. "\u5C71\u8C37\u51B0\u5DDD\u662F\u6307\u5728\u9AD8\u5C71\u96EA\u7DDA\u4EE5\u4E0A\u7684\u51B0\u539F\u7576\u4E2D\u3002\u5982\u679C\u51B0\u5C64\u958B\u59CB\u5F80\u4E0B\u9762\u79FB\u52D5\uFF0C\u4E14\u904E\u96EA\u7DDA\u5F8C\u7E7C\u7E8C\u4E0B\u79FB\uFF0C\u6D41\u52D5\u60C5\u5F62\u9177\u4F3C\u5C71\u8C37\u4E2D\u7684\u6CB3\u5DDD\uFF0C\u56E0\u6B64\u7A31\u70BA\u5C71\u8C37\u51B0\u5DDD,\u7B80\u79F0\u8C37\u51B0\u5DDD\u3002\u5C71\u8C37\u51B0\u5DDD\u7684\u7BC4\u570D\u662F\u4EE5\u96EA\u7DDA\u4F86\u7576\u4F5C\u754C\u7DDA\u3002\u5C71\u8C37\u51B0\u5DDD\u7E3D\u9577\u5EA6\u53EF\u9AD8\u9054\u6578\u5341\u516C\u91CC\uFF0C\u539A\u9054\u767E\u7C73\u4E4B\u591A\u3002\u56E0\u51B0\u4F53\u81EA\u8EAB\u7684\u91CD\u91CF\u800C\u4F1A\u7F13\u6162\u79FB\u52A8\uFF0C\u901F\u5EA6\u4E00\u822C\u4E3A\u6BCF\u5E74\u6570\u5341\u7C73\u81F3\u4E00\u3001\u4E8C\u767E\u7C73\u3002\u4E3B\u8981\u5206\u5E03\u5728\u9AD8\u5C71\u5730\u533A\uFF0C\u4EE5\u963F\u5C14\u5351\u65AF\u5C71\u533A\u7684\u5C71\u8C37\u51B0\u5DDD\u6700\u4E3A\u5178\u578B\uFF0C\u6545\u53C8\u79F0\u4E3A\u963F\u5C14\u5351\u65AF\u51B0\u5DDD\u3002"@zh . . . . . . . "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: \n* Ice flow is constrained by the underlying bedrock topography \n* Ice flow is unrestricted by surrounding topography"@en . "Die Glazialmorphologie beschreibt und erkl\u00E4rt den Aufbau und die Entstehung der Oberfl\u00E4chenformen, die durch Gletscher und deren Schmelzw\u00E4sser entstehen."@de . . . . . . . . . . . . . . . . . . . . . . . . "Glacier morphology"@en . . . . . . . . . . . . . . "Geomorfologia glaciale"@it . . . . "1119653208"^^ . "16494"^^ . . . . . . . "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."@it . . "Die Glazialmorphologie beschreibt und erkl\u00E4rt den Aufbau und die Entstehung der Oberfl\u00E4chenformen, die durch Gletscher und deren Schmelzw\u00E4sser entstehen."@de . . . . . . . . . . . . . . . . . "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."@it . . . . . . . . . . . . . . . . "6633688"^^ . "\u5C71\u8C37\u51B0\u5DDD\u662F\u6307\u5728\u9AD8\u5C71\u96EA\u7DDA\u4EE5\u4E0A\u7684\u51B0\u539F\u7576\u4E2D\u3002\u5982\u679C\u51B0\u5C64\u958B\u59CB\u5F80\u4E0B\u9762\u79FB\u52D5\uFF0C\u4E14\u904E\u96EA\u7DDA\u5F8C\u7E7C\u7E8C\u4E0B\u79FB\uFF0C\u6D41\u52D5\u60C5\u5F62\u9177\u4F3C\u5C71\u8C37\u4E2D\u7684\u6CB3\u5DDD\uFF0C\u56E0\u6B64\u7A31\u70BA\u5C71\u8C37\u51B0\u5DDD,\u7B80\u79F0\u8C37\u51B0\u5DDD\u3002\u5C71\u8C37\u51B0\u5DDD\u7684\u7BC4\u570D\u662F\u4EE5\u96EA\u7DDA\u4F86\u7576\u4F5C\u754C\u7DDA\u3002\u5C71\u8C37\u51B0\u5DDD\u7E3D\u9577\u5EA6\u53EF\u9AD8\u9054\u6578\u5341\u516C\u91CC\uFF0C\u539A\u9054\u767E\u7C73\u4E4B\u591A\u3002\u56E0\u51B0\u4F53\u81EA\u8EAB\u7684\u91CD\u91CF\u800C\u4F1A\u7F13\u6162\u79FB\u52A8\uFF0C\u901F\u5EA6\u4E00\u822C\u4E3A\u6BCF\u5E74\u6570\u5341\u7C73\u81F3\u4E00\u3001\u4E8C\u767E\u7C73\u3002\u4E3B\u8981\u5206\u5E03\u5728\u9AD8\u5C71\u5730\u533A\uFF0C\u4EE5\u963F\u5C14\u5351\u65AF\u5C71\u533A\u7684\u5C71\u8C37\u51B0\u5DDD\u6700\u4E3A\u5178\u578B\uFF0C\u6545\u53C8\u79F0\u4E3A\u963F\u5C14\u5351\u65AF\u51B0\u5DDD\u3002"@zh . . . . . . . "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: \n* Ice flow is constrained by the underlying bedrock topography \n* Ice flow is unrestricted by surrounding topography"@en . . "Glazialmorphologie"@de . . "\u5C71\u8C37\u51B0\u5DDD"@zh . . . . . . . . . . . .