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Stillwater River

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Geologic relationships of the J-M Reef at the West Fork area, West Fork of the Stillwater River. A. Generalized stratigraphic section and surface geologic map of the West Fork adit area showing the major olivine-bearing members and the location of the dated sample (ST11-16; map and section modified from Mann et al., 1985). At the West Fork area, the lowermost four olivine-bearing members (O1-O4) are missing and O5B lies directly on gabbronorite belonging to GN2; the J-M Reef is contained within O5B. Contour lines are in feet and each interval represents a change in elevation of 20 ft. B. Photograph of the J-M Reef exposed in the cliffs along the west side of the West Fork of the Stillwater River. The major units are separated by dashed lines (from Mann et al., 1985). The dated sample was collected from the O5B member ~180 m along strike to the northwest (right), just above the West Fork adit. Field of view of photograph is approximately 60 m.
Published: 01 May 2016
Fig. 2 Geologic relationships of the J-M Reef at the West Fork area, West Fork of the Stillwater River. A. Generalized stratigraphic section and surface geologic map of the West Fork adit area showing the major olivine-bearing members and the location of the dated sample (ST11-16; map and section
Series: Short Courses
Published: 01 January 2005
DOI: 10.3749/9780921294764.ch18
EISBN: 978-0-921294-76-4
... Fork of the Stillwater River. This paper summarizes the original results of the soil and talus fines geochemical surveys and provides new interpretations of these data. Surficial Geology of the Study Area The Beartooth Mountains are a rugged mountain range that extends for about 120 km...
FIGURES | View All (11)
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1999
AAPG Bulletin (1999) 83 (5): 812–813.
... was! Under his guidance many fields were discovered. Among those having a large impact on Apache's success was the Stillwater field in and around Stillwater, Oklahoma. This discovery and subsequent development "made" Apache and put it among the top domestic exploration companies of the time. In the late...
Book Chapter

Series: Society of Economic Geologists Guidebook Series
Published: 01 January 1993
DOI: 10.5382/GB.18.01
EISBN: 9781934969717
... Abstract Interstate 80 between Elko and Carlin, Nevada, follows the valley of the Humboldt River. The Humboldt drains a 17,000 square mile basin along its 275 mile course, located entirely within the State of Nevada. While barely a trickle of water in late summer, spring floods may swell...
Series: Society of Economic Geologists Guidebook Series
Published: 01 January 1993
DOI: 10.5382/GB.18
EISBN: 9781934969717
Journal Article
Journal: Geosphere
Published: 26 September 2018
Geosphere (2018) 14 (6): 2505–2532.
...N.E. Moore; A.L. Grunder; W.A. Bohrson Abstract The Steens Basalt, southeast Oregon, USA, initiated at 17 Ma as the earliest pulse of the Columbia River Flood Basalt of the northwestern USA. New and existing stratigraphically controlled data reveal temporal changes in lava flow character, and whole...
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Journal Article
Journal: Economic Geology
Published: 01 May 2016
Economic Geology (2016) 111 (3): 771–782.
...Fig. 2 Geologic relationships of the J-M Reef at the West Fork area, West Fork of the Stillwater River. A. Generalized stratigraphic section and surface geologic map of the West Fork adit area showing the major olivine-bearing members and the location of the dated sample (ST11-16; map and section...
FIGURES | View All (6)
Journal Article
Published: 01 January 2001
Exploration and Mining Geology (2001) 10 (1-2): 35–49.
... ± pyrrhotite + millerite ± pentlandite, typically surrounded by epidote. The majority of the Cu-Ni-PGE mineralization displays low ratios of Pt/Pd (~0.20) and high ratios of Cu/Ni (~2.9), which are similar to those of the Lac des Iles and the River Valley mafic-ultramafic complexes. The lithologies in Legris...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1957
AAPG Bulletin (1957) 41 (2): 353–354.
... are recognized: (1) interbedded and intertonguing non-marine, brackish-water, and shallow-water marine strata that contain a tropical to warm-temperate flora and marine invertebrate fauna of late Eocene age and include the Stillwater, Kushtaka, and Tokun formations in the Katalla district and an unnamed...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1941
GSA Bulletin (1941) 52 (1): 49–60.
... of the Jordan-Oneota contact rises from 200 feet above sea level in the region of Austin to over 1150 feet on the crest of a local high to the southwest of Winona. Faults occur along the valley of the St. Croix River north of Stillwater and along the Mississippi valley at Hastings and Red Wing. University...
Journal Article
Journal: GSA Bulletin
Published: 01 July 1938
GSA Bulletin (1938) 49 (7): 1045–1066.
... advances, called “stages” in this paper, were named, in stratigraphic order, Monarch, Arapaho, River, and Stillwater. The ages tentatively assigned them are, respectively: Late Wisconsin, Middle Wisconsin, Early Wisconsin (Iowan), and not younger than Illinoian. Some investigation of preglacial...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1901
GSA Bulletin (1901) 12 (1): 313–342.
... of the Saint Croix river. The northern limit of the district is near latitude 46° 25′, at the boundary line between Minnesota and Wisconsin; the southernmost point exposed is in the lower Dalles of the Saint Croix near Franconia (latitude 45° 15′), although the lava flows of the southern exposures stretch...
Journal Article
Published: 26 March 2025
American Mineralogist (2025)
... 5HHI VXUIDFH WUDFH 4XDWHUQDU\ GHSRVLWV 7HUWLDU\ LQWUXVLYH URFNV 3DOHR]RLF VHGLPHQWDU\ URFNV 0LGGOH %DQGHG 8SSHU %DQGHG /LPHVWRQH Stillwater River 1\H E 6HULHV NP =RQH *DEEURQRULWH 6 2OLYLQH EHDULQJ 9 5 $QRUWKRVLWH WestFork Stillwater River :HVW )RUN DGLW 6WLOOZDWHU PLQH VKDIW 0RXQWDLQ 9LHZ DUHD 3DOHR...
Image
Fig. 1.
Published: 19 September 2015
F ig . 1. Outline of the Beartooth uplift with the major blocks labeled. The darker shade in the Stillwater block is the Stillwater Layered Igneous Complex (2.7 Ga). The LLMC and its temporal equivalents occur throughout the Beartooth Plateau and South Snowy blocks. Also shown are the locations
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 February 2017
Lithosphere (2017) 9 (1): 100–116.
... by the Stillwater Mining Company. Discernible surface outcrops are rare across the 20 km trace of the SPF ( Cox and Holick, 2008 ), and comprehensive observation is restricted to the subsurface. Paleozoic strata displaced by the SPF at high elevations above the Stillwater River Valley ( Jones et al., 1960 ; Page...
FIGURES
Image
Generalized map of the Stillwater Complex (after p 1977) showing the location of the Boulder River area studied by Labotka and Kath (2001) and the Mountain View area of this investigation.
Published: 01 February 2008
F igure 1. Generalized map of the Stillwater Complex (after p 1977) showing the location of the Boulder River area studied by Labotka and Kath (2001) and the Mountain View area of this investigation.
Journal Article
Published: 01 June 2016
Mineralogical Magazine (2016) 80 (4): 585–637.
... River) and exposure of the complex along the northern edge to the Beartooth plateau. Geophysical evidence suggests that the complex extends at depth for a distance of at least 25 km to the northeast ( Kleinkopf, 1985 ), and a Stillwater Mining Company technical report ( Abbott et al., 2011 ) has...
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Image
Outline of Beartooth uplift with the major Archean blocks labeled (modified after Mueller et al. 2014; Henry et al. 2015). The darker shade in the Stillwater block is the Stillwater Layered Igneous Complex (2.7 Ga). The Long Lake Magmatic Complex (LLMC) and its temporal equivalents occur throughout the Beartooth Plateau and South Snowy blocks. The location of the iron-formation samples used in this study are in the Quad Creek (QC) and Hellroaring Plateau (HR) areas. Also labeled are the Slough Creek batholith (SCB), Jardine Metasedimentary Sequence (JMS), and Yellowstone River shear zone (SZ). White areas indicate Phanerozoic cover. The location of the Beartooth uplift is shown in the inset of North America. (Color online.)
Published: 01 January 2018
Figure 1. Outline of Beartooth uplift with the major Archean blocks labeled (modified after Mueller et al. 2014 ; Henry et al. 2015 ). The darker shade in the Stillwater block is the Stillwater Layered Igneous Complex (2.7 Ga). The Long Lake Magmatic Complex (LLMC) and its temporal equivalents
Journal Article
Journal: Economic Geology
Published: 23 October 2020
Economic Geology (2020) 115 (8): 1799–1826.
... part of the complex and the Stillwater mine, located in the Stillwater River valley in the eastern part of the complex ( Fig. 1 ). The complex also hosts deposits of stratiform chromitite (named A to K from lowermost to uppermost chromitite layer), some with associated PGE mineralization (the A and B...
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Journal Article
Journal: GSA Bulletin
Published: 01 October 2001
GSA Bulletin (2001) 113 (10): 1312–1323.
..., which was emplaced into a sequence of metasedimentary rocks including iron formation, quartzite, graywacke, and argillite. In the region near the Boulder River, where the width of exposed country rock is greatest, the rocks beneath the Stillwater Complex are mostly biotite-bearing...
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