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Record W6948240197 · doi:10.5066/p13axwaa

Morphometric Landslide Susceptibility Results of the Northwestern United States and Southwestern Canada Derived from Elevation Data

2025· dataset· en· W6948240197 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueUSGS DOI Tool Production Environment · 2025
Typedataset
Languageen
FieldEnvironmental Science
TopicParasite Biology and Host Interactions
Canadian institutionsnot available
Fundersnot available
KeywordsLandslideLogistic regressionElevation (ballistics)TerrainWatershedSampling (signal processing)Regression

Abstract

fetched live from OpenAlex

Landslide susceptibility models show the potential of landslide occurrence at a location. These models are pivotal for reducing losses associated with landslides (Godt and others, 2022). In this data release, we include susceptibility results from the associated manuscript by Woodard and Mirus (2025). This manuscript shows how a morphometric model can create consistent and effective susceptibility models over large regions (> 100 km2) by analyzing the terrain’s topography. The model assumes that areas with high relative slope and hillslope area in comparison to the rest of the terrain are more susceptible to landsliding. As the model’s only input is elevation data, it mitigates the data biases common in the data-driven statistical methods (e.g., machine learning) generally used over these scales. We compare the morphometric model outputs to a parsimonious national susceptibility map and logistic regression machine learning models. The national susceptibility map is available in Belair and others, (2024). The two logistic regression models are trained on the landslide data available in the Willamette Valley Hydrologic Unit Code (HUC) 4 watershed (Oregon Department of Geology and Mineral Industries [DOGAMI], 2024). To account for the effects of the sampling ratio of event to non-event data points, we create two logistic regression models. The first uses a 1:1 sampling ratio of landslide to non-landslide points and the second uses all the data within the training data which results in a 1:33 sampling ratio. Environmental datasets requisite for the logistic regression models are all derived from the three-dimensional elevation program (3DEP) (U.S. Geological Survey, 2019a) preprocessed within the National Hydrography Dataset (U.S. Geological Survey, 2019b). The morphometric model was derived using only the 3DEP dataset without any input of where landslides have occurred. All model outputs are shown with slope units. This data release includes the following files: 1) logistic regression results with 1:1 sampling ratio over Willamette Valley HUC4 watershed (1709) (Logistic_1709_1.zip); 2) logistic regression results with 1:33 sampling ratio over Willamette Valley HUC4 watershed (1709) (Logistic_1709_All.zip); 3) morphometric results with uniform weights over the Willamette Valley HUC4 watershed (1709) (Morph_Uniform_1709.zip); 4) morphometric results with area weights over the 1701 HUC 4 watershed (Morph_Area_1701.zip); 5) morphometric results with area weights over the 1702 HUC 4 watershed (Morph_Area_1702.zip); 6) morphometric results with area weights over the 1703 HUC 4 watershed (Morph_Area_1703.zip); 7) morphometric results with area weights over the 1704 HUC 4 watershed (Morph_Area_1704.zip); 8) morphometric results with area weights over the 1705 HUC 4 watershed (Morph_Area_1705.zip); 9) morphometric results with area weights over the 1706 HUC 4 watershed (Morph_Area_1706.zip); 10) morphometric results with area weights over the 1707 HUC 4 watershed (Morph_Area_1707.zip); 11) morphometric results with area weights over the 1708 HUC 4 watershed (Morph_Area_1708.zip); 12) morphometric results with area weights over the 1709 HUC 4 watershed (Morph_Area_1709.zip); 13) morphometric results with area weights over the 1710 HUC 4 watershed (Morph_Area_1710.zip); 14) morphometric results with area weights over the 1711 HUC 4 watershed (Morph_Area_1711.zip); 15) morphometric results with area weights over the 1712 HUC 4 watershed (Morph_Area_1712.zip). 16) shape file field descriptors (Field_Descriptors.txt) Each zip-file contains the vector shapefiles of interest, which can be extracted using most archiver software. References Cited Belair, G.M., Jones, J.M., Martinez, S.N., Mirus, B.B., and Wood, N.J., 2024, Slope-relief threshold landslide susceptibility models for the United States and Puerto Rico: U.S. Geological Survey data release, accessed January 21, 2024, at https://doi.org/10.5066/P13KAGU3 Godt, J.W., Wood, N.J., Pennaz, A.B., Mirus, B.B., Schaefer, L.N., and Slaughter, S.L., 2022, National Strategy for Landslide Loss Reduction: U.S. Geological Survey Open-File Report 2022–1075, 36 p. Oregon Department of Geology and Mineral Industries [DOGAMI], 2024, Statewide Landslide Information Database for Oregon [SLIDO]: accessed January 21, 2024, at https://www.oregon.gov/dogami/slido/Pages/data.aspx U.S. Geological Survey, 2019a, 3D Elevation Program 1/3 arcsecond: U.S. Geological Survey website, accessed January 21, 2024, at https://apps.nationalmap.gov/downloader/ U.S. Geological Survey, 2019b, U.S. Geological Survey National Hydrography Dataset Plus High Resolution: U.S. Geological Survey website, accessed January 21, 2024, at https://apps.nationalmap.gov/downloader/ Woodard, J.B., Mirus, B.B., 2025, Overcoming the data limitations in landslide susceptibility modelling: Science Advances, v. 11, no. 8, doi:10.1126/sciadv.adt1541.

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.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Dataset · Consensus signal: Dataset
Teacher disagreement score0.392
Threshold uncertainty score0.896

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 science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.017
GPT teacher head0.258
Teacher spread0.241 · 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