Twin Creek limestone (Jurassic) in the western interior of the United State
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Twin Creek limestone (Jurassic) in the western interior of the United State

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Published by U.S. Govt. Print. Off. in Washington .
Written in English

Subjects:

Places:

  • West (U.S.)

Subjects:

  • Geology -- West (U.S.),
  • Geology, Stratigraphic -- Jurassic,
  • Paleontology -- West (U.S.)

Book details:

Edition Notes

Bibliography: p. 99-102.

Statementby Ralph W. Imlay.
SeriesGeological Survey professional paper 540
Classifications
LC ClassificationsQE75 .P9 no. 540
The Physical Object
Paginationiv, 105 p.
Number of Pages105
ID Numbers
Open LibraryOL256481M
LC Control Numbergs 66000297
OCLC/WorldCa3354289

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Get this from a library! Twin Creek limestone (Jurassic) in the western interior of the United States,. [Ralph W Imlay] -- A description of the stratigraphic and faunal succession in the Twin Creek Limestone and regional comparisons with contemporary formations. Whitney Canyon-Carter Creek field is a giant sour gas and condensate reservoir located in extreme southwestern Wyoming in the Fossil basin area of the Wyoming thrust belt. Discovered in , the field contains 36 wells within an area 13 mi long and 2 mi wide. Porous dolomites of the Mississippian Mission Canyon formation contain over 70% of. Twin Creek limestone (Jurassic) in the western interior of the United States (DLC)gs (OCoLC) Material Type: Document, Government publication, National government publication, Internet resource: Document Type: Internet Resource, Computer File: All Authors / Contributors: Ralph W Imlay; Geological Survey (U.S.). Dinoflagellate and Organic Facies Stratigraphy of the Twin Creek Limestone (Jurassic) in Western Wyoming and Northeastern Utah, U.S.A. Robert Scott Van Pelt City University of New York, - Dinoflagellates, Fossil - pages.

@article{osti_, title = {Correlation of Twin Creek limestone with Arapien shale in Arapien embayment, Utah - preliminary appraisal}, author = {Sprinkel, D.A. and Waanders, G.L.}, abstractNote = {Striking and important stratigraphic patterns have emerged as a result of recent work during which members of the Twin Creek Limestone were correlated with the Arapien Shale, all of Middle. Twin Creek Limestone, in Wyoming; This disambiguation page lists articles about distinct geographical locations with the same name. If an internal link led you here, you may wish to change the link to point directly to the intended article. The hallmark of Twin Creeks’ exclusive country club lifestyle is the private, championship 7,yard, par 72 Fred Couples Signature Golf Course. The picturesque acres of dramatic rolling terrain is highlighted by low-lying ravines lined with limestone outcroppings and century-old oak and pecan trees. WHEREVER YOU ARE IN LIFE, DISCOVER WHAT LIFE IS ALL ABOUT. Twin Creeks Country Club. Challenge our championship 7,yard par 72 signature golf course by Masters Champion Fred Couples. acres of dramatic rolling terrain are highlighted by low-lying ravines lined with limestone outcroppings and century-old oak and pecan trees.

TWIN CREEK LIMESTONE (JURASSIC) in the Western Interior of the United States. A description of the stratigraphic & faunal succession in the Twin Creek Limestone & regional comparisons with contemporary formations. Geological Survey Professional Paper [Ralph W. Imlay] on *FREE* shipping on qualifying offers. The overlook is located near the base of the Glen Rose hills. The weak shale and sand layers form flats; the intervening Cow Creek limestone forms bold bluffs overlooking the river. We can view these rocks close up on the trail to Trammell's Crossing, in the Twin Falls area, and farther downstream to the east. ADDITION BOOK View Print (1 token View Print (1 token) Limestone Creek Estates Sheet 1. View Print (1 token) Limestone Creek Estates Sheet 2. View Print (1 token) OAKVIEW ADDITION REPLAT BLK 29 BOOK Rancho El Arrollo. View Print (1 token) Re-Plat of Twin Ponds Villas 3rd Addition Lots View Print (1 token. Much of the route is in the Jurassic Twin Creek Limestone, which includes oolitic, sandy, silty, fossiliferous, massive, and/or shaley (some intensely shattered) limestone. The formation also consists of small amounts of red siltstone and shale. The red shale at mile may be a remnant of an ancient soil or erosion surface.