Astoria Formation Are Exposed at Jumpoff Joe
COAS TAL LANDFORMS N EWPOR T - LI NCOLN C IT Y Vo l. 36 , No.5 M ay 1974 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES The Ore Bin Published Monthly By STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Head Office: 1069 State Office Bldg., Portland, Oregon - 97201 Telephone: 229 - 5580 FIELD OFFICES 2033 First Street 521 N. E. "E" Street Boker 97814 Grants Pass 97526 xxxxxxxxxxxxxxxxxxxx Subscription rate - $2.00 per colenc:br yeor Available bock issues $.25 each Second closs postage paid at Portland, Oregon GOVERNING BOARD R. W. deWeese, Portland, Chairman Willicwn E. Miller, Bend H. lyle Von Gordon, Grants Pass STATE GEOLOGIST R. E. Corcoran GEOLOGISTS IN CHARGE OF FIELD OFFICES Howard C. Brooks, Boker Len Romp, Grants Pass Permission i, gront.d to r.int information contained herein . Credit gillen the Stot. of Oregon o.pcrtment of Geology and Min.al Industri. for compiling thi, information will be appreciated. Stote of O r egon The ORE BIN Deportmentof Geology ond Minerol Indu$ITies Volum e 36,No.5 1069 Siote Office Bldg. May 1974 Portlond Oregon 97201 ROCK UNITS AND COASTAL LANDFORMS BETWEEN NEWPORT AND liNCOLN CITY, OREGON Ernest H. lund Deportment of Geology, University of Oregon The coost between Newport and lincoln City is composed of sedimen tary rock punctuated locally by volcanic rock. Where the shore is on sedi mentary rock, it is characterized by a long, sandy beach in front of a sea cliff. Perched above the sea cliff is the sandy marine terrace that fringes most of this segment of the Oregon coost.
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