1-20 OF 134 RESULTS FOR

Spokane River basin

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 May 2002
Geochemistry: Exploration, Environment, Analysis (2002) 2 (2): 131–142.
...Cecile A. Grosbois; Arthur J. Horowitz; James J. Smith; Kent A. Elrick Abstract Surface sediments in the Spokane River Basin are enriched in Pb, Zn, As, Cd, Sb, and Hg relative to local background levels. Maximum enrichment occurs in the Upper Spokane River in close proximity to Lake Coeur d'Alene...
FIGURES | View All (6)
Image
General location of the <b>Spokane</b> <b>River</b> <b>Basin</b> and sample locations. The map i...
Published: 01 May 2002
Fig. 1 General location of the Spokane River Basin and sample locations. The map insert details the Coeur d'Alene River Basin; the area outlined by dashed lines demarcates the 54 km 2 Bunker Hill Superfund Site.
Series: GSA Special Papers
Published: 01 September 2016
DOI: 10.1130/2016.2522(08)
... The Blackbird cobalt-copper (Co-Cu) district in the Salmon River Mountains of east-central Idaho occupies the central part of the Idaho cobalt belt—a northwest-elongate, 55-km-long belt of Co-Cu occurrences, hosted in grayish siliciclastic metasedimentary strata of the Lemhi subbasin...
Journal Article
Journal: GSA Bulletin
Published: 31 August 1933
GSA Bulletin (1933) 44 (4): 675–722.
... the Spokane Flood. Critical examination of the area by the writer has revealed new facts regarding the extent of the flood between . . . 2 J Harlen Bretz: Channeled scablands of the Columbia Plateau. Jour. Geol., vol. 31, 1923, pp. 617–649; J Harlen Bretz: Dalles type of river channel. Jour. Geol...
Series: Society for Sedimentary Geology
Publisher: Society for Sedimentary Geology
Published: 01 January 2017
DOI: 10.2110/sepmsp.107.12
EISBN: 9781565763456
... ABSTRACT: Understanding of very thick Late Devonian shelf strata in Idaho is hindered by formation terminologies. Interpreted genetically, and in combination with lower accommodation settings in Montana, strata reveal craton-to-basin geometries and analogues similar to other western Laurentian...
FIGURES | View All (12)
Series: Geological Society, London, Special Publications
Published: 01 January 2008
DOI: 10.1144/SP301.3
EISBN: 9781862395497
... and Columbia valleys beyond the scablands, for these valleys received all the discharge of the great glacial rivers …. If there is no evidence for a greatly flooded condition of these valleys then the hypothesis is wrong …. Bretz (1925 b ) traced the Spokane Flood evidence downstream to the Snake...
FIGURES | View All (6)
Series: GSA Field Guide
Published: 01 January 2016
DOI: 10.1130/2016.0041(05)
EISBN: 9780813756417
... Abstract The Moscow-Pullman basin, located on the eastern margin of the Columbia River flood basalt province, consists of a subsurface mosaic of interlayered Miocene sediments and lava flows of the Imnaha, Grande Ronde, Wanapum, and Saddle Mountains Basalts of the Columbia River Basalt Group...
FIGURES | View All (15)
Journal Article
Journal: Economic Geology
Published: 01 September 2012
Economic Geology (2012) 107 (6): 1081–1088.
... of subsidence rates ( Lydon, 2000 ) and detrital sources. The lower basin fill (lower Belt, Ravalli Group, Piegan Group) accumulated under rapid subsidence rates and was derived via major river systems from a non-North American source to the southwest. Much slower subsidence rates characterize the upper basin...
FIGURES
Journal Article
Journal: Geosphere
Published: 01 April 2007
Geosphere (2007) 3 (2): 91–107.
..., White River may have potential for concealed precious and/or base metal deposits at shallow depth. Both areas are products of the ancestral Cascade arc. Goldfield lies within the Great Basin physiographic province in an area of middle Miocene and younger Basin and Range and Walker Lane faulting, whereas...
FIGURES | View All (7)
Journal Article
Published: 01 June 2015
Italian Journal of Geosciences (2015) 134 (2): 323–336.
... related to mining are still recorded by the ecosystem, namely on waterways of the Paglia and Tiber River basins. In particular, the close spatial connection between the town of Abbadia San Salvatore, the Hg mine within its immediate neighborhood, and the drainage catchment of the Paglia River has...
FIGURES | View All (7)
Journal Article
Journal: Economic Geology
Published: 01 November 2004
Economic Geology (2004) 99 (7): 1355–1384.
... that most of the Kuna formed in slope and basin settings characterized by anoxic or dysoxic bottom water and by local high productivity. Shallow-water facies of the Lisburne Group in the Red Dog area are present locally in the Endicott Mountains allochthon and throughout the Kelly River allochthon...
FIGURES | View All (7)
Journal Article
Journal: Palynology
Published: 22 December 2017
Palynology (2017) 41 (0): 189–220.
... of the Sappington Formation showing the contact with sandstone Unit 5. None The late Famennian/early Tournaisian interval (DCB) at Logan Gulch on the northern bank of the Gallatin River ( Figures 1 – 3 ) is represented by the Three Forks (upper Trident Member), Sappington and Lodgepole formations (Sandberg...
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1966
AAPG Bulletin (1966) 50 (12): 2614–2621.
... movement near Kemmerer, Wyoming, may not apply to the time of movement on the Absaroka 150 miles away along the edge of the Snake River Plain. These considerations bear on the discussions to follow, and great care in analysis is necessary if we hope to gain an understanding of a complex assemblage...
Journal Article
Journal: Economic Geology
Published: 01 March 2004
Economic Geology (2004) 99 (2): 295–312.
... these changes have significant implications for mine, district and regional structural geology and mapping, basin architecture, district-scale fluid flow, alteration halos, district-scale metal zonation, and regional metallogeny. Fluid inclusion analyses indicate that ore formed at approximately 250° to 350...
FIGURES | View All (14)
Series: Society for Sedimentary Geology
Publisher: Society for Sedimentary Geology
Published: 01 January 2017
DOI: 10.2110/sepmsp.107.13
EISBN: 9781565763456
... of the Missouri River, and is one of the earliest areas in the western United States to be geologically examined. Lewis and Clark traveled through this area in the summer of 1805, and the first geologic observations of the area were documented by Hayden (1869) . The earliest geologists ( Peale 1893 , 1896...
FIGURES | View All (18)
Journal Article
Published: 05 February 2016
Canadian Journal of Earth Sciences (2016) 53 (6): 548–564.
... ). The site was mentioned by Berry (1929) in his monograph on the Miocene Latah Formation, from outcrops to the east and south of Republic extending to Spokane and on into Idaho near Clarkia. Berry interpreted Republic as part of the Latah Formation. Roland W. Brown described additional specimens from...
FIGURES | View All (6)
Series: Field Guide
Published: 01 January 2003
DOI: 10.1130/0-8137-0004-3.1
EISBN: 9780813756042
... this view the main path of the flood outbursts from the Pend Oreille Lake basin can be followed across the trench, south toward Coeur d’Alene, and west to Spokane. Another floodpath was to the north down the Hoodoo Valley to the Pend Oreille River and Little Spokane River via Newport, Washington. The water...
FIGURES | View All (9)
Journal Article
Journal: GSA Bulletin
Published: 01 May 2010
GSA Bulletin (2010) 122 (5-6): 678–689.
... in water a few hundred meters deep. Blocked from flowing north by mountains and the ice sheet, this water rapidly deepens in Spokane valley to overflow the low drainage divide to the south, flooding the Cheney-Palouse scabland. The Cheney-Palouse overland flow into Snake River floods Pasco Basin for a full...
FIGURES | View All (11)
Journal Article
Journal: Economic Geology
Published: 01 November 2004
Economic Geology (2004) 99 (7): 1415–1434.
... allochthonous sheets, three of which have been subject to regional and detailed structural analysis. The lowermost of these is the Endicott Mountains allochthon, which is overlain by the structurally higher Picnic Creek and Kelly River allochthons. Each individual allochthon is itself internally imbricated...
FIGURES | View All (14)
Journal Article
Journal: GSA Bulletin
Published: 01 May 2000
GSA Bulletin (2000) 112 (5): 668–682.
... ( Figs. 7B and 8 ; ∼350 m, down to the west), offset units deposited during stage 3 and formed north-trending embayments into the Bully Creek basin (Fig. 8) which cuts across the Oregon-Idaho graben near its northern margin. Late middle Miocene to Pliocene subsidence along the western Snake River...
FIGURES | View All (8)