noun ବିଶେଷ୍ୟ
/ˈɛskɚ/
(geology) a long winding ridge of post glacial gravel and other sediment
(ଭୂବିଜ୍ଞାନ) ପୋଷ୍ଟ ଗ୍ଲାସିଆଲ୍ କଙ୍କଡା ଏବଂ ଅନ୍ୟାନ୍ୟ ପଙ୍କର ଏକ ଲମ୍ବା ବୁଲୁଥିବା ରିଜ୍ |
noun ବିଶେଷ୍ୟ
1. A long, narrow, sinuous ridge created by deposits from a stream running beneath a glacier.
ଏକ ଗ୍ଲେସିୟର ତଳେ ଚାଲୁଥିବା ଏକ stream ରଣାରୁ ଜମା ଦ୍ୱାରା ସୃଷ୍ଟି ହୋଇଥିବା ଏକ ଲମ୍ବା, ସଂକୀର୍ଣ୍ଣ, ପାପପୂର୍ଣ୍ଣ ରିଜ୍ |
Another objection to the tunnel-valley interpretation comes from a comparison with eskers. The esker rivers and the tunnel-channel rivers of Wisconsin therefore seem to have been the result of significantly different meltwater regimes.
Another unusual ice-contact feature is an esker, a long, narrow, steep-sided ridge of glaciofluvial sand and gravel inhabiting a glaciated area. Eskers tend to follow valleys and lowlands, carefully picking a course between obstacles.
The multiple deltas must have formed sequentially, which led Thompson (1982) to conclude that the eskers were built in successive segments.
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