أعرض تسجيلة المادة بشكل مبسط

dc.date 2006-10-20T23:21:59Z
dc.date 2006-10-20T23:21:59Z
dc.date 1974-11
dc.date.accessioned 2013-10-16T07:40:29Z
dc.date.available 2013-10-16T07:40:29Z
dc.date.issued 2013-10-16
dc.identifier http://hdl.handle.net/1957/3189
dc.identifier.uri http://koha.mediu.edu.my:8181/xmlui/handle/1957/3189
dc.description Bold, rocky headlands alternating with long curved beaches, sand spits, and bays -- these are the dominant landforms that make up the more than 40 miles of scenic coastline between Roads End and Tillamook Bay. With the exception of Cape Kiwanda, which is composed of sandstone, the headlands are made of basalt, a rock that erodes slowly. The lowlands and bays between the headlands are in more easily eroded sedimentary rock. Thus the coastline is scalloped by a sequence of large protrusions and indentations. Viewed in detail, however, there are numerous small shoreline features such as points, knobs, coves, and sea stacks that are due to local variations in bedrock characteristics.
dc.language en_US
dc.publisher Oregon Department of Geology and Mineral Industries
dc.relation The Ore bin
dc.relation vol. 36, no. 11
dc.relation Reports and Publications -- Other Reports and Publications
dc.relation Explorer Site -- Oregon Explorer
dc.relation Explorer Site -- North Coast Explorer
dc.subject Thematic Classification -- Geography and Geology -- Geology
dc.subject Thematic Classification -- Geography and Geology -- Geomorphology
dc.title The Ore bin ; Vol. 36 No. 11 (November 1974)
dc.type Technical Report


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أعرض تسجيلة المادة بشكل مبسط