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Record W36206867 · doi:10.1016/j.jep.2022.115774

Subglacial processes, glacier dynamics, and deglacial processes and patterns associated with the Cordilleran Ice Sheet around Okanagan Valley, British Columbia.

2012· dissertation· en· W36206867 on OpenAlexaboutno aff
Jérôme-Etienne Lesemann

Bibliographic record

VenueJournal of Ethnopharmacology · 2012
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicCryospheric studies and observations
Canadian institutionsnot available
FundersChina Postdoctoral Science FoundationNational Natural Science Foundation of China
KeywordsGeologyIce sheetGlacierAntarctic ice sheetDeglaciationOceanographyIce streamPhysical geographyGeomorphologyGlacial periodGeographyCryosphereSea ice

Abstract

fetched live from OpenAlex

This thesis explores subglacial processes, glacier dynamics, and deglacial processes and patterns associated with the Cordilleran Ice Sheet (CIS) in Okanagan Valley and the neighbouring Thompson Plateau in southern British Columbia. Reconstructions of subglacial processes in an area of streamlined bedforms (drumlins) on Thompson Plateau reveal that sediments within drumlins and in intervening areas record evidence of lodgement, deformation, poreflow, conduit flow, debris flows, and suspension settling of fines within a network of subglacial cavities. These subglacial cavities developed within a regional bedrock basin. These sediments demonstrate that substrate deformation is not a dominant and pervasive process recorded within the drumlins. Based on i) drumlin morphology, including the presence of stoss-side crescentic troughs and en echelon arrangement, ii) drumlin composition consisting of sediment and bedrock, it is argued that drumlins on Thompson Plateau have an erosional origin. Further, regional spatial associations between drumlins and tunnel valleys (including some in bedrock) on Thompson Plateau and in Okanagan Valley, and arguments relying on the continuity of eroded sediments suggest that erosion by subglacial meltwater underburst(s) best explains the range of observations. Underbursts may have been associated with development and drainage of a subglacial ‘catch lake’ in Okanagan Valley. High geothermal heat flux in Okanagan Valley could have favoured subglacial lake development. Subglacial volcanic eruptions may have acted as triggers for lakedrainage. Lastly, deglaciation of the CIS led to development of a proglacial lake in Okanagan Valley (glacial Lake Penticton - gLP). Sediment delivery to gLP occurred via tributary valleys and possibly from an ice tongue along the valley axis. Regional delta correlations record a highstand of gLP at 500-525 m asl followed by a single drainage event which eroded a portion of the lacustrine valley fill to produce distinctive remnant valley-side benches (‘White Silt’ terraces) of lacustrine sediments. No evidence of glacioisostatic tilting could be discerned within the gLP basin, this is tentatively ascribed to lithospheric conditions favouring rapid crustal rebound, and to thin ice with uniform thickness in the gLP basin.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.375
Threshold uncertainty score0.755

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.013
GPT teacher head0.241
Teacher spread0.227 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations1
Published2012
Admission routes1
Has abstractyes

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