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Oregon Historic Trails Report Book (1998)
i ,' o () (\ ô OnBcox HrsroRrc Tnans Rpponr ô o o o. o o o o (--) -,J arJ-- ö o {" , ã. |¡ t I o t o I I r- L L L L L (- Presented by the Oregon Trails Coordinating Council L , May,I998 U (- Compiled by Karen Bassett, Jim Renner, and Joyce White. Copyright @ 1998 Oregon Trails Coordinating Council Salem, Oregon All rights reserved. No part of this document may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage or retrieval system, without permission in writing from the publisher. Printed in the United States of America. Oregon Historic Trails Report Table of Contents Executive summary 1 Project history 3 Introduction to Oregon's Historic Trails 7 Oregon's National Historic Trails 11 Lewis and Clark National Historic Trail I3 Oregon National Historic Trail. 27 Applegate National Historic Trail .41 Nez Perce National Historic Trail .63 Oregon's Historic Trails 75 Klamath Trail, 19th Century 17 Jedediah Smith Route, 1828 81 Nathaniel Wyeth Route, t83211834 99 Benjamin Bonneville Route, 1 833/1 834 .. 115 Ewing Young Route, 1834/1837 .. t29 V/hitman Mission Route, 184l-1847 . .. t4t Upper Columbia River Route, 1841-1851 .. 167 John Fremont Route, 1843 .. 183 Meek Cutoff, 1845 .. 199 Cutoff to the Barlow Road, 1848-1884 217 Free Emigrant Road, 1853 225 Santiam Wagon Road, 1865-1939 233 General recommendations . 241 Product development guidelines 243 Acknowledgements 241 Lewis & Clark OREGON National Historic Trail, 1804-1806 I I t . .....¡.. ,r la RivaÌ ï L (t ¡ ...--."f Pðiräldton r,i " 'f Route description I (_-- tt |". -
Characterization of Ecoregions of Idaho
1 0 . C o l u m b i a P l a t e a u 1 3 . C e n t r a l B a s i n a n d R a n g e Ecoregion 10 is an arid grassland and sagebrush steppe that is surrounded by moister, predominantly forested, mountainous ecoregions. It is Ecoregion 13 is internally-drained and composed of north-trending, fault-block ranges and intervening, drier basins. It is vast and includes parts underlain by thick basalt. In the east, where precipitation is greater, deep loess soils have been extensively cultivated for wheat. of Nevada, Utah, California, and Idaho. In Idaho, sagebrush grassland, saltbush–greasewood, mountain brush, and woodland occur; forests are absent unlike in the cooler, wetter, more rugged Ecoregion 19. Grazing is widespread. Cropland is less common than in Ecoregions 12 and 80. Ecoregions of Idaho The unforested hills and plateaus of the Dissected Loess Uplands ecoregion are cut by the canyons of Ecoregion 10l and are disjunct. 10f Pure grasslands dominate lower elevations. Mountain brush grows on higher, moister sites. Grazing and farming have eliminated The arid Shadscale-Dominated Saline Basins ecoregion is nearly flat, internally-drained, and has light-colored alkaline soils that are Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and America into 15 ecological regions. Level II divides the continent into 52 regions Literature Cited: much of the original plant cover. Nevertheless, Ecoregion 10f is not as suited to farming as Ecoregions 10h and 10j because it has thinner soils. -
Wolverines in Idaho 2014–2019
Management Plan for the Conservation of Wolverines in Idaho 2014–2019 Prepared by IDAHO DEPARTMENT OF FISH AND GAME July 2014 2 Idaho Department of Fish & Game Recommended Citation: Idaho Department of Fish and Game. 2014. Management plan for the conservation of wolverines in Idaho. Idaho Department of Fish and Game, Boise, USA. Idaho Department of Fish and Game – Wolverine Planning Team: Becky Abel – Regional Wildlife Diversity Biologist, Southeast Region Bryan Aber – Regional Wildlife Biologist, Upper Snake Region Scott Bergen PhD – Senior Wildlife Research Biologist, Statewide, Pocatello William Bosworth – Regional Wildlife Biologist, Southwest Region Rob Cavallaro – Regional Wildlife Diversity Biologist, Upper Snake Region Rita D Dixon PhD – State Wildlife Action Plan Coordinator, Headquarters Diane Evans Mack – Regional Wildlife Diversity Biologist, McCall Subregion Sonya J Knetter – Wildlife Diversity Program GIS Analyst, Headquarters Zach Lockyer – Regional Wildlife Biologist, Southeast Region Michael Lucid – Regional Wildlife Diversity Biologist, Panhandle Region Joel Sauder PhD – Regional Wildlife Diversity Biologist, Clearwater Region Ben Studer – Web and Digital Communications Lead, Headquarters Leona K Svancara PhD – Spatial Ecology Program Lead, Headquarters Beth Waterbury – Team Leader & Regional Wildlife Diversity Biologist, Salmon Region Craig White PhD – Regional Wildlife Manager, Southwest Region Ross Winton – Regional Wildlife Diversity Biologist, Magic Valley Region Additional copies: Additional copies can be downloaded from the Idaho Department of Fish and Game website at fishandgame.idaho.gov/wolverine-conservation-plan Front Cover Photo: Composite photo: Wolverine photo by AYImages; background photo of the Beaverhead Mountains, Lemhi County, Idaho by Rob Spence, Greater Yellowstone Wolverine Program, Wildlife conservation Society. Back Cover Photo: Release of Wolverine F4, a study animal from the Central Idaho Winter Recreation/Wolverine Project, from a live trap north of McCall, 2011. -
Clearwater Rapid Watershed Assessment
Clearwater - 17060306 Idaho 8 Digit Hydrologic Unit Profile December 2006 Tensed Farmington Clearwater - 17060306 8-Digit Hydrologic Unit LATAHLATAH Location Map Potlatch Bovill WHITMAN WHITMAN Deary (Washington) (Washington) Elk River Troy Moscow CLEARWATERCLEARWATER Kendrick Juliaetta Genesee Pierce Clearwater Peck Orofino Clarkston 17060306 Lapwai Culdesac Weippe Lewiston Asotin Reubens LEWISLEWIS Kamiah Craigmont Winchester Nezperce Kooskia Ferdinand NEZNEZ Stites PERCEPERCE Cottonwood !COEUR d ALENE MOSCOW! IDAHOIDAHO Grangeville LEWISTON! !REXBURG CALDWELL! !BOISE NAMPA! !IDAHO FALLS : BLACKFOOT ! !POCATELLO 0 5 10 15 20 25 TWIN! FALLS Miles The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, sex, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at 202-720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326W, Whitten Building, 14 th and Independence Avenue, SW, Washington DC 20250-9410 or call (202) 720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. 1 Clearwater - 17060306 Idaho 8 Digit Hydrologic Unit Profile December 2006 Introduction The Clearwater 8-Digit Hydrologic Unit Code (HUC) subbasin is 1,503,992 acres. Clearwater and Nez Perce counties each account for approximately 24 percent of the subbasin. Twenty two percent of the subbasin is in Latah County, 18 percent in Lewis County, 13 percent in Idaho County and less than 0.5% in Whitman County, Washington. -
Geographic Variations in Water Quality and Recreational Use Along the Upper Wallowa River and Selected Tributaries
AN ABSTRACT OF THE THESIS OF Theodore R. McDowellfor the degree ofDoctor of Philosophy in Geography presented on December 21, 1979 Title:Geographic Variations in Water Quality and Recreational Use Along the Upper Wallowa River and Selected Tributaries Abstract approved: Redacted for privacy Assistant Pro(sp)sornarl es Rosenfeld Physical, chemical and bacterial water quality parameters of the upper Wallowa River were sampled periodically between July 2, 1978 and June 9, 1979 at nine stream and lake sampling sites.Water upstream from Wallowa Lake was typified by low nutrient concentra- tions ( generally below detectable limits except for nitrates), low. specific conductivity (50-99 micromhos), and water temperatures below 15°C.Results of bacterial sampling were inconclusive, but sites and areas warranting further study were identified. An intensive study of spatial variations in bacterial water quality and recreational use was conducted at 15 stream and lake sampling sites on the East Fork of the Wallowa River between July 5 and September 3, 1979.Streamflow, precipitation, water temperatures, and fecal coliform bacteria counts were determined two or three times per week and during storm events.Levels and patterns of recreational use were also monitored during that period.Fecal coliform counts varied significantly (at the 0.001 p level) with geographic patterns of recreational use, but there was no significant relationship between levels of recreational use.Bacterial water quality also varied signi- ficantly (at the 0.001 p level) between -
The Geology of Part of the Snake River Canyon and Adjacent Areas in Northeastern Oregon and Western Idaho
AN ABSTRACT OF THE THESIS OF Tracy Lowell Vallier for the Ph.D. in Geology (Name) (Degree) (Major) Date thesis is presented May 1, 1967 Title THE GEOLOGY OF PART OF THE SNAKE RIVER CANYON AND ADJACENT AREAS IN NORTHEAXERN OREGON AND WESTERN IDAHO Abstract approved Redacted for Privacy (Major professor) The mapped area lies between the Wallowa Mountains of northeastern Oregon and the Seven Devils Mountains of western Idaho. Part of the Snake River canyon is in- cluded. A composite stratigraphic section includes at least 30,000 feet of strata. Pre- Tertiary and Tertiary strata are separated by a profound unconformity. Pre -Tertiary layered rocks are mostly Permian and Triassic volcani- clastic and volcanic flow rocks. At least four pre -Ter- tiary intrusive suites occur. Tertiary rocks are Miocene and Pliocene plateau basalts. Quaternary glacial materi- als and stream deposits locally mantle the older rocks. Permian ( ?) rocks of the Windy Ridge Formation are the oldest rocks and consist of 2,000 to 3,000 feet of keratophyre, quartz keratophyre, and keratophric pyro- clastic rocks. Unconformably ( ?) overlying the Windy Ridge Formation are 8,000 to 10,000 feet of volcaniclastic rocks and minor volcanic flow rocks of the Hunsaker Creek Formation of Middle Permian (Leonardian and Wordian) age. Spilitic flow rocks of the Kleinschmidt Volcanics are interlayered with and in part overlie the Hunsaker Creek Formation and comprise a sequence about 2,000 to 3,000 feet thick. The Paleozoic layered rocks were intruded by the Holbrook - Irondyke intrusives, composed of keratophyre porphyry, quartz keratophyre porphyry, diabase, and gab- bro. -
Phacelia Lyallii and Physaria Didymocarpa Var
FIELD INVESTIGATIONS OF TWO SENSITIVE PLANT SPECIES ON THE SALMON NATIONAL FOREST: PHACELIA LYALLII AND PHYSARIA DIDYMOCARPA VAR. LYRATA by Robert K. Moseley, Michael Mancuso and Steven L. Caicco Natural Heritage Section Nongame/Endangered Wildlife Program Bureau of Wildlife December 1990 Idaho Department of Fish and Game 600 South Walnut, P.O. Box 25 Boise, Idaho 83707 Jerry M. Conley, Director Cooperative Challenge Cost-share Project Salmon National Forest Idaho Department of Fish and Game ABSTRACT Field investigations of Phacelia lyallii (Lyall's phacelia) and Physaria didymocarpa var. lyrata (Salmon twin bladderpod) were conducted on the Salmon National Forest by the Idaho Department of Fish and Game's Natural Heritage Program. The investigations were a cooperative Challenge Cost-share project between the Department and the Salmon NF. Lyall's phacelia is endemic to the northern Rocky Mountains, occurring on the southern edge of its range in Idaho, while Salmon twin bladderpod is restricted to the Salmon area. Both plants are on the Intermountain Region's Sensitive Plant Species List. Previous to 1990, only three populations of Lyall's phacelia were known from the Salmon NF, two in the Beaverhead Mountains east of Salmon and one in the northern Lemhi Range. Inventories this year did not expand on this pattern much, discovering only three new populations in the Beaverhead's; this despite considerable searches in the Beaverhead Mountains, Lemhi Range, and Salmon River Mountains. Less than 2,000 plants are known from Idaho. No clear threats to long-term viability were apparent, but the highly localized nature of the populations make them vulnerable to extirpation from habitat destroying activities, such as mining. -
Oregon State Parks
iocuN OR I Hi ,tP7x OREGON STATE PARKS HISTORY 1917-1963 \STATE/ COMPILED by CHESTER H. ARMSTRONG JULY I. 1965 The actual date of the i is less than thirty years ag older, supported by a few o were an innovation as so lit The Oregon parks system o beautification advocated b: Governors, the early State ] neers. The records reveal out areas, made favorable were generous with their Roy A. Klein, State Highk& ary 29, 1932, as a leader wl The state parks system thought of highway beauti many highway users who h who could not well afford t] In the park story we fii the many influential people complete, it is necessary to thought or trend in the idea the thought of highway be, may see and follow the trai present state narks system. In the preparation of th $ been examined. It was neck ing to property acquisitions deeds and agreements. as tln records of the Parks Divisik Excellent information h; State Parks and Recreatioi A Public Relations Office. As many etbers. I Preface The actual date of the founding of the Oregon State Parks System is less than thirty years ago but the fundamental principles are much older, supported by a few of the leading park people of that time. They were an innovation as so little had been done by any state in the Union. The Oregon parks system owes its beginning to the thought of highway beautification advocated by many leaders of the state, including the Governors, the early State Highway Commissioners and Highway Engi- neers. -
Or Wilderness Protection in the Blue Mountain Ecoregion Have Been Identified by the Nature Conservancy As Vital to Protect Biodiversity in the Area
172 OREGON WILD Neither Cascades nor Rockies, but With Attributes of Both Blue Mountains Ecoregion xtending from Oregon’s East Cascades Slopes and Foothills to the from 30 to 130 days depending on elevation. The forests are home to Rocky Mountain intersection of Oregon, Idaho and Washington, the 15.3 million acres elk, mule deer, black bear, cougar, bobcat, coyote, beaver, marten, raccoon, fisher, of the Blue Mountains Ecoregion in Oregon are a conglomeration of pileated woodpecker, golden eagle, chickadee and nuthatch, as well as various species Emountain ranges, broad plateaus, sparse valleys, spectacular river canyons of hawks, woodpeckers, owls and songbirds. Wolves, long absent from Oregon, are and deep gorges. The highest point is the Matterhorn that rises to 9,832 making their return to the state in this ecoregion. Individuals from packs reintroduced feet in the Wallowa Mountains. The ecoregion extends into southeastern Washington in nearby Idaho are dispersing into Oregon. Fish species include bull and rainbow and west central Idaho. trout, along with numerous stocks of Pacific salmon species. Most of the mountain ranges in the Blue Mountains Ecoregion are volcanic. The Depending on precipitation, aspect, soil type, elevation, fire history and other Crooked River separates the Maury Mountains from the Ochoco Mountains, which are factors, one generally finds various combinations of Douglas-fir, ponderosa pine, lodge- separated from the Aldrich Mountains by the South Fork John Day River. The Aldrich pole, western larch, juniper and Engelmann spruce throughout the Blue Mountains. Mountains are separated from the Strawberry Mountain Range by Canyon Creek. Beginning approximately at the Lower Deschutes River and rising eastward, the These ranges generally run east-west. -
Redacted for Privacy
Redacted for privacy The Early Jurassic "Grade Creek conglomerate" has amini- mum thickness of 400 feetand unconformably overlies the Seven Devils Volcanics.Unconformably (?) overlying the conglomerate unit is the "Camp Creek latite" which is 300-400feet thick and Early Jurassic in age.Tectonicly overlying the latite is more than 1,000 feet of gray to black shales and interbedded conglomeraticschists of the Early Jurassic "Brownlee Canyon series." Flows ofMiocene to Early Pliocene Columbia River Basalthave a maximum thickness of 1, 000 feet and upconformably overlie all pre-Tertiaryrocks. Major phases of the Cuddy Mountain intrusive complex are porphyritic granodiorite (200 ± 5 m. y.), hornblende gabbro, and leucocratic quartz diorite in order of decreasing age. Two periods of alteration are present. The first episode altered part ofthe porphyritic granocliorite to a rock that is chemically and mineralogi- cally similar to the albite granites near Sparta, Oregon.The last stage represents hydrothermal alteration related tointrusion of leucocratic quartz diorite. Regional, contact, and dislocation metamorphism are present in this area.All pre-Tertiary stratigraphic units and the porphyritic granodiorite have been subjected to greenschist regional meta- morphism during Middle Jurassic time. The hornblende gabbro and leucocratic quartz diorite are believed to postdate regional meta- morphism. Parts of the porphyritic granodiorite and hornblende gabbro have been contact metamorphosed to the hornblende hornfels facies by the leucocratic quartz -
Recreation Overview
APPENDIX 8-1 RECREATION OVERVIEW SUMMARY: Recreation and tourism are increasingly important parts of Wallowa County’s economy. Overall tourism and recreation spending has doubled over the last ten years, with an increased emphasis on conventional tourism (As opposed to more traditional recreation such as hunting, fishing and backcountry trips, conventional tourism is more centered on nice lodging, fine dining, shopping and sight seeing). People come to Wallowa County for scenery, solitude, camping, picnicking, boating, snow and water skiing, snowmobiling, auto touring, hiking and backpacking, horseback riding, fishing, hunting, and to visit the shops, galleries and restaurants in the Joseph and the Wallowa Lake area.. Recreation is centered around Wallowa Lake and the Eagle Cap Wilderness and to a lesser extent the streams and rivers of the County including the Snake River and the Hells Canyon National Recreation Area. Tourism is centered around Joseph and the Wallowa Lake area. PAST AND PRESENT: Recreation and tourism are considered a primary part of the County’s economy , and are the fastest growing segment of the economy. Wallowa Lake and Joseph are the center of tourism in the County and the State Park at Wallowa Lake is a major attraction. The Joseph Economic Improvement District and resultant improvements has turned Joseph into a center for tourism, and has led to a doubling of businesses on main street. This industry is highly seasonal and operates from late May to mid October, with peak activity from the first of July to mid October. The tourist facilities at the lake, including the State Park parking area, the moorage and docks, short term rentals, the motels, and the restaurants, now stand idle during the winter months. -
Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington
Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey Cover. Palouse Falls, Washington. The Palouse River originates in Idaho and flows westward before it enters the Snake River near Lyons Ferry, Washington. About 10 kilometers north of this confluence, the river has eroded through the Wanapum Basalt and upper portion of the Grande Ronde Basalt to produce Palouse Falls, where the river drops 60 meters (198 feet) into the plunge pool below. The river’s course was created during the cataclysmic Missoula floods of the Pleistocene as ice dams along the Clark Fork River in Idaho periodically broke and reformed. These events released water from Glacial Lake Missoula, with the resulting floods into Washington creating the Channeled Scablands and Glacial Lake Lewis. Palouse Falls was created by headward erosion of these floodwaters as they spilled over the basalt into the Snake River. After the last of the floodwaters receded, the Palouse River began to follow the scabland channel it resides in today. Photograph by Stephen P. Reidel. Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington By Victor E. Camp, Stephen P. Reidel, Martin E. Ross, Richard J. Brown, and Stephen Self Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S.