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Record W4411927571 · doi:10.1111/bor.70027

Morphology and sedimentology of murtooized terrain on the southern Fraser Plateau, British Columbia, Canada

2025· article· en· W4411927571 on OpenAlexafffundabout
Alexander D. Sodeman, Tracy A. Brennand

Bibliographic record

VenueBoreas · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsSimon Fraser University
FundersNatural Sciences and Engineering Research Council of Canada
KeywordsSedimentologyGeologyPlateau (mathematics)TerrainMorphology (biology)GeomorphologyArchaeologyPaleontologyPhysical geographyGeographyCartography

Abstract

fetched live from OpenAlex

Recent public releases of Light Detection and Ranging (LiDAR) data in south central British Columbia (BC), Canada have revealed several landforms resembling ‘murtoos’, previously identified across portions of Scandinavia. In this study, we investigate the morphology and sedimentology of these landforms, the first report of their kind associated with the Cordilleran Ice Sheet (CIS). From remote observations using LiDAR data, we determined that these landforms do not fit the classification scheme of murtoos used by previous authors, and based on our own observations, we use the term ‘murtooized terrain’, due to their superficial similarities with Scandinavian murtoos. Murtooized terrain consists of 1–8 m high, distinctly steep slopes that can continue laterally up to 2 km, changing in orientation along their lateral lengths, creating angular, zig‐zag patterns. It can present as dense, subparallel groupings of slopes giving a washboard appearance. Murtooized terrain occurs in several landscape associations including till plains, ribbed terrain, isolated plateaus and near meltwater corridors. Murtooized terrain in association with till plains and ribbed terrains exhibits distinct hill‐hole pairs. It typically consists of diamicton interpreted as a regional till sheet winnowed by persistent subglacial groundwater flow, sometimes overlain by melt‐out till and covered with a surface veneer of silt and very fine sand interpreted as loess. Massive sand deposited by postglacial overland flows can fill small troughs at the foot of murtooized terrain slopes. The following event sequence explains the formation of murtooized terrain. The concentration of subglacial groundwater flow through very broad topographic troughs winnowed till and resulted in strong ice‐bed coupling through basal ice regelation. Following channelized subglacial floods (underbursts) associated with the formation of large (Chasm and Green Lake) meltwater corridors, the CIS underwent collapse and ice surface slopes were reorganized in the adjacent region. Murtooized terrain formed due to widespread, short‐term, glaciotectonism associated with this reorganization where the ice and bed were well coupled. Zig‐zag slopes and hill‐hole pairs are attributed to spatial variations in coupling. Stagnation followed forming melt‐out till and crevasse fill ridges. This hypothesis is distinctly different from those developed for the Scandinavian murtoos, suggesting either that the superficial similarities between BC murtooized terrain and Scandinavian murtoos are the products of formational equifinality or that the BC murtooized terrain is a distinct landform.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.039
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.008
GPT teacher head0.203
Teacher spread0.195 · 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 teacher head, not a consensus.

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
Published2025
Admission routes3
Has abstractyes

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