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Record W2982165838 · doi:10.4095/226123

Earthquake damage in the Ottawa-Gatineau region between 1830 and 2008

2008· report· en· W2982165838 on OpenAlexaffabout
Maurice Lamontagne, M Sheshpari, Kamran A. Khan

Bibliographic record

Venuenot available
Typereport
Languageen
FieldEnvironmental Science
TopicLandslides and related hazards
Canadian institutionsNatural Resources Canada
Fundersnot available
KeywordsGeographySeismologyGeologyPhysical geography

Abstract

fetched live from OpenAlex

Based on its earthquake hazard and population, the seismic risk of the OttawaGatineau region ("the region '') ranks third in Canadian urban areas. As part of a research activity that aims at defining microseismic zoning for the region, the historical earthquake damage was examined The available written documents were searched for iriformation on damage related to some eighteen events that were most likely to have had some impact in the region. It was found that between years 1830 and 2008, thirteen of these earthquakes reached or exceeded the Modified Mercalli Intensity (MMI) V level (fallen smalt abjects). Being located within the Western Quebec Seismic Zone, the region was subjected to some moderate earthquakes (magnitude between 5.0 and 6.2) at less than 300 km epicentral distance. The local earthquakes of 1856, 1861, 1908, 1909, 1913, 1914, 1917, 1924, 1933, 1935, 1944 and 1983 Jal! in that category. More distant earthquakes had some impact in Ottawa in 1870, 1924 and 1925 (epicenters in the Charlevoix Seismic Zone at about 450-525 km epicentral distance), in 1929 (Attica, N Y. at about 350 km distance) and in 1988 (Saguenay region at about 470 km distance). The impact of these earthquakes in the Ottawa-Gatineau region was assembled in a database. For each earthquake, the database provides a description of damage together with ifs geographic coordinates, ifs corresponding MMI and the supporting document as scanned images. Historically, certain wards sustained higher levels of ground motions due to moderate to large earthquakes.We found that the 10-50 m thick basin centered on the Museum of Nature had most instances of MMI VI and VIL In contrast, areas with thin veneer of unconsolidateddeposits, such as the Parliament occurrences of damage. Since most earthquakes have occurred in the first half of the 20th century when Ottawa only occupied a small proportion of the current urban area, it is uncertain if the areas with most occurrences of damage present the highest risk for future earthquakes. Knowledge of these more hazardous areas, such as the basin centered on the Museum of Nature, is of importance for land use planning and emergency preparedness.Hill and the Hull ward of Gatineau had almost no occurrences of damage. Since most earthquakes have occurred in the first half of the 20th century when Ottawa only occupied a small proportion of the current urban area, it is uncertain if the areas with most occurrences of damage present the highest risk for future earthquakes. Knowledge of these more hazardous areas, such as the basin centered on the Museum of Nature, is of importance for land use planning and emergency preparedness.

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)0.001
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: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.025
Threshold uncertainty score0.120

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.003
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.025
GPT teacher head0.250
Teacher spread0.225 · 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

Citations1
Published2008
Admission routes2
Has abstractyes

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