克雷瓦塞山谷冰川是南极洲的冰川，位于玛丽伯德地，全长约50公里，流经彻斯特山脉和桑德斯山，最终注入苏兹贝格湾，该冰川在1934年11至12月由美国探险队发现。

Crevasse Valley Glacier (76°46′S 145°30′W / 76.767°S 145.500°W / -76.767; -145.500) is a broad glacier about 30 miles (50 km) long, flowing west-southwest between the Chester Mountains and the Saunders Mountain to the Sulzberger Ice Shelf in Marie Byrd Land, Antarctica. It was discovered by a sledging party of the Byrd Antarctic Expedition, which visited this area in November–December 1934, and so named because of its extensively crevassed surface.