Cenozoic geology of the Reynolds Creek Watershed, Owyhee County, Idaho.

  • 248 Pages
  • 2.33 MB
  • English
Washington State University , [Pullman]
Geology -- Idaho., Geology, Stratigraphic -- Ceno
The Physical Object
Paginationxiv, 248 l.
ID Numbers
Open LibraryOL16602486M

Cenozoic geology of the Reynolds Creek experimental watershed, Owyhee County, Idaho. Moscow, Idaho Bureau of Mines and Geology, (OCoLC) Document Type: Book: All Authors / Contributors: David H McIntyre.

General Information. Title: Cenozoic geology of the Reynolds Creek experimental watershed, Owyhee County, Idaho Author(s): McIntyre, D.H.

Publishing Organization: Idaho Bureau of Mines and Geology Series and Number: Pamphlet P Publication Date: Map Scale:Cross Section: Yes Idaho.

book Latitude: 43° 25' 48" N () South Latitude: 43° 3' 36" N (). Cenozoic geology of the Reynolds Creek experimental watershed, Owyhee County, Idaho, [David H McIntyre] on *FREE* shipping on qualifying offers. Owyhee County is a county in the southwestern corner of the U.S.

state of of the census, the population The county seat is Murphy, and its largest city is Homedale. In area it is the second-largest county in Idaho, behind Idaho County.

Owyhee County is part of the Boise metropolitan is the location of slightly more than 50% of the Duck Valley Indian State: Idaho.

Cenozoic Geology of Idaho 0 10 20 Ml., I 0 10 20 30 Km Figure 1. Generalized geologic map of western Owyhee County, Idaho (modified from Ekren and others, ).File Size: 3MB.

Historical Weather. Below are weather averages from to according to data gathered from the nearest official weather station. The nearest weather station for both precipitation and temperature measurements is K which is approximately 13 miles away and has an elevation of 2, feet ( feet higher than Reynolds Creek).

Because the nearest station and this geographic feature may have Hardtrigger Creek: mi. Boise Office. Idaho Water Center Suite E. Front Street Boise, ID Cenozoic Geology of Idaho provides abundant information, including much that was previously unpublished, about the last 65 m.y.

of the earth's history in this interesting state. vegetation, (b) consolidated soils, and (c) consolidated geology. Mapping units listed in the legends are described in detail by Seyfried et al. Table 1.

Corner Coordinates for Reynolds Creek Experimental Watershed DEM Layer Map Corner Longitude Latitude Easting, m Northing, m NE 40 W43 19 N4, The geology and ore deposits of the South Mountain Mining District, Owyhee County, Idaho (Pamphlet / State of Idaho, Bureau of Mines and Geology) [Robert E.

Three Creek. Three Creek is a ranching area in southeastern Owyhee County, about Owyhee County miles south of the Snake River. The first ranch was established in the s by Joe Scott of Miles City, Montana, who named the area “71,” which was also the brand Scott used to identify his cattle.

the Reynolds Creek Experimental Watershed, located in the state of Idaho, United States, were analyzed to evaluate the extent and magnitude of the impact of climate warming on the hydrology and related resources in the interior northwestern United States. This analysis shows significant trends of increasing temperature at all elevations, with.

Basalt (Pliocene and Miocene). (Pliocene and Miocene) at surface, covers 34 % of this area Flows and cinder cones of olivine tholeiite basalt, and shallow basalt intrusives (~ Ma); includes basalt in Owyhee County and southwest of Twin Falls, basalt of Weiser (basalt to andesite), basalt of Cuddy Mountain (alkali basalt and picro-basalt) north of Cambridge, basalt in Mount Bennett Hills.

Requesting an item will add it to your shipping order. Payment will need to be completed by calling the IGS office ().

tentatively placed the Sucker Creek Fonnation age between and m.y. The fonnation is cwerlain by the Jump Creek Rhyolite dated by Annstrong and others (, p. 5) at ± m.y. Ekren and others (, p. ) show that part of the Sucker Creek Fonnation in Owyhee County in Idaho cwerlies an upper rhyolite, rhyolite por­File Size: 3MB.

Publication type: Report: Publication Subtype: USGS Numbered Series: Title: Geologic map of the Spring Creek Basin Quadrangle, Owyhee County, Idaho: Series title. Cherry Creek-Owyhee Resor t can be seen at right of photogroph.

State pork areo in center of photograph is situated on the Sucker Creek Formation. Woter level of lake is approximately 50 feet below normal. Usual level is indicated by vegetation line. Figure 3. Owyhee Dam, constructed in for irrigatian purposes. The dam is situated. Wikimedia Commons has media related to Bodies of water in Owyhee County, Idaho.

of Owyhee County, Idaho‎ (1 P) R Rivers of Owyhee County, Idaho‎ (2 C, 17 P) Pages in category "Bodies of water of Owyhee County, Idaho" This category contains only the following page. This list may not reflect recent changes.

Salmon Falls Creek. SNOTEL Site: Reynolds Creek State: Idaho Site Number: County: Owyhee Latitude: 43 deg; 17 min N Longitude: deg; 51 min W Elevation: feet Reporting since:. An archaeological survey of Pole Creek, Owyhee County, Idaho by Mark G.

Plew; 1 edition; First published in ; Subjects: Antiquities, Excavations (Archaeology); Places:.

Description Cenozoic geology of the Reynolds Creek Watershed, Owyhee County, Idaho. PDF

Tectonic and Magmatic Evolution of the Snake River Plain Volcanic Province: Idaho Geological Survey Bulle p.␣ ABSTRACT The western Snake River Plain is a Neogene-aged intracontinental rift basin, about 70 km wide and km long, trending northwest across the southern Idaho batholith.

Its southeastern end merges with the northeast. Wilderness Study Areas, Owyhee County, Idaho. D2 2. Map showing mineral resource potential and geology of the Owyhee River Canyon and the Deep Creek-Owyhee River Wilderness Study Areas, Owyhee County, Idaho.

6 3. Major elements of mineral resource potential/certainty classification. 11Author: Michael G. Sawlan, H.D. King, J.D. Hoffman, D.M. Kulik, P.N. Gabby, D.O. Capstick, A.R. Buehler. Geologic Map of the Grand View-Bruneau Area, Owyhee County, Idaho. Idaho Geologic Survey Technical Report Malde, H.E.

Stratigraphy of the Glenns Ferry Formation from Hammett to Hagerman, Idaho. USGS Bulletin: D. Mustoe, George. Western Washington University, Personal Communication, August National Park Service (). Reptiles and amphibians in deep canyons: the Big Jacks and Little Jacks Creek drainages of Owyhee County, Idaho / Title Variants: Alternative: Big Jacks and Little Jacks Creek drainages of Owyhee County, Idaho Related Titles.

Series: Technical bulletin (United States. Bureau of Land Management. Idaho State Office) ; By. Cenozoic Stratigraphy and Tectonic Evolution of the Raft River Basin, Idaho Paul L.

Williams’, Harry R. Covingtonz, and Kenneth L. Pierce* ABSTRACT The Raft River basin, a north-trending structure in the Basin and Range province south of the Snake River Plain, Idaho, is filled with upper Cenozoic.

OWYHEE RIVER REGION, IDAHO AND NEVADA Mineral Resources of the Owyhee Canyon and South Fork Owyhee River Wilderness Study Areas, Elko County, Nevada, and Owyhee County, Idaho By Eugene E. Foord, Michael J. Luessen, Dirk S. Hovorka, Joseph L. Plesha, V.J.S. Grauch, Marian Barton, anc/Harley D.

Download Cenozoic geology of the Reynolds Creek Watershed, Owyhee County, Idaho. PDF

King U.S. Geological SurveyCited by: 2. Reynolds Creek flows from south to north, heading in the Owyhee mountains at elevations exceeding m. The lower boundary of the experimental watershed is determined by the outlet weir location, which is near the head of a small canyon through which Reynolds Creek flows before entering the Snake River about 12 km to the north.

The western Snake River Plain (SRP) is a southeast-northwest–trending complex graben bounded on the SW by the Owyhee Front.

Details Cenozoic geology of the Reynolds Creek Watershed, Owyhee County, Idaho. FB2

This graben, which merges with the central SRP at its southeast end near Bruneau Canyon, is a subsidiary tectonic feature that resulted from southwest-northeast extension as the main SRP–Yellowstone hotspot trend evolved.

(5) Estimation of water yield from the upper Big Wood River basin, Trail Creek, Warm Springs Creek, and East Fork Big Wood River. Data were collected from February through November Ph¥sical Setting The upper Big Wood River basin is in Blaine County, north of File Size: 3MB.

Geology and mineral resources of a portion of the Silver City region, Owyhee County, Idaho. Responsibility [by] R.R. Asher. Imprint Moscow, Physical description p.

illus. (part fold.) maps (part fold.) 29 cm. Series Pamphlet (Idaho Bureau of Mines and Geology) ; no. Online. Available online At the library. SAL3 (off-campus storage). Ma The North Fork of the Owyhee River from the Idaho-Oregon State border upstream to the upstream boundary of the North Fork Owyhee River Wilderness.

Classification/Mileage: Wild — miles; Recreational — miles; Total — miles.Full text of "Reynolds Creek cooperative watershed study" Cenozoic geology of the Reynolds Creek Experimental Watershed, Owyhee County, Idaho.

Idaho Bureau of Mines and Geol. PamphletMoscow, Idaho, pp. Morris, R. P., and C. L. Hanson. Weighing and recording precipitation gage modification.The Fish Creek Reservoir quadrangle in south-central Idaho lies on the north-central margin of the Cenozoic Snake River Plain at the southern end of the Pioneer Mountains.

Rocks exposed in the quadrangle range in age from Paleozoic through Cenozoic. Mesozoic rocks are absent. Though Triassic and Jurassic sedimentary rocks may have been deposited in this area, they have been removed by .