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| INTRODUCTION TO THE GEOMORPHOLOGICAL PATTERN ON THE CAPE COD PENINSULA |
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| Abstract: |
| Cape Cod peninsula, located in the southeast of the massachusetts state, was formed by the accumulation of the moraine after the glacier melted in the late pleistocene and early Holocene. The moraine knobs, moraine plane, accumulated sand and gravel coast, erosional coast such as sea scarp and coastal dune etc. geomorphological patterns were evolved on the Cape Cod peninsula. Some part of the coast were effectively protected and utilized fay the resident but most of it still not been protected. |
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