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Also known as orogenesis, mountain building
地理地质学
Orogeny is the geological process that builds mountains, typically through the collision and deformation of Earth's crustal plates over millions of years. Understanding orogeny matters because it shapes the landscape we live on and helps explain the distribution of mountains, mineral resources, and geological hazards across our planet.
AI-generated from the Wikipedia summary — may contain errors.
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造山運動(英語:Orogeny)指地殼結構因為板塊運動產生劇烈變化,屬地殼變動的一種。該作用會產生岩石高度變形的帶狀區域,稱為造山帶(Orogens或Orogenic belts)。“Orogeny”一詞來自古希臘語詞根ὄρος(óros,山)和γενεια(geneia,誕生;起源)。造山運動是造成各大陸山地的主要機制;當大陸地殼因為造山運動產生褶皺和厚度增加時就形成山脈。涉及大範圍的地質作用統稱造運動(造運動?名詞需注解)。
Abstract from DBpedia / Wikipedia · CC BY-SA
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).
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