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Creator:: Oregon. Dept. of Geology and Mineral Industries and Lund, Ernest H.
Resource Type:: Journal
Full Text:: 97201 The ORE BIN Volume 35,no.12 December 1973 LANDFORMS ALONG THE COAST OF SOUTHERN COOS COUNTY

Creator:: Oregon. Dept. of Geology and Mineral Industries and Baldwin, Ewart Merlin, 1915-
Resource Type:: Journal
Full Text:: 1943 in connection with the State of Oregon-Coos County coal project (Allen and Baldwin, 1944) and has

Creator:: Oregon. Dept. of Geology and Mineral Industries and Lund, Ernest H.
Abstract:: This study is concerned with the post-Ice Age (Holocene) dunes in the coast segment between Coos Bay on the south and Sea Lion Point on the north. This is the longest strip of dunes along the Oregon coast and extends for a distance of about 55 miles. It is divided...
Resource Type:: Journal
Full Text:: exception of Curry County south of Port Orford, dunes are a common landform along the Oregon coast. Older

Creator:: Oregon. Dept. of Geology and Mineral Industries and Hopkins, William Stephen, 1931-
Resource Type:: Journal
Full Text:: , J., 1967, Geology of state parks near Cape Arago, Coos County, Oregon: The ORE BIN, v. 29, p. 61-82

Creator:: Oregon. Dept. of Geology and Mineral Industries and Lund, Ernest H.
Abstract:: 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...
Resource Type:: Journal
Full Text:: of the formation on this part of the Coast begins south of Cape Look- out, where it is exposed in

Creator:: Oregon. Dept. of Geology and Mineral Industries and Lund, Ernest H.
Abstract:: The 26-mile stretch of shore extending from Florence to Yachats is one of the most rugged and scenic parts of the Oregon Coast. Along most of this part of the coast the shore is bounded by basalt bedrock of varied types. Through differential erosion of the basalt, the many landforms,...
Resource Type:: Journal
Full Text:: Pleistocene to the present, ex- tend from the headlands south of Sea Lion Point (Fig. 6.) southward to Coos

Creator:: Oregon. Dept. of Geology and Mineral Industries and Lund, Ernest H.
Resource Type:: Journal
Full Text:: -mile stretch of the Oregon coast between Tillamook Bay and the Columbia River can be divided into three

Creator:: Oregon. Dept. of Geology and Mineral Industries, McKee, Thomas M., Orr, William N., 1939-, and Weinstein, B. B.
Resource Type:: Journal
Full Text:: localities south of Bandon as well as from submarine exposures off the Oregon coast (see figure 1). Figure 1

Creator:: Oregon. Dept. of Geology and Mineral Industries, Emilia, David A., Berg, Joseph W., Bales, W. E., and Wagner, Norman Spencer
Resource Type:: Journal
Full Text:: three miles from Susanville, Grant County, Oregon. By early the next morning news of the discovery was

Creator:: Oregon. Dept. of Geology and Mineral Industries and Lund, Ernest H.
Resource Type:: Journal
Full Text:: of Port Orford, and Floras Lake, a few miles south of the Coos-Curry County line, were formed by

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