CONFLICTS in the MULTIPLE USE of WALLOWA LAKE Abstract Approved Redacted for Privacy Keith W
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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 |". -
Interpreting Landscape Change in High Mountains of Northeastern Oregon from Long-Term Repeat Photography
United States Department of Interpreting Landscape Change in High Agriculture Forest Service Mountains of Northeastern Oregon from Pacific Northwest Research Station Long-Term Repeat Photography General Technical Report Jon M. Skovlin, Gerald S. Strickler, Jesse L. Peterson, PNW-GTR-505 May 2001 and Arthur W. Sampson Photo by Harley Richardson 1920 Photo by David Jensen 1992 Authors Jon M. Skovlin (retired) was a principal research scientist, Forestry and Range Sciences Laboratory, 1401 Gekeler Lane, La Grande, OR 97850. He now is a consultant on renewable natural resources, P.O. Box 121, Cove, OR 97824. Gerald S. Strickler (deceased) was a range scientist, Forestry and Range Sciences Laboratory, 1401 Gekeler Lane, La Grande, OR 97850. Jesse L. Peterson (deceased) was range examiner, Wallowa National Forest, Wallowa, OR, and later chief range examiner, Whitman National Forest, Baker City, OR. Arthur W. Sampson (deceased) was the pioneer range scientist, U.S. Department of Agriculture, Forest Service, and later Professor of Forestry, University of California, Berkeley, CA. This publication was prepared under contract with the Blue Mountains Natural Resources Institute, La Grande, OR. All photos not otherwise credited were taken by the senior author. Cover Photos Glacier Peak is a satellite point along Eagle Cap Ridge, which is the central watershed feature of the Wallowa Mountain batholith. Upper–This photo of Benson Glacier looking south from Glacier Lake was taken in about 1920. The conspicuous glacier flow lines and crevasses affirm its activity, which had been in recession since about 1870 after the end of the Little Ice Age in about 1850. Harley Richardson captured the Benson Glacier on film when it was in rapid retreat. -
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 -
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. -
West Fork Wallowa River Trail #1820
FOREST TRAILS SERVICE 2 to 3 day trip Wallowa-Whitman National Forest Wallowa Mountains Visitor Center Eagle Cap Wilderness 201 East 2nd Street P.O. Box 905 Joseph, OR 97846 (541) 426-5546 www.fs.usda.gov/wallowa-whitman WEST FORK WALLOWA RIVER TRAIL #1820 TRAIL BEGINNING: West Fork Wallowa River Trailhead (Wallowa Lake) TRAIL ENDING: Hawkins Pass ACCESS: From Enterprise, Oregon, take State Highway #82 through Joseph and past Wallowa Lake. The trailhead is at the end of the road approximately one mile past the lake. Parking is available at the trailhead along with a loading ramp and hitch rails for stock. ATTRACTIONS: The trail follows the west fork of the Wallowa River through open meadows and forests. The trail is a gradual climb to Six Mile Meadow, then becomes steeper up to Hawkins Pass. Many wildflowers can be seen along the trail such as mountain bluebells, forget-me-nots, paintbrush and columbine. There are fishing opportunities near Six Mile Meadows where the river flows a little slower. Keep your eyes open for indications of past landslides and avalanches. Frazier Lake and Little Frazier Lake are at the end of this hike, where you will have spectacular views of limestone cliffs and a waterfall cascading down the cliffs. CONSIDERATIONS: Northwest Forest Passes are NOT required at Wallowa Lake Trailhead. The trail is well maintained for hikers and stock. It is signed at the trailhead and at all main junctions. This trail provides access to many other trails, and to the Lakes Basin. There are no campsites at the trailhead. -
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. -
Transportation Development Division
SECTION II TRAFFIC VOLUMES ON STATE HIGHWAYS An asterisk (*) appearing to the left of a count location description indicates an Automatic Traffic Recorder (ATR) Station or Automatic Vehicle Classification (AVC) Station. See Section IV of this book for 2017 monthly traffic volumes, high hour volumes or historical trends at these stations. 29 30 2017 TRAFFIC VOLUMES ON STATE HIGHWAYS 2017 AADT All ATR Milepoint Vehicles AVC Location Description PACIFIC HIGHWAY NO. 1 Milepoint indicates distance from Oregon-California State Line 0.00 16900 Oregon-California State Line 5.02 16800 0.30 mile south of Siskiyou Interchange Neil Creek Automatic Traffic Recorder, Sta. 15-002, 0.86 mile south of Rogue Valley Highway No. 63 11.03 17200 * Interchange (OR99) 13.67 16600 0.50 mile south of Green Springs Highway Interchange (OR66) 18.11 28100 * North Ashland Automatic Traffic Recorder, Sta. 15-021, 0.98 mile south of North Ashland Interchange 19.87 39000 0.77 mile north of North Ashland Interchange 23.90 41500 0.50 mile south of Fern Valley Road Interchange 26.91 43100 0.30 mile south of South Medford Interchange Medford Viaduct Automatic Traffic Recorder, Sta. 15-019, 1.96 miles southeast of the North Medford 28.33 53200 * Interchange 30.59 42700 0.30 mile north of Crater Lake Highway Interchange (OR62) 34.94 38800 0.50 mile south of Seven Oaks Interchange 36.04 41100 0.60 mile north of Seven Oaks Interchange 42.84 40000 * Gold Hill Automatic Traffic Recorder, Sta. 15-001, 2.77 miles south of the Homestead Interchange 44.97 40300 0.50 mile east of Rogue River Highway (OR99), Homestead Interchange 45.61 39300 On Rogue River Bridge 48.32 39100 0.50 mile east of Rogue River Interchange 55.38 37800 0.40 mile south of East Grants Pass Interchange (US199) 57.56 28600 0.50 mile south of Redwood Highway (OR99), North Grants Pass Interchange 61.05 31700 0.40 mile south of Louse Creek Interchange Grave Creek Automatic Traffic Recorder, Sta. -
Joseph M. Licciardi for the Degree of Doctor of Philosophy in Geology Presented On
AN ABSTRACT OF THE DISSERTATION OF Joseph M. Licciardi for the degree of Doctor of Philosophy in Geology presented on September 26, 2000. Title: Alpine Glacier and Pluvial Lake Records of Late Pleistocene Climate Variability in the Western United States. Redacted for privacy Abstract approved: Peter U. Clark This investigation focuses on the development of Quaternary dating techniques to construct high-resolution numerical chronologies of late-Pleistocene climate variability in the western United States. Cosmogenic 3He concentrations were measured in radiocarbon-dated olivine-bearing Holocene lava flows in Oregon, yielding a mean production rate of 116 ± 3 3He atoms g1 yf'. This value is consistent with previous estimates at mid-latitides, and helps refine the accuracy of the cosmogenic 3He dating technique. Cosmogenic 3He and 10Be chronologies were developed for well-preserved moraine sequences in the northern Yellowstone region, Montana, and in the Wallowa Mountains, Oregon. Cosmogenic data indicate that the northern outlet glacier of the Yellowstone ice cap reached its terminal moraine at 16.7 3He ka / 16.2 '°Be ka, and retreated to 50% of its maximum extent by13.8 ka. In the Wallowa Mountains, two major late-Pleistocene alpine glacier advances occurred at21 and -'17 ka, and a minor advance occurred at '-41 ka. The '-21 ka advance in the Wallowa Mountains coincides with the last glacial maximum, and is correlative with the last Pinedale maximum advance in the Wind River Mountains. The '-47 ka advance in the Wallowa Mountains is probably correlative with the advance of the northern Yellowstone outlet glacier. The youngest event in the Wallowa Mountains, at -11 ka, may be correlative to an advance that deposited the Titcomb Lakes moraines in the Wind River Mountains during the Younger Dryas. -
SUMMER HORSEPACK ADVENTURES 64591 Steen Rd TRIPS Joseph, OR 97846 541-432-6545 [email protected] Steens-Packtrips.Com
STEEN’S WILDERNESS SUMMER HORSEPACK ADVENTURES 64591 Steen Rd TRIPS Joseph, OR 97846 541-432-6545 [email protected] steens-packtrips.com WHERE DO THE TRIPS GO Our trips can go anywhere in Hells Canyon and the Eagle Cap Wilderness. We begin in Hells canyon in the spring, exploring wide open country that was the winter range for the Nez pierce Indians and home to many homesteaders. We run our Hells Canyon trips in April, May & June. After that it gets too hot in the canyon for our comfort and we move to the Eagle Cap Wilderness where the snow has just began to clear on the high passes and trails are beginning to open up after a long winter & spring of trees blowing down. Mid July through mid September is a great time to be in the Eagle Cap wilderness exploring The High Alpine country and fishing the high mountain lakes. TRIP STARTING POINT We will meet you at either our ranch 2 miles from Joseph, OR or at the designated trailhead. We will discuss this prior to the trip. GETTING TO JOSEPH, OREGON If you are driving, you can reach Joseph by taking Highway 82 off of I 84 in LaGrande or by taking Highway 3 from Lewiston, ID. Joseph is 76 miles from LaGrande and 80 miles from Lewiston. If you will not be driving in to Joseph, we can make arrangements to pick you up at the airport in Lewiston, Walla Walla, Pendleton, or Pasco. LODGING Most of our guests arrive in Joseph a day or two prior to their trip. -
Nez Perce National Historic Trail Progress Report Fall 2009
Nez Perce National Historic Trail Progress Report Fall 2009 Administrator’s Corner I would like to open this message by introducing you to Roger Peterson. Roger recently accepted the position of Public Affairs Specialist for the Nez Perce National Historic Trail (NPNHT). I want to recognize him for his exemplary work and for stepping up to take on this position. He has already earned respect for us within our Administration through his professionalism, knowledge, and dedication to the NPNHT. I know that you will welcome him to our trails community. I have a long list of items that I want to work on over the next year. These include the need to continue fine tuning our challenge cost share program, Sandi McFarland, at the Conference on National Scenic and Historic trails in Missoula, launching into our public sensing meetings in preparation for the revision of the Mont., July 2009 NPNHT comprehensive management plan, implementing a trail wide interpretive strategy to update old signs, and finding opportunities for new ones, to name a few. As Trail Administrator, the stewardship and care of our NPNHT, service to our visitors, education, interpretation, and expansion of our challenge cost share program are some of my core responsibilities. I will continue working to ensure that all Trail visitors have a positive experience, no matter if they visit by foot, horse, motorized, or virtually via the Trail’s website. Stewardship of our natural and cultural resources has always been a core value of mine. Our mission is to manage this treasured landscape of history for the enjoyment of future generations. -
Wallowa County Wildfire Protection Plan August 30, 2017
Wallowa County Wildfire Protection Plan August 30, 2017 IV. Wallowa County Profile Introduction The Nez Perce Tribe originally occupied a territory that encompassed virtually all of what is now north central Idaho as well as extensive portions of what is now southeastern Washington and northeastern Oregon, including Wallowa County. Wallowa County has a long history of Native American influence, with the Wallowa Band of the Nez Perce once making the Wallowa Valley their home for hunting, fishing, and gathering. They followed changing seasons from headwaters of rivers in spring, to high mountains of the Wallowas in summer and returned to deep canyons of the Snake River and its tributaries in winter (Nez Perce 2017). Wallowa County, Oregon's far northeastern county, shares state boundaries with both Washington and Idaho. The county is mostly mountainous and forms the headwaters of several important tributaries to the Columbia/Snake River System. About 3/5 of the land area in Wallowa County is publicly owned, including lands administered by a variety of federal, state, and local agencies (Table IV – 1). Most public land is part of the Wallowa-Whitman National Forest and is administered by the United States Forest Service (USFS). Wallowa County is considered part of the northern portion of the Blue Mountain range characterized by a dissection of ridges and valleys typical of the Blue Mountains. The rugged landscape hosts the Blue’s most scenic mountains called the Wallowas. These snow-capped peaks, dramatic river canyons are classic glacial topography (WCChamber, 2017). Wallowa County encompasses 3,152 square miles (2,017,280 acres).