Skosmos: GCMD: PINGO

... > EARTH SCIENCE > SOLID EARTH > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > PINGO

PINGO

A mound of earth-covered ice found in the Arctic and subarctic that can reach up to 70 metres (230 ft) in height and up to 600 m (2,000 ft) in diameter. The term originated as the Inuvialuktun word for a small hill. A pingo is a periglacial landform, which is defined as a nonglacial landform or process linked to colder climates. Periglacial suggests an environment located on the margin of past glaciers. However, freeze and thaw cycles influence landscapes outside areas of past glaciation. Therefore, periglacial environments are anywhere freezing and thawing modify the landscape in a significant manner

2013-02-18 10:39:35.0 [tbs1979] Insert Concept add broader relation (PINGO [4a0c46ff-2d07-442d-b141-6156d9ea4a2e,82453] - FLUVIAL LANDFORMS [cb5193ab-2d7a-4b35-b7ec-f16ce78ae270,64131]);
2013-04-01 08:52:56.0 [tbs1979] insert Definition (id: null text: A mound of earth-covered ice found in the Arctic and subarctic that can reach up to 70 metres (230 ft) in height and up to 600 m (2,000 ft) in diameter. The term originated as the Inuvialuktun word for a small hill. A pingo is a periglacial landform, which is defined as a nonglacial landform or process linked to colder climates. Periglacial suggests an environment located on the margin of past glaciers. However, freeze and thaw cycles influence landscapes outside areas of past glaciation. Therefore, periglacial environments are anywhere freezing and thawing modify the landscape in a significant manner language code: en);

https://gcmd.earthdata.nasa.gov/kms/concept/4a0c46ff-2d07-442d-b141-6156d9ea4a2e

RDF/XML TURTLE JSON-LD

Skosmos