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Record W4322004963 · doi:10.5194/egusphere-egu23-8382

Investigation of prehistoric landslide dams in the central Andes of Chile and Argentina

2023· preprint· en· W4322004963 on OpenAlexaff
Sergio A. Sepúlveda, Stella M. Moreiras, Pilar Jeanneret, Mariana Correas González, Kimberly Bravo, Jacqueline Azanero, Marisol Lara

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEnvironmental Science
TopicLandslides and related hazards
Canadian institutionsSimon Fraser University
Fundersnot available
KeywordsLandslideGeologyHoloceneDeglaciationGlacial periodPleistocenePhysical geographyRange (aeronautics)GeomorphologyArchaeologyPaleontologyGeography

Abstract

fetched live from OpenAlex

Large volume landslides are common features in the high-topography Andes of central Chile and Argentina (31°-35°S). Many of these landslide deposits, mostly dating from Late Pleistocene to Holocene and related to a combination of deglaciation effects, seismicity and climate pattern changes, were large enough to block the glacial valleys and form landslide dams, some of which remain holding lakes until today. In this paper, we review and investigate some conspicuous landslide dams deposits from prehistoric times in the Andes Main Range in Chile and Argentina and the Andes Frontal Range in Argentina. A bibliographic review is followed by remote sensing analysis to obtain the main morphometric parameters of the landslides and the dams, complemented with field investigations in some of them. The landslide dams related with the rock slope failures of Portillo (1.1 km3, ~13 ka), Salto del Soldado (0.2 km3, 14- 9 Ka) Mesón Alto (4.3 km3, 4.7 Ka), Cortaderas-San Nicolás (2.4 km3, Holocene) and the Pangal complex (0.3 km3 , 40-11 ka) in the Chilean Western slope and the Laguna Blanca (81 hm3, ~12 ka), Horcones (0.35 km3, ~11-8 Ka), Negro (~18 Ka), Amarillo (~8Ka), and Laguna Atuel (56 hm3,~3 Ka) landslides in the Argentinean Eastern slope are described. Eldest rock avalanches associated with a seismic triggering mechanism that generate dammed lakes were previously studied in the Central Argentinean Andes such as Tigre Dormido (1.7 km3, ~46 Ka), Placetas Amarillas (1.6 km3, ~150 ka), and Piedras Blancas (0.89 km3, ~130 Ka). In these cases, the fine lake sequences reach 30 m in thickness but no outburst terraces were identified downstream, hardly supporting their catastrophic drainage.In both Chile and Argentina, most preserved damming collapses correspond in general to huge rock avalanches, even though some slides and debris flows also blocked narrow valleys. In general, studied ancient dams are isolated in mountain remote areas but they show evidences of catastrophic ruptures that emphases their importance in the cascade hazard scenarios. While the large majority of identified dams in the region are thousands of years old, some historic cases show that these processes still occur and pose a geological hazard. Given the large area that can be affected by outburst floods downstream the usually remote landslide sites, potentially impacting villages as well as mining, energy, and transportation infrastructure, these geohazards must be considered in risk reduction strategies in the Andean region.

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: none
GenreCandidate signal: Empirical · Consensus signal: none
Teacher disagreement score0.037
Threshold uncertainty score0.073

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0040.004
Science and technology studies0.0000.000
Scholarly communication0.0010.000
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 head0.023
GPT teacher head0.230
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

Citations0
Published2023
Admission routes1
Has abstractyes

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