... was done in the Jefferson Valley of southwestern Montana (approximately 90 km southeast of the Deer Lodge Valley), an area where no well log data yet exist for Cenozoic basin fill. However, well log and seismic reflection data are available from Cenozoic basin fill of the Deer Lodge Valley, southwestern...

... of species occurrences in the Cypress Hills area and the Red Deer Valley. BE, Belanger Menber; DMT, Drumheller Marine Toungue; DP, Dinosaur Park Formation; FR, Frenchman Formation; KT, Kneehills Tuff; LC, Lethbridge Coal Zone (coal thickness has been exaggerated); ML, Medicine Lodge Member; OX, Oxarart...

...). 1872, December 10, 4:30 p . m . - - E p i c e n t e r probably between Deer Lodge and Helena. VI at Deer Lodge where the Independent (issue of December 14, 1872) reported the "valley was given a healthy earthshaking, which lasted The exact dates on which the sounds were heard is uncertain. Pardee (1926...

... released from K-feldspar during step heating : Earth and Planetary Science Letters , v. 123 , p. 95 – 104 , doi: 10.1016/0012-821X(94)90260-7 . Heise B.A. , 1983 , Structural geology of the Mt. Haggin area, Deer Lodge country, Montana [M.S. thesis] : Missoula, Montana , University...

... Ranch local fauna (C0173, Deer Lodge basin) is included ( Fig. 1 ). To facilitate the comparison with this upper Cabbage Patch assemblage, located about 26 km from the Bert Creek area of the Flint Creek basin, a lower Cabbage Patch assemblage from the Tavenner Ranch Local Fauna is also included (MV6613...

... the big shake last fall. Deer Lodge, Montana 1872/12/15 ~10:00, Sunday. Fort Lapwai, Idaho Two sharp shocks separated by a very slight interval. 1872/12/14 20:00, Saturday (Foreshock? Mainshock reported at 22:00 here.) 1872/12/15 04:30, Sunday. Fort Simcoe, Washington Almost every hour...

...-50862. By courtesy of the National Archives of Canada, I have a copy of Weston’s field notes for 1889. His account of the Red Deer River trip is most graphic. In the area between the future sites of the Tolman and Morrin bridges, he observed and tried to collect numerous bones of “Dinosaurians...

... as an important component of handaxe and other assemblages such as High Lodge, Hoxne and Bowman s Lodge (Ashton 1992; Ashton & McNabb 1992; McNabb 1992). Artefacts from the dark brown silty clay In Area I a biface made on a thin piece of tabular flint was found within the dark brown silty clay, 25cm above...

... into underlying Cenozoic and Mesozoic units and overlaps the Flint Creek fault in the eastern Flint Creek basin ( Fig. 8F ). Vertebrate fossils collected from Fm facies have Clarendonian ages (NALMA), and uppermost Gf facies have been correlated with Hemphillian (NALMA) gravels in the nearby Deer Lodge...

... by Morgan 5 who gives it an average thickness of 260 feet; 230 feet of sandstone-chert conglomerates and 30 feet of dark shale at the base. In this central area there are only three definite stratigraphic markers which can be traced into areas outside of Oklahoma. These are the Deer Creek limestone...

..., on the diorites of Glen Tilt - pushing his bike from Rusholme to the field area and lodging with a gamekeeper's family. His first stroke of luck came on applying for a Strathcona scholarship to Cambridge. The admissions tutor at St. John's College, James Wordie (the geologist on Shackleton's 1914 expedition...

... Esteven and Whitemud formations of the Cypress Hills area represent the middle Edmonton and upper part of the basal Edmonton section as developed on Red Deer River. It is most probable that the beds above the typical Fox Hills, the thickness of which was previously stated, represent the lower part...

..., PhiUipaburg4. , Big Hole. 5, Grasshopper.6, HomePrairie. 7, Medidne Lmlge. 8, Muddy Creek. 9, Nicholia. 10, Flint Creek-Avon-NevadaCreek. 11, Deer Lodge. 12, Divide. 13, Mdrome. 14, Reaverhead.15, Bhcktail Deer Creek. 16, SageCreek. 17, Red Rack River. 18, Upper Ruby River. 19, Centennial. 20, Jefferson.21...

... County, Montana, the northwest-southeast axis of thinning on Baker-Glendive, the area of zero Devonian in the Glendive field, Montana, the northeast-southwest axis of thinning in the Richey area, and the north-south axis of thinning in the Tioga-Beaver Lodge-Croff area. Devonian production is established...

... Powell and Clark Counties, southeastern Granite County, and in northern Deer Lodge and Jefferson Counties is in a tectonically complex area marginal to the plutonic province of the Boulder batholith and related stocks. Emmons and Calkins (1913 , p. 68) suggested that thinning was caused by nondeposition...

... Cretaceous dinosaur-bearing Edmonton series in the Red Deer Valley area of Alberta. Allan and Sanderson (1945) formalized the nomen- clature to Paskapoo and Edmonton Formations and moved the contact upward from the top of the "Big Seam" (Ardley or No. 14 coal seam) to the base of the first brown-weathering...

... western half of edifice (see Fig. 20 ). Several vents peripheral to edifice are indicated by stars and identified by unit label ( Table 1 ). Abbreviations: HL—Horseshoe Lake; LG—Lake George; LP—Lincoln Peak; ML—downtown Mammoth Lakes; MMSA—Mammoth Mountain Ski Area (Main Lodge); RL—Reds Lake; SL—Shadow...

... the Snake River Plain from the eastern Missouri River Basin ( Fig. 2 ). Our proposed route for the paleo-Snake River again crosses the modern continental divide back into the Columbia Basin over the lower (1800 m asl) Deer Lodge Pass. While the modern topography profile suggests ~250–300 m of relief between...