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Record W2909688394 · doi:10.4095/261329

Surficial geology, Lac La Hache, British Columbia

2009· report· en· W2909688394 on OpenAlexaffabout
A Plouffe

Bibliographic record

Venuenot available
Typereport
Languageen
FieldEarth and Planetary Sciences
TopicGeological Modeling and Analysis
Canadian institutionsNatural Resources Canada
Fundersnot available
KeywordsGeologyForestryPhysical geographyArchaeologyGeography

Abstract

fetched live from OpenAlex

The Lac la Hache map area (92P/14) dominantly lies within the Fraser Plateau physiographic region except for the valley of Lac la Hache which is part of the Fraser Basin. The Fraser Plateau is a region of rolling topography with an average elevation of approximately 1200 m above sea level and the Fraser Basin is the dissected portion of the plateau. The Lac la Hache map area includes an important drainage divide. A large part of the map area drains to the west towards Lac la Hache which empties into San Jose River, a tributary of Fraser River. The eastern sector of the map area drains to the east and is part of the North Thompson River drainage. The region is predominantly underlain by till which consists of a poorly sorted diamicton with clasts of all size. Bedrock outcrops are rare and limited in extent. In some of the valleys and the low areas, till is overlain by glaciofluvial sediments which were deposited in meltwater streams at the end of the last glaciation. Glaciolacustrine sediments, deposited in glacial lakes which formed at the end of the last glaciation, were mapped in the Bridge Creek, Lac la Hache, and the upper Bradley Creek valleys. Lacustrine sediments are present at the periphery of modern lakes throughout the map area. These were deposited at a time when the lakes occupied a higher level. Modern stream sediments (alluvium) are present in extent large enough to be mapped in some of the valleys. Colluvial deposits are mapped on steep slopes throughout the map area. One large landslide was mapped approximately 5 km south of Spring Lake. During the last glaciation, probably at glacial maximum, ice was dominantly moving to the south southwest to southeast as recorded by flutings, crag-and-tails, drumlins, and striations. However, an earlier phase of ice flow generally to the west is recorded by flutings southwest of Lang Lake, southeast of Rail Lake, and north of Timothy Lake. This first ice-movement is also recorded in the glacial striation record. During deglaciation, both the eastward and westward drainages were blocked by ice and/or sediments which lead to the development of glacial lakes in the valleys. A large partly buried valley, probably related to a Tertiary drainage system, extends southeast from Lac la Hache. This valley was in part eroded by glacial meltwater and hence is mapped as a large meltwater channel.

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)0.001
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 score0.027
Threshold uncertainty score0.091

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.004
Science and technology studies0.0030.000
Scholarly communication0.0020.000
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0270.003

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 head0.026
GPT teacher head0.233
Teacher spread0.207 · 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

Citations2
Published2009
Admission routes2
Has abstractyes

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