Krivodol Glacier
Krivodol Glacier is a 3.8 km long glacier on Smith Island, South Shetland Islands in Antarctica draining the southeast slopes of Imeon Range northeast and east of Antim Peak, southeast of Varshets Saddle and south of Slatina Peak.| Tap on a place to explore it |
Places of Interest
Highlights include Slatina Peak and Antim Peak.
Slatina Peak
Peak
Slatina Peak is a peak rising to 1691 m in Imeon Range on Smith Island, South Shetland Islands. Situated 2 km northeast of Antim Peak, to which it is linked by Varshets Saddle, 4.09 km east by south of Villagra Point, and 1.9 km south of Drinov Peak.
Antim Peak
Peak
Photo: Cfrohlich, Public domain.
Antim Peak is the ice-covered peak rising to 1,995 m in Imeon Range on Smith Island in the South Shetland Islands, Antarctica. Situated 2.25 km and 1.3 km northeast of the summit Mount Foster and Evlogi Peak, respectively, 5.4 km south-southwest of Mount Pisgah, 16 km southwest of Cape Smith, and 16 km northeast of Cape James.
Sevlievski Peak
Peak
Sevlievski Peak is the ice-covered peak rising to 1740 m in Imeon Range on Smith Island, South Shetland Islands. Situated 1 km south of Drinov Peak and 890 m north by east of Slatina Peak.
Krivodol Glacier
- Type: Glacier with an elevation of 1,719 metres
- Description: glacier in Antarctica
- Category: landform
- Location: Antarctica
- View on OpenStreetMap
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Satellite Map
Discover Krivodol Glacier from above in high-definition satellite imagery.
In Other Languages
From Cebuano to Swedish—“Krivodol Glacier” goes by many names.
- Cebuano: “Krivodol Glacier”
- Chinese: “克里沃多爾冰川”
- German: “Kriwodol-Gletscher”
- Hebrew: “קרחון קריבודול”
- Hebrew: “קרחון קריוודול”
- Italian: “Ghiacciaio Krivodol”
- Norwegian Nynorsk: “Krivodolbreen”
- Swedish: “Krivodol Glacier”
Notable Places Nearby
Highlights include Imeon Range and Vakarel Saddle.
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About Mapcarta. Text is available under the CC BY-SA 4.0 license, except for photos, directions, and the map. Description text is based on the Wikipedia page “Krivodol Glacier”. Photo: ravas51, CC BY-SA 2.0.