Smith Glacier
Smith Glacier ( is a low-gradient Antarctic glacier, over 160 km long, draining from Toney Mountain in an ENE direction to Amundsen Sea. A northern distributary, Kohler Glacier, drains to Dotson Ice Shelf but the main flow passes to the sea between Bear Peninsula and Mount Murphy, terminating at Crosson Ice Shelf.Smith Glacier
- Type: Glacier
- Description: glacier in Marie Byrd Land, Antarctica
- Categories: ice stream and landform
- Location: Antarctica
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Satellite Map
Discover Smith Glacier from above in high-definition satellite imagery.
In Other Languages
From Bulgarian to Swedish—“Smith Glacier” goes by many names.
- Bulgarian: “Смит (ледник)”
- Bulgarian: “Смит”
- Cebuano: “Smith Glacier”
- Chinese: “史密斯冰川”
- German: “Smith-Gletscher”
- Hebrew: “קרחון סמית‘”
- Hebrew: “קרחון סמית’”
- Italian: “Ghiacciaio Smith”
- Norwegian Nynorsk: “Smithbreen”
- Swedish: “Smith Glacier”
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