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Influence of the lithological and geotechnical properties of rocks upon morphology of glacial valleys

Listed in NASA Earthdata CMR

The long and cross sectional forms of glacial valleys and cirques are a reflection of relationship between the abrasive and plucking processes occuring at the base of a glacier and the resistance of the bedrock mass to these processes.

Description

Field work was carried out to examine the forms of glacially eroded slopes and bedrock forms with respect to the Rock Mass Strength classification of Selby (1980, 1982) and to correlate this data with petrological and laboratory geomechanical characterisitics of rocks sampled in the field.

Samples and investigations took place in the Taylor, Wright, Upper and Victoria Valleys and the Asgaard and Olympus Ranges.

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Topics

Provenance · 1 source records, 11 field assertions
SourceKeyLast seenRaw
NASA Earthdata CMRC1214593317-SCIOPS15 d agoJSON v1
FieldAssertionExtractorEvidence
access_levelsource · NASA CMRconnector:nasa_cmr@1.0.0
concepts[instrument].gcmd_instrument:visual-observationssource · NASA CMRconnector:nasa_cmr@1.0.0
concepts[measured_variable].gcmd:earth-science/land-surface/erosion-sedimentation/erosionsource · NASA CMRconnector:nasa_cmr@1.0.0
concepts[measured_variable].gcmd:earth-science/land-surface/geomorphic-landforms-processessource · NASA CMRconnector:nasa_cmr@1.0.0
concepts[measured_variable].gcmd:earth-science/land-surface/geomorphic-landforms-processes/glacial-processessource · NASA CMRconnector:nasa_cmr@1.0.0
concepts[platform].gcmd_platform:field-investigationsource · NASA CMRconnector:nasa_cmr@1.0.0
descriptionsource · NASA CMRconnector:nasa_cmr@1.0.0/umm/Abstract
spatialsource · NASA CMRconnector:nasa_cmr@1.0.0/umm/SpatialExtent
temporalsource · NASA CMRconnector:nasa_cmr@1.0.0/umm/TemporalExtents
titlesource · NASA CMRconnector:nasa_cmr@1.0.0/umm/EntryTitle
version_labelsource · NASA CMRconnector:nasa_cmr@1.0.0