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Statements

Subject Item
dbr:Glacier_morphology
rdfs:label
Glacier morphology Geomorfologia glaciale Glazialmorphologie 山谷冰川
rdfs:comment
Die Glazialmorphologie beschreibt und erklärt den Aufbau und die Entstehung der Oberflächenformen, die durch Gletscher und deren Schmelzwässer entstehen. La geomorfologia glaciale studia e descrive il prodotto dall'azione dei ghiacciai sulla superficie terrestre, la maggior parte delle aree oggi caratterizzate da questa morfologia sono state create dal movimento dei grandi ghiacciai continentali durante le . In alcune regioni, come la Fennoscandia e le Ande meridionali, se ne trovano grandi estensioni, mentre in altre come il Sahara sono state scoperte vecchie forme fossili di superfici rocciose modellate dal ghiaccio. 山谷冰川是指在高山雪線以上的冰原當中。如果冰層開始往下面移動,且過雪線後繼續下移,流動情形酷似山谷中的河川,因此稱為山谷冰川,简称谷冰川。山谷冰川的範圍是以雪線來當作界線。山谷冰川總長度可高達數十公里,厚達百米之多。因冰体自身的重量而会缓慢移动,速度一般为每年数十米至一、二百米。主要分布在高山地区,以阿尔卑斯山区的山谷冰川最为典型,故又称为阿尔卑斯冰川。 Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. Types of glaciers can range from massive ice sheets, such as the Greenland ice sheet, to small cirque glaciers found perched on mountain tops. Glaciers can be grouped into two main categories: * Ice flow is constrained by the underlying bedrock topography * Ice flow is unrestricted by surrounding topography
foaf:depiction
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dcterms:subject
dbc:Glaciology dbc:Geomorphology
dbo:wikiPageID
6633688
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1119653208
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dbo:thumbnail
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dbo:abstract
山谷冰川是指在高山雪線以上的冰原當中。如果冰層開始往下面移動,且過雪線後繼續下移,流動情形酷似山谷中的河川,因此稱為山谷冰川,简称谷冰川。山谷冰川的範圍是以雪線來當作界線。山谷冰川總長度可高達數十公里,厚達百米之多。因冰体自身的重量而会缓慢移动,速度一般为每年数十米至一、二百米。主要分布在高山地区,以阿尔卑斯山区的山谷冰川最为典型,故又称为阿尔卑斯冰川。 Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. Types of glaciers can range from massive ice sheets, such as the Greenland ice sheet, to small cirque glaciers found perched on mountain tops. Glaciers can be grouped into two main categories: * Ice flow is constrained by the underlying bedrock topography * Ice flow is unrestricted by surrounding topography Die Glazialmorphologie beschreibt und erklärt den Aufbau und die Entstehung der Oberflächenformen, die durch Gletscher und deren Schmelzwässer entstehen. La geomorfologia glaciale studia e descrive il prodotto dall'azione dei ghiacciai sulla superficie terrestre, la maggior parte delle aree oggi caratterizzate da questa morfologia sono state create dal movimento dei grandi ghiacciai continentali durante le . In alcune regioni, come la Fennoscandia e le Ande meridionali, se ne trovano grandi estensioni, mentre in altre come il Sahara sono state scoperte vecchie forme fossili di superfici rocciose modellate dal ghiaccio.
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