Batagaika crater

E369918

Batagaika crater is a massive, rapidly expanding thermokarst depression in Siberia’s permafrost, often called a “megaslump” and studied as a striking indicator of climate change.

All labels observed (2)

Label Occurrences
Batagaika crater canonical 1
Batagaika megaslump 1

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf geological formation
megaslump
permafrost feature
thermokarst depression
causeOfFormation ground ice melt
surface subsidence
climateZone continuous permafrost zone
contains fossil remains
ice-rich permafrost
pollen records
sedimentary sequences
country Russia
environmentType subarctic
expansionDirection along valley sides
upslope
expansionRate several meters per year
formationProcess permafrost thaw
thermokarst processes
hasAlternativeName Batagaika crater
surface form: Batagaika megaslump

Batagay megaslump
Batagayka crater
hasApproximateDepth up to about 100 meters
hasApproximateLength about 1 kilometer
hasApproximateWidth hundreds of meters
locatedIn Sakha Republic
Yakutia
locatedInRegion Siberia
locatedOnContinent Asia
monitoredBy field surveys
satellite imagery
nearRiver Yana River NERFINISHED
nearSettlement Batagay
notableFor evidence of past climates
evidence of past ecosystems
exposing ancient permafrost
rapid lateral growth
observedSince 1960s
primaryDriver climate warming
permafrost degradation
risk landscape destabilization
release of greenhouse gases
studiedAs indicator of climate change
studiedBy climate researchers
geomorphologists
permafrost scientists
surfaceMaterial ice-rich loess
permafrost sediments
timeOfInitialFormation late 20th century
triggerEvent deforestation near slope

How these facts were elicited

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.

Batagay locatedNear Batagaika crater
Batagaika crater hasAlternativeName Batagaika crater
this entity surface form: Batagaika megaslump