Statements (107)
| Predicate | Object |
|---|---|
| gptkbp:instance_of |
gptkb:glacier
|
| gptkbp:accessibility |
difficult
accessible via air travel |
| gptkbp:climate |
polar climate
collected from ice cores important for Antarctic climate research |
| gptkbp:climate_impact |
global sea levels
important for global climate models |
| gptkbp:collaborations |
international research teams
collaborations with universities |
| gptkbp:conducts_research_on |
glaciology
|
| gptkbp:conducts_surveys_on |
gptkb:New_Zealand_Antarctic_Research_Program
|
| gptkbp:coordinates |
83° S 168° E
|
| gptkbp:diameter |
up to 1,000 meters
significant ice mass |
| gptkbp:discharge |
Beardmore Glacier Ice Stream
|
| gptkbp:discovered_by |
gptkb:Robert_Falcon_Scott
|
| gptkbp:discovery_year |
1902
|
| gptkbp:emergency_services |
conducted for climate studies
|
| gptkbp:environmental_concerns |
climate change
climate change impact |
| gptkbp:environmental_impact |
conducted in the region
|
| gptkbp:environmental_initiatives |
monitored for changes
|
| gptkbp:expedition |
gptkb:British_Antarctic_Expedition
used by early explorers part of early 20th-century explorations |
| gptkbp:first_ascent |
1902
|
| gptkbp:flows_into |
gptkb:Ross_Ice_Shelf
|
| gptkbp:funding |
funded by various grants
|
| gptkbp:geological_features |
crevasses
seracs observed in recent decades moraines and outwash plains shapes surrounding landscape study of ice cores important for studying past climate site for glaciological research. |
| gptkbp:geological_formation |
conducted by geological teams
|
| gptkbp:glacial_monitoring |
ongoing monitoring programs
|
| gptkbp:glaciological_research |
site for scientific studies
|
| gptkbp:historical_expeditions |
gptkb:Scott's_Antarctic_Expedition_1910-1913
|
| gptkbp:historical_significance |
early 20th century exploration
used in early Antarctic expeditions |
| https://www.w3.org/2000/01/rdf-schema#label |
Beardmore Glacier
|
| gptkbp:ice_core_samples |
collected for analysis
|
| gptkbp:ice_flow |
dynamic movement
|
| gptkbp:ice_flow_direction |
northward
|
| gptkbp:ice_flow_dynamics |
studied for understanding ice movement
|
| gptkbp:ice_flow_rate |
varies with seasons
|
| gptkbp:ice_thickness_variability |
varies across the glacier
|
| gptkbp:is_explored_in |
gptkb:Robert_Falcon_Scott
Antarctic expeditions |
| gptkbp:landforms |
Mounts of the Queen Alexandra Range
|
| gptkbp:landscape |
gptkb:Queen_Alexandra_Range
|
| gptkbp:length |
about 30 kilometers
about 100 kilometers |
| gptkbp:location |
gptkb:Antarctica
|
| gptkbp:map |
gptkb:USGS
topographic surveys satellite imagery used |
| gptkbp:named_after |
Sir William Beardmore
|
| gptkbp:notable_features |
icefalls and crevasses
|
| gptkbp:part_of |
gptkb:Ross_Dependency
gptkb:Queen_Alexandra_Range |
| gptkbp:photography |
scientific documentation
|
| gptkbp:publication |
numerous studies published
|
| gptkbp:research |
environmental monitoring
remote sensing climate change impacts glacial retreat glacial geology paleoclimate data climate modeling climate patterns climate variability glacial hydrology paleoenvironments geophysical surveys glacial erosion glacial landforms climate feedback mechanisms glacial dynamics ecosystem impacts ice melt rates ice sheet stability ice age research ice core analysis glacial isostatic adjustment glacial sedimentology ice flow modeling |
| gptkbp:research_focus |
paleoclimate reconstruction
|
| gptkbp:research_importance |
key for understanding glacial dynamics
|
| gptkbp:research_institutes |
various universities
various Antarctic research programs |
| gptkbp:significance |
gptkb:scientific_research
|
| gptkbp:surrounding_area |
gptkb:Transantarctic_Mountains
gptkb:Queen_Alexandra_Range |
| gptkbp:terrain |
characterized by rugged terrain
|
| gptkbp:tourism |
limited access
|
| gptkbp:width |
about 5 kilometers
|
| gptkbp:wildlife |
gptkb:birds
gptkb:seals penguins penguins and seals |
| gptkbp:zone |
polar climate
|
| gptkbp:bfsParent |
gptkb:Scott's_Last_Expedition_1910-1913
|
| gptkbp:bfsLayer |
6
|