Draft Exhibit Outline June 23, 2020 Wallowa History Center
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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. -
Wallowa County, Oregon and Environs
Moving On By Winona Johnson Holloway J; ~tnn,I ~M ;r= ·~ - ;}/-~ _?~ lq?7 Moving On by WinonaJohnson Holloway ©1989 Shadow Butte Press Live Oak, California All rights reserved included the right to reproduce this book or parts thereof in any form Cover picture courtesy of Alice Mccully Printed by "The Printer" in Davis, California, U.S.A. I I dedicate this book to Merritt Louis Holloway, whose genes have mixed with mine to produce our own line of descendants, now in its fourth generation. Thank you Merritt for having such interesting ancestors. Thank you for our adventurous life together. II Our past is not a dead past. It is still alive in little pockets and trickles to surprise us in places still to be found. How lucky are those who have perceived it- a spark that shines within us dimly-to tell us who we are and why and how. We know better where we are going, if we know from whence we came. WJH III Grover and Zora Johnson and family, 1926 Front: Zora, Grace, Joe, Tom, Maybeth, Grover Rear: Winona, Dorofy, Ellen, Mildred IV Moving On Contents Chapter 1 Others came before me ............................................................................ 1 Chapter 2 The world is full of a number of things ................................................. 15 Chapter 3 That was the time that was, a time that will not come again ............... 39 Chapter 4 Of fun and foibles ................................................................................ 71 Chapter 5 As the twig is bent, the tree's inclined ................................................... 87 Chapter 6 Making do ............................................................................................ 103 Chapter 7 On my own .......................................................................................... 125 Chapter 8 In which we try it out there in the big world ........................................... -
Longley Meadows Fish Habitat Enhancement Project Heritage Resources Specialist Report
Longley Meadows Fish Habitat Enhancement Project Heritage Resources Specialist Report Prepared By: Reed McDonald Snake River Area Office Archaeologist Bureau of Reclamation June 20, 2019 Heritage Resources Introduction This section discusses the existing conditions and effects of implementation of the Longley Meadows project on cultural resources, also known as heritage resources, which are integral facets of the human environment. The term “cultural resources” encompasses a variety of resource types, including archaeological, historic, ethnographic and traditional sites or places. These sites or places are non- renewable vestiges of our Nation’s heritage, highly valued by Tribes and the public as irreplaceable, many of which are worthy of protection and preservation. Related cultural resource reports and analyses can be found in the Longley Meadows Analysis File. Affected Environment Pre-Contact History The Longley Meadows area of potential effect (APE) for cultural resources lies within the Plateau culture area, which extends from the Cascades to the Rockies, and from the Columbia River into southern Canada (Ames et al. 1998). Most of the archaeological work in the Columbia Plateau has been conducted along the Columbia and Snake Rivers. This section discusses the broad culture history in the Southern Plateau. Much variability exists in the Plateau culture area due to the mountainous terrain and various climatic zones within it. Plateau peoples adapted to these differing ecoregions largely by practicing transhumance, whereby groups followed -
DOGAMI Special Paper 6, Geology of the La Grande Area, Oregon
oc w 0... � 0... GEOLOGY OF THE LA GRANDE AREA, -' � u w OREGON 0... V) 1980 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUS TRIES D.A. HULL, STATE GEOLOGIST STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1069 State Office Building, Portland, Oregon 97201 SPECIAL PAPER 6 '\. � Warren Barrash John G. Bond John D. Kauffman Ramesh Venkatakrishnan GEOSCIENCE RESEARCH CONSULTANTS t1JSC�I IDAHO Conducted in conformance with ORS 516.030 Funded by the Oregon Department of Geology and Mineral Industries under contract with the U.S. Department of Energy DE-FC07-79ET27220 GOVERNING BOARD STATE GEOLOGIST John L. Schwabe, Chairman Portland Donald A. Hu11 Robert W. Doty Talent DEPUTY STATE GEOLOGIST C. Stanley Rasmussen Baker John D. Beaulieu CONTENTS page ILLUSTRATIONS iv Figures iv Tables iv Plates iv INTRODUCTION 1 Purpose and Scope 1 Acknowledgments 1 Program Summary 1 Chronology and presentation of 1979 study 1 Division of work 2 General Se tting 2 Location and access 2 Physiography and climate 2 Previous Work 2 Regional Overview 5 Thermal Springs and Wells 7 STRATIGRAPHY 10 Columbia River Basalt Group 10 Grande Ronde Basalt 13 Basalt of Glass Hill 15 Diktytax1tic basalt 17 Glassy bas a 1t 17 Coarse-grained basalt 17 Black olivine basalt 17 Interbedded sediments 19 Andesites of Mahogany Mountain and Craig Mountain 19 Quaternary deposits 20 STRUCTURE 24 Photo-Linear Fabric 24 Long linears 27 Topographic linears 27 Short linears 27 Photo-linear fault-trace associations 27 Tectonic considerations 29 Hilgard Uplands 30 Grande Ronde syncline 30 Hilgard mono�line 30 Sheep Creek monocline 31 Hhiskey Creek fault system 31 Rock Creek fault system 31 Peach Canyon fault 31 Morris Hill fault 33 Long Prairie fault 33 La Grande Front 33 Wilson Canyon-�1i11 Creek faults 33 Deal Creek fau 1 t 33 La Grande fault system 34 Craig t-1ountain 34 l�estern boundary structures 34 Structures within the Craig Mountain structural block 37 Craig Mountain Front 37 Grande Ronde Valley 37 GEOLOGIC HISTORY 39 REFERENCES CITED 43 APPENDIX 45 iii ILLUSTRATIONS Figures Page 1. -
River Basin Assessment
RIVER BASIN ASSESSMENT UPPERIMIDDLE GRANDE RONDE RIVER 8t CATHERINE CREEK June 1995 Developed By: Leslie B. Bach Oregon Department of Environmental Quality Project Staff: Thomas Kaye ~ Oregon Department of Agriculture Larry Caton & D. Mitch Wolgamott. .. Oregon Department of Environmental Quality Jim Turner & Mary Hanson Oregon Department of Fish and Wlldllfe Daniel Wermlel Oregon Department of Geology and Mineral Industries Eric Gillett & Mathew Gilson .. Oregon Department of Administrative Services (State Service Center for Geographical Information Systems) ti.u BLJ: The Oregon Watershed Health Program ACKNOWLEDGMENTS Water Quality Division Administrator Mike Downs Surface Water Section Kevin Downing, Acting Manager Layout Design, Graphics, 8t Typesetting Hope Y. Smith CCJJonnie" Word Processing Chris R. Watson A number ofpeople assisted in creating this document by providing data, analysis, information, ideas or technical review. A sincere thank you goes to: Dr. Ellen Blsbop - Oregon Watersbed Healtb Program; Marcia Brett - Oregon State University, Aaron Bodor Oregon Dept. of Environmental Quality; Stepbanle Burcbfield - Oregon Dept. of Flsb and Wildlife; Mlcbael Clscell Oregon Water Resources Department; Amy Clark - Oregon Dept. of Environmental Quality; Sbaron Clarke - U.S. Forest Service, Pacific Nortbwest Researcb Station;Rlcbard Cooper - Oregon Water ResourcesDepartment; Ronald Geltgey - Oregon Dept. of Geology and Minerai Industries; Karl Grover - USFS, Wallowa·Wbltman National Forest; Milton mil - Oregon Dept. of Flsb and Wildlife; Mark HenJum - Oregon Dept. of Flsb and Wildlife; Dr. Herbert Huddleston - Oregon State University; Cbarles Huntington - Clearwater Blostudles, Inc.; Dr. Ray Jalndl - Oregon Dept. of Agriculture; Jimmy Kagan - Oregon Natural Heritage Program; Albert Mlrati - Oregon Dept. of Flsb and Wildlife; Reed Marbut - Oregon Water Resources Department; Kelly Moore - Oregon Dept. -
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 -
Ripples Sum05
RRipplesipples Fall 2005 in the Grande Ronde R I V E R S U N I T I N G N E I G H B O R S . Q U A R T E R L Y N E W S F R O M T H E G R A N D E R O N D E M O D E L W A T E R S H E D The first question one may ask is “Why is this Grande Ronde Basin fisheries managers feel it Catching necessary?” The second might be “What is an is imperative that the endemic fish stocks in the springspring endemic stock?” The answer to the second ques- Grande Ronde are maintained to preserve op- tion might help answer the first. A fish stock is tions for use of these stocks in future artificial defined as “a part of a fish population usually propagation programs and to rebuild the Grande with a particular migration pattern, specific Ronde chinook populations. chinookchinook spawning grounds, and subject to a distinct fish- ery.” An endemic stock is defined as “native to nake River spring chinook populations or limited to a specific region.” Maintaining a S have declined in both the Grande Ronde on the run native stock preserves the genetics of a popula- River Basin and in the entire Snake River Basin, by Lyle Kuchenbecker, GRMW tion that has evolved over many generations. A many to the point of extinction. The Grande native stock has unique characteristics that en- Ronde River Basin historically supported large he restoration of spring chinook in the able it to survive over the long term under con- populations of spring and fall chinook. -
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. -
Characterization of Groundwater in the Upper Grande Ronde Basin - 01/16/2019
Oregon Water Resources Department Characterization of Groundwater in the Upper Grande Ronde Basin - 01/16/2019 Characterization of Groundwater in the Upper Grande Ronde Basin NOTE: It is important to note that this information is for planning purposes only; any interpretation is done at the discretion of the planning group. If the group would like to use this information beyond its initially intended use as an informational resource to inform planning, OWRD requests that the group contact OWRD staff. Also, OWRD requests that staff be able to review any products that this information is used in – including those related to place-based planning- in order to ensure accurate use of the data and analysis. Introduction and Purpose This memo is intended to expand upon the background and data included in the Upper Grande Ronde (UGR) Place-Based Planning Step 2 and Step 3 reports regarding groundwater supply for current and future appropriation. The purpose of the memo is to introduce and document foundational groundwater concepts important to the Upper Grande Ronde basin and how those concepts, along with legal controls, impact current and future groundwater supply. For a broader exploration of groundwater, please review the USGS Publication, “Groundwater and Surface Water – A Single Resource” (Winter 1998). This memo is organized by the following sections: Understanding groundwater supply for appropriation Understanding capture What we know about the UGR groundwater resources – physical and legal controls Summary of gaps in groundwater data -
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. -
Grande Ronde Model Watershed
Grande Ronde Model Watershed 1114 J Avenue La Grande OR 97850 From ph 541-663-0570 fax 541-962-1585 Summer/Fall 2010 the Ripplesipples Board of Directors R Mike Hayward, Chairman Archives The Story of Lostine, Oregon Wallowa County Board of Commissioners in theGrande Ronde compiled by Heather Hall, GRMW Steve McClure, Vice Chairman . Union County Board of Commissioners R I V E R S U N I T I N G N E I G H B O R S Q U A R T E R L Y N E W S F R O M T H E G R A N D E R O N D E M O D E L W A T E R S H E D Anna Cavinato Eastern Oregon University Allen Childs Assessing Confederated Tribes of the Umatilla Indian Reservation Larry Christman, Public Interest Representative Catherine Ted Taylor, Public Interest Representative Norm Cimon, Conservationist Representative Larry Cribbs, Economic Development & Industry Creek: Representative Bruce Eddy, Fish and Wildlife Representative Daryl Hawes, Private Landowner Representative How does this ABOVE: Lostine area map Joe McCormack, Nez Perce Tribe Image by Mason Bailie, GRMW Lostine is a small, multi-faceted Pat Wortman, Private Forest & Landowners river flow? community located between Wallowa and and three lumber mills. Lostine became Enterprise in the Wallowa Mountain range. incorporated in 1903. Staff Members by Lyle Kuchenbecker RIGHT: Map of Lostine was established in 1878 by G.E. Today, with a population of roughly Jeff Oveson the Catherine 200+, many visitors stop and explore this Laughlin. Mr. -
ARMAND MINTHORN TAPE #1 December 16, 2005 Interviewed by Micheal L
ARMAND MINTHORN TAPE #1 December 16, 2005 Interviewed by Micheal L. Minthorn Transcribed by Micheal L. Minthorn Side A I: This is an oral history interview about Native American involvement in the Grande Ronde Valley in Union County with Armand Minthorn. It is uh, Friday, December 16th, 2005. All right, um, now naturally you and I both know that uh, uh, the Grande Ronde Valley has been a, a by-way at least if not a gathering ground for natives from the area for uh, hundreds of years. Um, that‟s what we‟re here to talk about today. Um, we‟re looking for stories for uh, history of natives that in particular have evolved out of Union County. And so I‟m here to talk to you about that. What can you tell me? AM: Well the, the history of the Grande Ronde Valley goes back at least 4,000 years. Not a couple hundred. There‟s archaeological sites in the Grande Ronde Valley that have been dated 2,500 and even up to 4, 000. La Grande, of course is known as “Kop koppa” which means place of cottonwoods. And even before the Treaty of 1855 was signed, um, La Grande or Kop koppa was the traditional gathering grounds for all of the tribes. Um, mainly because of the fish and because of the camas root. But they would gather in the Grande Ronde Valley and it was a traditional gathering ground. The last know traditional gathering in Kop koppa was prior to uh, the Treaty of 1855 where they gathered there to talk about the white people.