Cryopedology, CRYOPEDOLOGYCRYOTURBATION, CRYOPEDOLOGYCRYONIVATION AND CRYOPEDOLOGYcryoplanation
Bibliographic record
Abstract
Andersson, J. G., 1906, Solifluction, a component of subaerial denudation, J. Geol., 14, 91–112. Google Scholar Baulig, H., 1957, Peneplains and pediplains, Bull. Geol. Soc. Am., 68, 913–930 (translated by C. A. Cotton). Google Scholar Beskow, G., 1930, Erdfliessen und Structurböden der Hochgebirge im Licht der Frosthebung, Geol. Foren. Stockholm Forh., 52, 622–637. Google Scholar Bryan, K., 1946, Cryopedology, the study of frozen ground and intensive frost action with suggestions on nomenclature, Am. J. Sci., 244, 622–642. Google Scholar Bryan, K., 1949, The geologic implications of cryopedology, J. Geol., 57, 101–104. Google Scholar Butrym, J., Cegla, J., Dzulynski, S., and Nakonieczny, S., 1964, New interpretation of periglacial structures, Akad. Nauk (Krakow). Folia Quaternaria, 34pp. Google Scholar Cailleux, A., 1948, Étude de cryopédologie, Expéd. polaires franç., Miss. Paul E. Victor, Paris, C.D.U., 8pp. Google Scholar Cairnes, D. D., 1912a, Differential erosion and equiplanation in portions of Yukon and Alaska, Bull. Geol. Soc. Am., 23, 333–348. Google Scholar Cairnes, D. D., 1912b, Some suggested new physiographic terms (equiplanation, deplanation and aplanation), Am. J. Sci., Ser. 4, 34, 75–87. Google Scholar De Terra, H., 1940, Some critical remarks concerning W. Penck's theory of piedmont benchlands in mobile mountain belts, Symposium, Walter Penck's Contrib. to Geomorph., ed. von Engeln, Ann. Assoc. Am. Geogr., 30, 241–246. Google Scholar Eakin (Iakim), H. M., 1916, The Yukon-Koyukuk region, Alaska, Bull. U.S. Geol. Surv., 631, 67–82. Google Scholar Edelman, C. H., Florschutz, F., and Jeswiet, J., 1936, Über spätpleistozäne und frühholozäne kryoturbate Ablagerungen in den östl. Niederlanden, Verhandel. Geol. Mijbouwk. Ned. Kolonien, Geol. Ser. , XI, 4, 301–336. Google Scholar Gripp, K., and Simon, W. G., 1933, Experiments zum Brodelbodenproblem, Centralbl. f. Min. , Abt. B, 433–440. Google Scholar Gripp, K., and Simon, W. G., 1934, Nochmals zum Problem des Brodelbodens, Centralbl. f. Min. , Abt. B, 283–286. Google Scholar Guillien, Y., 1949, Gel et dégel du sol: les méchanismes morphologiques, L'Information Géographique (Paris), 13, 104–116. Google Scholar Guillen, Y., 1951, Cyropédologie? périglaciaire?, Ann. Géogr., 60, 52–54. Google Scholar Guillien, Y., Marcelin, P., and Rondeau, A., 1951, Le modelé cryonival autour de Nimes et d'Avignon, Compt. Rend. Acad. Sci. (Paris), 253, 1131–1132. Google Scholar Hamelin, L. E., and Clibbon, P., 1962, Vocabulaire périglaciaire bilingue (français et anglais), Cahiers de Géographie de Quebec , No. 12, 201–226. Google Scholar Hamelin, L. E., and Cook, F. A., 1965, Illustrated Glossary of Periglacial phenomena. Le périglaciaire par l'image, Geographical Branch-Direction de la Géographie, Ministère des Mines, Ottawa. Google Scholar Lozinski, W., 1909, Ueber die mechanische Verwitterung der Sandstein im gemässigten Klima, Acad. Sci. de Cracovie (Cl. des. Sci., Math. et Nat.) Bull., 1–25. Google Scholar Muller, S. W., 1947, Permafrost or Permanently Frozen Ground and Related Engineering Problems, Ann Arbor, Edwards Bros. 231pp. (Strateg. Eng. Study 62, U.S. Army, 1945). Google Scholar Paterson, T. T., 1941, On a world correlation of the Pleistocene, Trans. Roy. Soc. Edinburgh, 60, Pt. 2, 373 435. Google Scholar Raup, H. M., 1951, Vegetation and cryoplanation, Ohio J. Sci., 51, 105–116. Google Scholar Salomon-Calvi, W., 1929, Arktische Bodenformen in der Alpen, Heidelberger Akad. der Wiss. (Math-natur. Kl.), 1–31. Google Scholar Sharp, R. P., 1942a, Periglacial involutions in north-eastern Illinois, J. Geol., 50, 113–133. Google Scholar Sharp, R. P., 1942b, Soil structures in the St. Elia's Range, Yukon Territory, J. Geomorphol., 5, 274–301. Google Scholar Sharpe, C. F. S., 1938, Landslides and related phenomena, a study of mass-movements of soil and rock, New York, Columbia University Press, 137pp. Google Scholar Taber, S., 1929, Frost heaving, J. Geol., 37, 428 461. Google Scholar Taber, S., 1930, The mechanics of frost heaving, J. Geol., 38, 303–317. Google Scholar Cross-references Altiplanation ; Cirque ; Colluvium ; Cryology , etc.; Frost Action ; Frost Heaving ; Frost Riving ; Head ; Mass Movement ; Mass Wasting ; Moraine ; Nivation ; Patterned Ground ; Periglacial Landscapes ; Permafrost ; Regolith and Saprolite ; Rock Stream ; Slopes ; Soil Creep ; Solifluction . Download references
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 imitationNot 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.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.001 | 0.000 |
| Meta-epidemiology (narrow) | 0.001 | 0.001 |
| Meta-epidemiology (broad) | 0.001 | 0.000 |
| Bibliometrics | 0.001 | 0.000 |
| Science and technology studies | 0.001 | 0.001 |
| Scholarly communication | 0.000 | 0.002 |
| Open science | 0.001 | 0.000 |
| Research integrity | 0.002 | 0.003 |
| Insufficient payload (model declined to judge) | 0.007 | 0.001 |
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; both teacher heads agree on what is shown here.
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".