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3 edition of Stratigraphy and fauna of the Astoria Miocene of southwest Washington found in the catalog.

Stratigraphy and fauna of the Astoria Miocene of southwest Washington

Thomas John Etherington

Stratigraphy and fauna of the Astoria Miocene of southwest Washington

by Thomas John Etherington

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  • 16 Currently reading

Published by University of California Press in Berkeley, Calif .
Written in English

    Subjects:
  • Paleontology -- Miocene,
  • Paleontology -- Washington (State)

  • Edition Notes

    Statementby Thomas John Etherington.
    SeriesUniversity of California publications. Bulletin of the Department of Geological Sciences, v.20, no.5, University of California publications in geological sciences -- v. 20, no. 5.
    The Physical Object
    Paginationp. vi, [31]-142, [1] leaf of plates [i.e. plates 1-14]
    Number of Pages142
    ID Numbers
    Open LibraryOL13539337M
    LC Control Number31000539
    OCLC/WorldCa5959376

    Wesselingh et al. Stratigraphy of Miocene Amazonian deposits. Scripta Geol., () (Pilsbry & Olsson, ) might form a second co-occurring biostratigraphic indicator. Both the fauna from the Middle Magdalena basin referred to in literature as the ‘La Cira. Foraminifera, Stratigraphy, and Paleoecology of the Quinault Formation, Point Grenville-Raft River Coastal Area, Washington.

    Stratigraphic and Structural Interpretation of Willapa Basin. Stephen P. Palmer. Willapa basin is a middle Eocene to Holocene depocenter in southwestern Washington and on the adjacent continental shelf. Surface geology, biostratigraphy, and seismic and well data have been used to develop a stratigraphic and structural interpretation of the basin. The Miocene (/ ˈ m aɪ. ə ˌ s iː n, ˈ m aɪ. oʊ-/ MY-ə-seen, MY-oh-) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Charles Lyell; its name comes from the Greek words μείων (meiōn, "less") and καινός (kainos, "new") and means "less recent" because it has 18% fewer modern sea invertebrates than the Pliocene.

    that the Astoria Formation overlaps the Nye Mudstone and rests on the upper Oligocene Yaquina Formation about 8~ miles north of this stop. The Nye-Astoria contact is best exposed at Jumpoff Joe (fig. 2), 1~ miles north of Stop 1. Marine Pleistocene terrace deposits overlie both Miocene units at this stop. To the north along the beach, mas­. Geology, Stratigraphic -- Miocene. See also what's at your library, or elsewhere. Broader terms: Geology, Stratigraphic; Geology, Stratigraphic -- Neogene; Narrower.


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Stratigraphy and fauna of the Astoria Miocene of southwest Washington by Thomas John Etherington Download PDF EPUB FB2

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Buy Stratigraphy and fauna of the Astoria Miocene of southwest Washington, (University of California publications. Bulletin of the Department of Geological Sciences) by Etherington, Thomas John (ISBN:) from Amazon's Book Store.

Everyday low Author: Thomas John Etherington. Etherington, F.J.,Stratigraphy and fauna of the Astoria Miocene of southwest Washington: University of California Publications in Geological Sciences, v.

20, no. 5, p.(incl. geologic map, scale approx. ,) author redescribes unit as the "Astoria formation" and presents good historical summary and description of "best. The Mascall fauna is a well-known middle Miocene (Barstovian) mammalian assemblage in the Pacific Northwest. It has been collected for over years and collecting intensity has increased since the establishment in of a national monument enclosing the type area of the by: 1.

Mark L. Ferns, Jason D. McClaughry, "Stratigraphy and volcanic evolution of the middle Miocene to Pliocene La Grande–Owyhee eruptive axis in eastern Oregon", The Columbia River Flood Basalt Province, Stephen P.

Reidel, Victor E. Camp, Martin E. Ross, John A. Wolff, Barton S. Martin, Terry L. Tolan, Ray E. Wells. Download citation file. A sequence of early to middle Miocene, continental and marine beds of conglom- erate, sandstone, and siltstone, exposed in the southwest- ernmost portion of Washington, is tentatively correlated with the Astoria Formation of Oregon on the basis of their contained fauna, their stratigraphic position, and their lithologic characteristics (RAU; SNAVELEYet al.

Paleontology and stratigraphy of the Miocene Saddleback Valley limestone, Orange County, Southern California Article (PDF Available) November with 1, Reads How we. Full text of "The post-Eocene formations of Western Washington" See other formats PROCEEDINGS OF TIIF CALIFORNIA ACADEMY OF SCIENCES Fourth Series Vol.

VI, No. 2, pp. May 6, II THE POST-EOCENE FORMATIONS OF WESTERN WASHINGTON BY Charles E. Weaver Assistant Professor of Geology, University of Washington, Seattle. Paleomagnetism of the Oligocene and Miocene Lincoln Creek and Astoria formations, Knappton, Washington.

Natural History Museum of Los Angeles County Science Series Molluscan fauna of the “Miocene" Namigata Formation in the Namigata area, Okayama Prefecture, southwest Japan.

H.,The Miocene of Astoria and Coos Bay, Oregon. Paleogene and lower Neogene biochronology of western Japan (I. On the Paleogene stratigraphy and molluscan fauna in the vicinity of Nishisonogi Peninsula Cited by: 1.

Etherington, T. / STRATIGRAPHY AND FAUNA OF THE ASTORIA MIOCENE OF SOUTHWEST WASHINGTON, University of California Publications, Vol # 5, pages 31 -plates 1Berekely,pb, - 3 - $ GEOLEX. Summary of Citation: Astoria Publication: Etherington, F.J.,Stratigraphy and fauna of the Astoria Miocene of southwest Washington: University of.

MIOCENE MARINE MOLLUSKS FROM THE ASTORIA FORMATION IN OREGON By ELLEN JAMES MOORE ABSTRACT The marine Astoria formation of Miocene age occurs in western Oregon. Fossiliferous exposures are limited almost entirely to the sea cliffs along the Pacific Ocean in Tillamook and Lincoln by: AbstractA new occurrence of fossil butternut is recognized based on a.

Studies, beginning in southwest Washington in the late s and continuing into the s, resulted in the initial correlation of Washington's Tertiary sequence with Cali­ fornia foraminiferal stages and the establishment of provincial zones.

This framework was later extended to the early and middle Tertiary rocks of northwest Washington. Stratigraphy, Age, and Tectonic Setting of the Miocene-Pliocene Lacustrine Sediments of the Western Snake River Plain, Oregon and Idaho Glenns Ferry, Idaho, along the southwest edge of the plain suggests that these lakes occupied approxi- mately the same basin.

The Grassy Mountain and Blackjack basalts, de- File Size: 1MB. ———————, Fauna of the type Tejon: Its relation to the Cowlitz phase of the Tejon group of Washington: California Academy of Sciences Proceedings, ser. 4, v. 5, p.pls. ———————, Stratigraphy and fauna of the Tejon Eocene of California: University of California Publications, Bulletin of the.

Formation (Early Miocene) which is composed of ash-flow tuffs, with interlayers of lavas and fluvial deposits (Vance, ). The Heppsie Andesite (Miocene) sits above the Wasson Formation. The Colestin, Roxy, Wasson, and Heppsie Formations collectively are referred to as the Western Size: 1MB.U.S.

GEOLOGICAL SURVEY THE CENOZOIC GEOLOGY OF THE OREGON AND WASHINGTON COAST RANGE and ROAD LOG for the NORTHWEST PETROLEUM ASSOCIATION 9TH ANNUAL FIELD TRIP CENOZOIC GEOLOGY OF COASTAL NORTHWEST OREGON by Parke D.

Snavely, Jr.1, Ray Wells1, and Diane Minasian1 Open-File Report 93 Author: P.D. Snavely, R.E. Wells, D.L. [email protected]{osti_, title = {Stratigraphic framework, sedimentology and structural setting of Miocene-Pliocene sediments of the Abu Qir area, offshore Nile delta}, author = {Ince, D.M.

and Deibis, S. and McSherry, A. and Seymour, W.P.}, abstractNote = {The offshore Nile delta contains significant gas resources which are currently undergoing both production and appraisal in the .