Earthquakes in Pacific Canada
Notice bibliographique
Résumé
Major earthquakes in Japan, New Zealand and Chile have made many Canadians wonder if the same thing could happen here. Those events remind us that earthquakes can cause major damage and possibly loss of life. Earthquake activity, is common across much of Canada. Each year, seismologists record and locate approximately 5,000 mostly small earthquakes across the country. Although scientists canmp;gt;'t predict when an earthquake will occur, research can help us take steps to prepare for, and reduce losses from, future earthquakes. Scientists with Natural Resources Canada study earthquakes around the world. That research helps us understand what could happen here and learn how we can better protect our homes and communities. Earthquake research is important to modern building codes, helping us create structures to withstand earthquake hazards. This is particularly important on the coast of British Columbia. The Pacific Coast is part of the Pacific Ring of Fire. and is the most earthquake-prone region in Canada. In fact, earthquakes occur every day on the west coast. In the offshore region to the west of Vancouver Island, more than 100 earthquakes of magnitude 5 or greater have occurred during the past 70 years. If these are near land, the shaking would be quite unsettling with dishes falling off shelves and minor damage occurring. Every 250 to 850 years, there is evidence of giant earthquakes of approximately 9 occurring off the west coast. These large mega thrust earthquakes can cause extensive damage to urban areas and are similar to the one that struck Japan in March 2011. In February 2010 a subduction earthquake hit the coast of Chile. Chile presents a compelling case study, and not only because its quake produced the kind of shaking that may affect Vancouver and Victoria. It also has in place similar building standards to those in Canada. John Cassidy of Natural Resources Canada had a chance to visit the area. That earthquake was a magnitude 8.8 and it occurred when an ocean plate just offshore of Chile was pushed beneath the continent. It moved about 20 meters, and it caused very strong shaking that people felt for two or three minutes. Here in British Columbia we have exactly the same type of tectonic setting. An ocean plate offshore is being pushed beneath Vancouver Island, Washington, and Oregon, and we have exactly the same type of earthquakes along our coast. We also know that our building codes are very similar to those in Chile, and so shortly after the earthquake I travelled with a group of earthquake engineers to Chile and we travelled through the hardest hit regions of the country to look at damage patterns and to learn what we can apply here in British Columbia. What we found was that the area of impact of that earthquake was huge -- 600 kilometres long, and going about 100 kilometres inland. It damaged buildings, and bridges, and highways, and seriously impacted the economy. In the coastal areas where there was very strong shaking there was also a tsunami 2 to 3 meters high, but in some areas ten or fifteen meters high and that tsunami came in twenty or thirty minutes after the earthquake, and in some cases a few hours, after the earthquake. What we found specifically was the oldest buildings were the hardest hit, those buildings that were constructed before modern building codes. Modern buildings in general did well, but there was still damage to the interior of those buildings, and there was a lot of damage to the outside with windows and bricks coming down. Modern building codes in Chile, the result of a lot of earthquake research, saved thousands and thousands of lives NRCanmp;gt;'s earthquake research helps us understand seismic activity and supports efforts across Canada to minimize damage to our roads, bridges, houses and communities. No one can say for sure when the next big earthquake will hit the Pacific coast, but by knowing what could happen, we better equip Canadians with the information they need to prepare. For more information, visit our website at EarthquakesCanada.ca and follow us on Twitter at Twitter.com slash Canadaquakes, to get the latest information on magnitude, location, and time of earthquakes in Canada.
Récupéré en direct depuis OpenAlex et désinversé. Les résumés ne sont pas conservés dans cette base de données : les index inversés représentent 8,6 Go des 9,3 Go de texte de la base, et le serveur dispose de 13 Go libres.
Comment cette classification a été obtenuedéplier
Prédiction distillée sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.
Scores Codex et Gemma par catégorie
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,000 | 0,000 |
| Méta-épidémiologie (sens strict) | 0,000 | 0,000 |
| Méta-épidémiologie (sens large) | 0,000 | 0,000 |
| Bibliométrie | 0,000 | 0,000 |
| Études des sciences et des technologies | 0,000 | 0,000 |
| Communication savante | 0,000 | 0,000 |
| Science ouverte | 0,001 | 0,000 |
| Intégrité de la recherche | 0,000 | 0,000 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,000 | 0,000 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
machine, non validéePrédiction automatique; un appel candidat d’une seule tête enseignante, pas un consensus.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».