A proglacial river is a river that flows from the margin of a glacier. These rivers are strongly affected by the highly-seasonal water supply from the glacier and by the large supply of sediment that arrives at the glacier terminus. This high sediment supply often makes them steep and braided. Many modern proglacial rivers drain glaciers in the mountain ranges of Alaska and the Himalayas. Past and present proglacial rivers in front of large ice sheets deposited large outwash plains of sediment.
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| - Sungai Proglasial (in)
- Proglacial river (en)
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| - A proglacial river is a river that flows from the margin of a glacier. These rivers are strongly affected by the highly-seasonal water supply from the glacier and by the large supply of sediment that arrives at the glacier terminus. This high sediment supply often makes them steep and braided. Many modern proglacial rivers drain glaciers in the mountain ranges of Alaska and the Himalayas. Past and present proglacial rivers in front of large ice sheets deposited large outwash plains of sediment. (en)
- Sungai proglasial adalah sungai yang mengalir dari tepi gletser . Sungai-sungai ini sangat dipengaruhi oleh pasokan air es yang mencair dan bersifat sangat musiman, serta dipengaruhi oleh pasokan sedimen besar yang sampai di ujung gletser. Pasokan sedimen yang tinggi ini sering kali membuatnya curam dan teranyam . Banyak sungai proglasial modern yang mengering, seperti di pegunungan Alaska dan Himalaya. (in)
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| - A proglacial river is a river that flows from the margin of a glacier. These rivers are strongly affected by the highly-seasonal water supply from the glacier and by the large supply of sediment that arrives at the glacier terminus. This high sediment supply often makes them steep and braided. Many modern proglacial rivers drain glaciers in the mountain ranges of Alaska and the Himalayas. Past and present proglacial rivers in front of large ice sheets deposited large outwash plains of sediment. (en)
- Sungai proglasial adalah sungai yang mengalir dari tepi gletser . Sungai-sungai ini sangat dipengaruhi oleh pasokan air es yang mencair dan bersifat sangat musiman, serta dipengaruhi oleh pasokan sedimen besar yang sampai di ujung gletser. Pasokan sedimen yang tinggi ini sering kali membuatnya curam dan teranyam . Banyak sungai proglasial modern yang mengering, seperti di pegunungan Alaska dan Himalaya. (in)
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