Belukha Glacier system

E542929

The Belukha Glacier system is an extensive network of glaciers surrounding and descending from Belukha Mountain in the Altai range of Siberia, forming one of the region’s most significant ice complexes.

All labels observed (3)

How this entity was disambiguated

Statements (41)

Predicate Object
instanceOf glacier
glacier system
affectedBy climate change
associatedWith Belukha Mountain
creates glacial landforms
glacial valleys
moraines
proglacial lakes
descendsFrom Belukha Mountain
drainsInto Katun River basin
linked to: Katun River
elevationRange high-mountain zone of Belukha massif
environmentalRole long-term water storage in solid form
regulation of seasonal river discharge
evolvesThrough glacial flow
feeds headwaters of the Katun River
formedBy long-term snow accumulation and compaction
hasClimate cold continental climate
hasPart cirque glaciers
firn fields
icefalls
valley glaciers
hasProcess glacial ablation
glacial accumulation
hasSurfaceFeature crevasses
seracs
snowfields
influences local climate around Belukha Mountain
regional hydrology of the Altai
locatedIn Altai Mountains
Golden Mountains of Altai UNESCO World Heritage Site
Russia
Siberia
partOf Altai glacier system
Ob River basin hydrological system
showsTrend recent glacier retreat
significance major freshwater reservoir for downstream ecosystems
one of the most important ice complexes in the Altai region
subjectOf glaciological research in the Altai
surrounds Belukha Mountain
usedFor mountaineering access routes
scientific expeditions

How these facts were elicited

Referenced by (3)

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

Belukha Mountain isCoveredBy Belukha Glacier system
Belukha Glacier system partOf Altai glacier system
linked to: Belukha Glacier system
East Belukha hasGlacier Belukha glaciers
linked to: Belukha Glacier system