2 edition of Laramie and the overlying Livingston formation in Montana found in the catalog.
Laramie and the overlying Livingston formation in Montana
Walter Harvey Weed
|Statement||by Walter Harvey Weed ; with report on flora by Frank Hall Knowlton.|
|Series||Bulletin of the United States Geological Survey -- no. 105, U.S. Geological Survey bulletin -- no. 105.|
|Contributions||Knowlton, Frank Hall, 1860-1926., Geological Survey (U.S.)|
|The Physical Object|
|Pagination||vi, 68 p. :|
|Number of Pages||68|
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Additional Physical Format: Online version: Weed, Walter Harvey, Laramie and the overlying Livingston formation in Montana (OCoLC) Title. The Laramie and the overlying Livingston formation in Montana / Title Variants: Alternative: House miscellaneous documents, 2d Session, 53d Congress ''94, vol.
26 Alternative: Miscellaneous documents of the House of Representatives for the Second Session of the. Excerpt from The Laramie and the Overlying Livingston Formation in Montana In the foothill country, lying at the base of the mountains south of the Yellowstone river, near Livingston, Montana, a series of water-laid strata, composed mainly of volcanic detritus and overlying the coal-bear in g Laramie beds, was Observed by the writer inwhile studying the geology of the region, in Author: Walter Harvey Weed.
Genre/Form: book: Additional Physical Format: Print version: Weed, Walter Harvey, Laramie and the overlying Livingston formation in Montana. The Laramie and the overlying Livingston formation in Montana / Pages; Table of Contents The Laramie and the overlying Livingston formation in Montana / By.
Weed, Walter Harvey, If you are generating a PDF of a journal article or book chapter, please Cited by: 1. The Laramie and the Overlying Livingston Formation in Montana: With Report on Flora by F.H.
Knowlton avg rating — 0 ratings — 6 editions Want to Read saving 5/5(1). The Laramie and the overlying Livingston formation in Montana. by Weed, Walter Harvey, ; Knowlton, Frank Hall, Annotated list of the fossil plants of the Bozeman, Montana, coal field, with table of distribution and description of new species a guide-book and itinerary for the use of tourists and travellers.
41 pp. 4 pi. Price 5 cents. The Laramie and the Overlying Livingston Formation in Montana, by Walter Harvey Weed, with Report on Flora, by Frank Hall Knowlton. 68 pp. 6 pi. Price 10 cents. The Colorado Formation and its Invertebrate Fauna, by. The Hell Creek Formation in Montana overlies the Fox Hills Formation and underlies the Fort Union Formation, and the boundary with the latter occurs near the Cretaceous-Paleogene boundary (K-Pg), which defines the end of the Cretaceous period and has been dated to 66 ± Ma old.
The 90 metres of deposit was created in about 2 million years. Fauna characteristic of the Hell Creek (Lancian Type: Geological formation. Review of Palaeobotany and Palynology, 57 () Elsevier Science Publishers B.V., Amsterdam -- Printed in The Netherlands POST-BARREMIAN (EARLY CRETACEOUS) TO PALEOCENE PALEOBOTANICAL COLLECTIONS IN THE WESTERN INTERIOR OF NORTH AMERICA JAMES U.
McCLAMMER, JR,1 and DAVID R. CRABTREE2 Chapel Street, New Cited by: 8. The Tongue River is a tributary of the Yellowstone River, approximately mi ( km) long, in the U.S.
states of Wyoming and Tongue rises in Wyoming in the Big Horn Mountains, flows through northern Wyoming and southeastern Montana and empties into the Yellowstone River at Miles City, of the course of the river is through the beautiful and varied landscapes of ⁃ coordinates: 44°49′06″N °27′20″W.
The border zone peraluminous granitoids (K2O/Na2O = ; Ba ppm; mg-numberweakly fractionated REE patterns with enrichment at the LREE end; delta(18)O = parts per. Our field trip destination has roots in early efforts at MSU to take advantage of the natural laboratory represented by the Gallatin National Forest in general, and sites near Langohr Campground in Hyalite Canyon in particular (Figs.
1 and 2).The Gallatin National Forest is a ~2 million-acre forest established in that stretches from just south of Bozeman to the northwestern corner of.
The Hell Creek Formation is an intensively-studied division of mostly Upper Cretaceous and some lower Paleocene rocks in North America, named for exposures studied along Hell Creek, near Jordan, formation includes portions of Montana, North Dakota, South Dakota, and Montana, the Hell Creek Formation overlies the Fox Hills : Montana North Dakota South Dakota Wyoming.
Erosion occurred between ∼ and cal yr B.P. on the upwind region of the dune field, followed by relative stability and soil formation between ∼ and cal yr B.P.
Newly recognized paleovalley deposits in the uppermost Cretaceous and Paleocene Ferris and Hanna formations (Wroblewski, ) in the Hanna and Carbon basins of south-central Wyoming present a unique opportunity to examine processes of valley incision and filling within tectonically active areas near presence of tidal facies (e.g., bundled, double mud-draped foresets, topsets.
The Laramie and the overlying Livingston formation in Montana / (Washington: Govt. Print. Off., ), by Walter Harvey Weed, Frank Hall Knowlton, and Geological Survey (U.S.) (page images at HathiTrust). Sandstone Depositional Environments Edited by.
Peter A. Scholle and Darwin Spearing. Published by. The American Association of Petroleum Geologists Tulsa, OklahomaU.S.A. Roberts, A.E.,Stratigraphy of Madison Group near Livingston, Montana, and discussion of karst and solution-breccia features: U.S.
Geological Survey Professional Paper B, 23 p. Google ScholarCited by: Upper Cretaceous and lower Tertiary strata in the Big Bend region of Texas comprise a gradational sequence of marine, paralic, and terrestrial sediments ().Marine shelf deposits of the Pen Formation interfinger with paralic deposits of the Aguja Formation and grade upward to inland fluvial flood-plain deposits of the Javelina and Black Peaks Formations (Maxwell et al.,Lehman, ).Cited by:.
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