Bibliographic record
Abstract
Kyklo Creek (NTS 94I/11) map area was inundated by the Laurentide Ice Sheet during the late Wisconsinan glaciation (ca. 25 000 - 10 000 years ago). A thick blanket of clay and fine-silt-rich till was deposited by westward flowing ice across most of the region; glacial flow direction is depicted by west and southwestward-oriented flutings that also exhibit a rotation of flow around a bedrock-cored upland situated in the northeast part of the map. The area is dominantly flat, and covered extensively by bog and fen deposits. Thick peat accumulations (>2-3 m) locally form hummocky surfaces, accentuated by thermokarst (melt) of underlying discontinuous permafrost (units O1k, Ok). Hummocky till, including patterns interpreted to represent controlled moraines and crevasse-squeeze ridges lie only a few metres above the surrounding wetlands, and are typically covered by an aspen-dominated Boreal forest cover. Prominent ice-marginal channels that formed during regional deglaciation are depicted in the northwest part of the map area. There, a small glaciofluvial fan (unit Gf) provided a local aggregate source (now exhausted). It is likely that other such deposits occur in similar geographic associations, however, the ability to detect them is greatly limited by the extensive wetland and forest cover, in addition to the general difficulty accessing this terrain. Outcrops of Shaftesbury Formation shale bedrock are found in the northeast part of the map area. Only a thin till veneer mantles this bedrock-cored upland in contrast to the rest of the map area where borrow pits expose thickness of till >4-10 m.
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How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot 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.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.001 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.002 | 0.003 |
| Science and technology studies | 0.003 | 0.000 |
| Scholarly communication | 0.002 | 0.000 |
| Open science | 0.001 | 0.001 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.052 | 0.007 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
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".