Geologic Map of IDAHO
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Planetary Geologic Mappers Annual Meeting
Program Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Planetary Geologic Mappers Annual Meeting June 12–14, 2018 • Knoxville, Tennessee Institutional Support Lunar and Planetary Institute Universities Space Research Association Convener Devon Burr Earth and Planetary Sciences Department, University of Tennessee Knoxville Science Organizing Committee David Williams, Chair Arizona State University Devon Burr Earth and Planetary Sciences Department, University of Tennessee Knoxville Robert Jacobsen Earth and Planetary Sciences Department, University of Tennessee Knoxville Bradley Thomson Earth and Planetary Sciences Department, University of Tennessee Knoxville Abstracts for this meeting are available via the meeting website at https://www.hou.usra.edu/meetings/pgm2018/ Abstracts can be cited as Author A. B. and Author C. D. (2018) Title of abstract. In Planetary Geologic Mappers Annual Meeting, Abstract #XXXX. LPI Contribution No. 2066, Lunar and Planetary Institute, Houston. Guide to Sessions Tuesday, June 12, 2018 9:00 a.m. Strong Hall Meeting Room Introduction and Mercury and Venus Maps 1:00 p.m. Strong Hall Meeting Room Mars Maps 5:30 p.m. Strong Hall Poster Area Poster Session: 2018 Planetary Geologic Mappers Meeting Wednesday, June 13, 2018 8:30 a.m. Strong Hall Meeting Room GIS and Planetary Mapping Techniques and Lunar Maps 1:15 p.m. Strong Hall Meeting Room Asteroid, Dwarf Planet, and Outer Planet Satellite Maps Thursday, June 14, 2018 8:30 a.m. Strong Hall Optional Field Trip to Appalachian Mountains Program Tuesday, June 12, 2018 INTRODUCTION AND MERCURY AND VENUS MAPS 9:00 a.m. Strong Hall Meeting Room Chairs: David Williams Devon Burr 9:00 a.m. -
12. Owyhee Uplands Section
12. Owyhee Uplands Section Section Description The Owyhee Uplands Section is part of the Columbia Plateau Ecoregion. The Idaho portion, the subject of this review, comprises southwestern Idaho from the lower Payette River valley in the northwest and the Camas Prairie in the northeast, south through the Hagerman Valley and Salmon Falls Creek Drainage (Fig. 12.1, Fig. 12.2). The Owyhee Uplands spans a 1,200 to 2,561 m (4,000 to 8,402 ft) elevation range. This arid region generally receives 18 to 25 cm (7 to 10 in) of annual precipitation at lower elevations. At higher elevations, precipitation falls predominantly during the winter and often as snow. The Owyhee Uplands has the largest human population of any region in Idaho, concentrated in a portion of the section north of the Snake River—the lower Boise and lower Payette River valleys, generally referred to as the Treasure Valley. This area is characterized by urban and suburban development as well as extensive areas devoted to agricultural production of crops for both human and livestock use. Among the conservation issues in the Owyhee Uplands include the ongoing conversion of agricultural lands to urban and suburban development, which limits wildlife habitat values. In addition, the conversion of grazing land used for ranching to development likewise threatens wildlife habitat. Accordingly, the maintenance of opportunity for economically viable Lower Deep Creek, Owyhee Uplands, Idaho © 2011 Will Whelan ranching operations is an important consideration in protecting open space. The aridity of this region requires water management programs, including water storage, delivery, and regulation for agriculture, commercial, and residential uses. -
See Grantees
Organization Name Program Area County Amount Funded East region Aid for Friends Housing and Assistance Bannock $20,000.00 Aid for Friends Housing and Assistance Bannock $14,285.00 Bear Lake Healthcare Foundation Health Bear Lake $17,500.00 Bingham County Senior Center Food and Basic Needs Bingham $15,000.00 Bingham Crisis Center Domestic Violence Bingham $5,000.00 Bingham Crisis Center Domestic Violence Bingham $5,415.00 Center for Hope Health Bonneville $1,000.00 Challis Senior Citizens Inc Food and Basic Needs Custer $1,150.00 Club, Inc. Housing and Assistance Bonneville $14,285.00 Community Resource Center of Teton Valley Housing and Assistance Teton $10,000.00 Eastern Idaho Community College Food and Basic Needs Bonneville $5,000.00 Eastern Idaho Community Partnership Housing and Assistance Bonneville $15,000.00 Family Services Alliance of SE Idaho Inc Domestic Violence Bannock $14,000.00 Family Services Alliance of SE Idaho Inc Domestic Violence Bannock $5,415.00 Gate City Christian Church Food and Basic Needs Bannock $2,000.00 Giving Cupboard Food and Basic Needs Jefferson $5,000.00 Idaho State University Food and Basic Needs Bannock $20,000.00 JRM Foundation (Fort Hall COVID‐19 Relief Fund) Food and Basic Needs Bannock $5,000.00 Lemhi County Crisis Intervention, Mahoney House Domestic Violence Lemhi $7,800.00 Lemhi County Crisis Intervention, Mahoney House Domestic Violence Lemhi $5,415.00 NAMI Idaho Health Bannock $16,000.00 Oneida Crisis Center Food and Basic Needs Oneida $1,500.00 Pocatello Free Clinic Health Bannock $8,300.00 Regional Council for Christian Ministry Food and Basic Needs Bonneville $7,345.00 Rigby Senior Center Food and Basic Needs Jefferson $5,000.00 Senior Activity Center Food and Basic Needs Bingham $2,530.00 Senior Citizens' Community Center, Inc. -
Geologic Maps of Washington
GEOLOGIC MAPS OF WASHINGTON DGER GM-53 124° 117° 123° 122° 121° 120° CANADA 119° 118° 49° 49° WASHINGTON STATE PEND DGER OFR 2000-5 WHATCOM DGER OFR 90-5 USA FERRY (scale 1:500,000) OREILLE Roche Mount Bellingham Robinson Oroville Republic Colville Harbor Baker Mtn 125° OKANOGAN DGER OFR 2003-17 48°30 USGS Map I-2660 DGER OFR 90-10 DGER OFR 90-13 48°30 CANADA DGER OFR 90-11 SAN USA Port JUAN SKAGIT DGER DGER OFR 90-12 ISLAND OFR 90-9 Cape Angeles Port Sauk Nespelem Chewelah Flattery Townsend River Twisp Omak USGS Map I-1198F DGER OFR 2003-5 DGER OFR 2003-6 DGER DGER OFR 90-14 48° USGS Map I-1198G USGS Map I -2592 OFR 95-3 DGER OFR 90-16 48° CLALLAM USGS OFR 93-233 STEVENS IDAHO SNOHOMISH DOUGLAS JEFFERSON USGS OFR 91-147 CHELAN Mount Coulee Forks Seattle Skykomish Banks Spokane Olympus River Chelan Lake Dam DGER OFR 2000-4 DGER OFR 2003-4 DGER OFR 90-17 47°30 KITSAP USGS Map I-1963 USGS Map I-1661 DGER OFR 90-6 DGER OFR 90-15 47°30 GRAYS GIS data only KING LINCOLN SPOKANE Copalis HARBOR GRANT Snoqualmie Moses Beach Shelton Tacoma Wenatchee Ritzville Rosalia MASON Pass Lake DGER OFR 2003-16 KITTITAS DGER OFR 2003-15 47° DGER OFR 87-3 USGS Map I-2538 USGS Map I-1311 DGER OFR 90-1 DGER OFR 90-2 DGER OFR 90-7 47° WHITMAN PIERCE ADAMS THURSTON Westport Chehalis Mount Priest Pullman River Centralia Yakima Connell LEWIS Rainier Rapids FRANKLIN DGER DGER OFR 87-8 DGER OFR 87-8 DGER 46°30 DGER OFR 87-11 DGER OFR 87-16 OFR 86-4 OFR 94-12 DGER OFR 94-13 DGER OFR 94-14 DGER OFR 94-6 46°30 PACIFIC GARFIELD YAKIMA DGER COLUMBIA OFR 86-3 BENTON Ilwaco WAHKIAKUM Mount Clarkston Mount Richland Walla Walla Astoria St. -
Glossary Glossary
Glossary Glossary Albedo A measure of an object’s reflectivity. A pure white reflecting surface has an albedo of 1.0 (100%). A pitch-black, nonreflecting surface has an albedo of 0.0. The Moon is a fairly dark object with a combined albedo of 0.07 (reflecting 7% of the sunlight that falls upon it). The albedo range of the lunar maria is between 0.05 and 0.08. The brighter highlands have an albedo range from 0.09 to 0.15. Anorthosite Rocks rich in the mineral feldspar, making up much of the Moon’s bright highland regions. Aperture The diameter of a telescope’s objective lens or primary mirror. Apogee The point in the Moon’s orbit where it is furthest from the Earth. At apogee, the Moon can reach a maximum distance of 406,700 km from the Earth. Apollo The manned lunar program of the United States. Between July 1969 and December 1972, six Apollo missions landed on the Moon, allowing a total of 12 astronauts to explore its surface. Asteroid A minor planet. A large solid body of rock in orbit around the Sun. Banded crater A crater that displays dusky linear tracts on its inner walls and/or floor. 250 Basalt A dark, fine-grained volcanic rock, low in silicon, with a low viscosity. Basaltic material fills many of the Moon’s major basins, especially on the near side. Glossary Basin A very large circular impact structure (usually comprising multiple concentric rings) that usually displays some degree of flooding with lava. The largest and most conspicuous lava- flooded basins on the Moon are found on the near side, and most are filled to their outer edges with mare basalts. -
To See a Complete List of All Special Plates Types Available
2021 SPECIAL LICENSE PLATE FUND INFORMATION Plate Program Fund Name Responsible Organization (Idaho Code) Program Purpose Friends of 4-H Division University of Idaho Foundation 4H (49-420M) Funds to be used for educational events, training materials for youth and leaders, and to better prepare Idaho youth for future careers. Agriculture Ag in the Classroom Account Department of Agriculture (49-417B) Develop and present an ed. program for K-12 students with a better understanding of the crucial role of agriculture today, and how Idaho agriculture relates to the world. Appaloosa N/A Appaloosa Horse Club (49-420C) Funding of youth horse programs in Idaho. Idaho Aviation Foundation Idaho Aviation Association Aviation (49-420K) Funds use by the Idaho Aviation Foundation for grants relating to the maintenance, upgrade and development of airstrips and for improving access and promoting safety at backcountry and recreational airports in Idaho. N/A - Idaho Department of Parks and Recreation Biking (49-419E) Funds shall be used exclusively for the preservation, maintenance, and expansion of recreational trails within the state of Idaho and on which mountain biking is permitted. Capitol Commission Idaho Capitol Endowment Income Fund – IC 67-1611 Capitol Commission (49-420A) To help fund the restoration of the Idaho Capitol building located in Boise, Idaho. Centennial Highway Distribution Account Idaho Transportation Department (49-416) All revenue shall be deposited in the highway distribution account. Choose Life N/A Choose Life Idaho, Inc. (49-420R) To help support pregnancy help centers in Idaho. To engage in education and support of adoption as a positive choice for women, thus encouraging alternatives to abortion. -
Flood Basalts and Glacier Floods—Roadside Geology
u 0 by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 WASHINGTON STATE DEPARTMENTOF Natural Resources Jennifer M. Belcher - Commissioner of Public Lands Kaleen Cottingham - Supervisor FLOOD BASALTS AND GLACIER FLOODS: Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 Kaleen Cottingham - Supervisor Division of Geology and Earth Resources WASHINGTON DEPARTMENT OF NATURAL RESOURCES Jennifer M. Belcher-Commissio11er of Public Lands Kaleeo Cottingham-Supervisor DMSION OF GEOLOGY AND EARTH RESOURCES Raymond Lasmanis-State Geologist J. Eric Schuster-Assistant State Geologist William S. Lingley, Jr.-Assistant State Geologist This report is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources P.O. Box 47007 Olympia, WA 98504-7007 Price $ 3.24 Tax (WA residents only) ~ Total $ 3.50 Mail orders must be prepaid: please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources. Front Cover: Palouse Falls (56 m high) in the canyon of the Palouse River. Printed oo recycled paper Printed io the United States of America Contents 1 General geology of southeastern Washington 1 Magnetic polarity 2 Geologic time 2 Columbia River Basalt Group 2 Tectonic features 5 Quaternary sedimentation 6 Road log 7 Further reading 7 Acknowledgments 8 Part 1 - Walla Walla to Palouse Falls (69.0 miles) 21 Part 2 - Palouse Falls to Lower Monumental Dam (27.0 miles) 26 Part 3 - Lower Monumental Dam to Ice Harbor Dam (38.7 miles) 33 Part 4 - Ice Harbor Dam to Wallula Gap (26.7 mi les) 38 Part 5 - Wallula Gap to Walla Walla (42.0 miles) 44 References cited ILLUSTRATIONS I Figure 1. -
Idaho Mountain Goat Management Plan (2019-2024)
Idaho Mountain Goat Management Plan 2019-2024 Prepared by IDAHO DEPARTMENT OF FISH AND GAME June 2019 Recommended Citation: Idaho Mountain Goat Management Plan 2019-2024. Idaho Department of Fish and Game, Boise, USA. Team Members: Paul Atwood – Regional Wildlife Biologist Nathan Borg – Regional Wildlife Biologist Clay Hickey – Regional Wildlife Manager Michelle Kemner – Regional Wildlife Biologist Hollie Miyasaki– Wildlife Staff Biologist Morgan Pfander – Regional Wildlife Biologist Jake Powell – Regional Wildlife Biologist Bret Stansberry – Regional Wildlife Biologist Leona Svancara – GIS Analyst Laura Wolf – Team Leader & Regional Wildlife Biologist Contributors: Frances Cassirer – Wildlife Research Biologist Mark Drew – Wildlife Veterinarian Jon Rachael – Wildlife Game Manager Additional copies: Additional copies can be downloaded from the Idaho Department of Fish and Game website at fishandgame.idaho.gov Front Cover Photo: ©Hollie Miyasaki, IDFG Back Cover Photo: ©Laura Wolf, IDFG Idaho Department of Fish and Game (IDFG) adheres to all applicable state and federal laws and regulations related to discrimination on the basis of race, color, national origin, age, gender, disability or veteran’s status. If you feel you have been discriminated against in any program, activity, or facility of IDFG, or if you desire further information, please write to: Idaho Department of Fish and Game, P.O. Box 25, Boise, ID 83707 or U.S. Fish and Wildlife Service, Division of Federal Assistance, Mailstop: MBSP-4020, 4401 N. Fairfax Drive, Arlington, VA 22203, Telephone: (703) 358-2156. This publication will be made available in alternative formats upon request. Please contact IDFG for assistance. Costs associated with this publication are available from IDFG in accordance with Section 60-202, Idaho Code. -
Tectonic Alteration of a Major Neogene River Drainage of the Basin and Range
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2016 TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE Stuart D. Parker Follow this and additional works at: https://scholarworks.umt.edu/etd Part of the Tectonics and Structure Commons Let us know how access to this document benefits ou.y Recommended Citation Parker, Stuart D., "TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE" (2016). Graduate Student Theses, Dissertations, & Professional Papers. 10637. https://scholarworks.umt.edu/etd/10637 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE By STUART DOUGLAS PARKER Bachelor of Science, University of North Carolina-Asheville, Asheville, North Carolina, 2014 Thesis Presented in partial fulfillment of the requirements for the degree of Master of Science in Geology The University of Montana Missoula, MT May, 2016 Approved by: Scott Whittenburg, Dean of The Graduate School Graduate School James W. Sears, Committee Chair Department of Geosciences Rebecca Bendick Department of Geosciences Marc S. Hendrix Department of Geosciences Andrew Ware Department of Physics and Astronomy Parker, Stuart, M. S., May, 2016 Geology Tectonic alteration of a major Neogene river drainage of the Basin and Range Chairperson: James W. -
10. Palouse Prairie Section
10. Palouse Prairie Section Section Description The Palouse Prairie Section, part of the Columbia Plateau Ecoregion, is located along the western border of northern Idaho, extending west into Washington (Fig. 10.1, Fig. 10.2). This section is characterized by dissected loess-covered basalt plains, undulating plateaus, and river breaks. Elevation ranges from 220 to 1,700 m (722 to 5,577 ft). Soils are generally deep, loamy to silty, and have formed in loess, alluvium, or glacial outwash. The lower reaches and confluence of the Snake and Clearwater rivers are major waterbodies. Climate is maritime influenced. Precipitation ranges from 25 to 76 cm (10 to 30 in) annually, falling primarily during the fall, winter, and spring, and winter precipitation falls mostly as snow. Summers are relatively dry. Average annual temperature ranges from 7 to 12 ºC (45 to 54 ºF). The growing season varies with elevation and lasts 100 to 170 days. Population centers within the Idaho portion of the section are Lewiston and Moscow, and small agricultural communities are dispersed throughout. Outdoor recreational opportunities include hunting, angling, hiking, biking, and wildlife viewing. The largest Idaho Palouse Prairie grassland remnant on Gormsen Butte, south of Department of Fish and Moscow, Idaho with cropland surrounding © 2008 Janice Hill Game (IDFG) Wildlife Management Area (WMA) in Idaho, Craig Mountain WMA, is partially located within this section. The deep and highly-productive soils of the Palouse Prairie have made dryland farming the primary land use in this section. Approximately 44% of the land is used for agriculture with most farming operations occurring on private land. -
The Track of the Yellowstone Hot Spot: Volcanism, Faulting, and Uplift
Geological Society of America Memoir 179 1992 Chapter 1 The track of the Yellowstone hot spot: Volcanism, faulting, and uplift Kenneth L. Pierce and Lisa A. Morgan US. Geological Survey, MS 913, Box 25046, Federal Center, Denver, Colorado 80225 ABSTRACT The track of the Yellowstone hot spot is represented by a systematic northeast-trending linear belt of silicic, caldera-forming volcanism that arrived at Yel- lowstone 2 Ma, was near American Falls, Idaho about 10 Ma, and started about 16 Ma near the Nevada-Oregon-Idaho border. From 16 to 10 Ma, particularly 16 to 14 Ma, volcanism was widely dispersed around the inferred hot-spot track in a region that now forms a moderately high volcanic plateau. From 10 to 2 Ma, silicic volcanism migrated N54OE toward Yellowstone at about 3 cm/year, leaving in its wake the topographic and structural depression of the eastern Snake River Plain (SRP). This <lo-Ma hot-spot track has the same rate and direction as that predicted by motion of the North American plate over a thermal plume fixed in the mantle. The eastern SRP is a linear, mountain- bounded, 90-km-wide trench almost entirely(?) floored by calderas that are thinly cov- ered by basalt flows. The current hot-spot position at Yellowstone is spatially related to active faulting and uplift. Basin-and-range faults in the Yellowstone-SRP region are classified into six types based on both recency of offset and height of the associated bedrock escarpment. The distribution of these fault types permits definition of three adjoining belts of faults and a pattern of waxing, culminating, and waning fault activity. -
Boise Caldwell Nampa Idaho Falls Pocatello Twin Falls
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