One such example is pingos (DDE-90028881), which are conical hills formed when groundwater freezes and expands beneath the surface. As this process continues over thousands of years, pingos rise above their surroundings like icy mounds. Another fascinating feature found in periglacial areas is patterned ground (DDE-90028864). This phenomenon occurs due to freeze-thaw processes that sort sediments into distinctive arrangements such as polygons or stripes. The resulting patterns create an otherworldly appearance across vast stretches of land. Permafrost acts as a natural freezer preserving ancient remains like mammoths (DDE-90028863). When these creatures became trapped in ice thousands of years ago, they were remarkably preserved until discovered by scientists today—a testament to the power environments. The harsh conditions prevailing in these regions pose challenges for both humans and wildlife alike. However, some organisms have adapted remarkably well to survive here. Arctic foxes (DDE-90028860), snowshoe hares (DDE-90028859), and musk oxen (DDE-90028858) are just a few animals that thrive despite sub-zero temperatures. Climate change poses significant threats to periglacial environments.