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Burnt River Water Temperature Study Commitee Final Report
BURNT RIVER WATER TEMPERATURE STUDY STEERING COMMITTEE FINAL REPORT Prepared for the Burnt River Steering Committee by David Duncan and Associates Boise, Idaho April 2002 TABLE OF CONTENTS INTRODUCTION ............................................................................................................................ 1 Study Description ...................................................................................................................... 1 Study Area ................................................................................................................................. 1 OBJECTIVE 1: FACTORS CONTRIBUTING TO STREAM TEMPERATURES ...................... 2 Baseline Temperatures............................................................................................................... 2 Upper Watersheds .............................................................................................................. 2 Lower Watersheds .............................................................................................................. 2 How Does Heat Energy Enter and Leave a Stream? ................................................................. 3 Radiation.................................................................................................................................... 5 Atmospheric Radiation....................................................................................................... 7 Radiation from Riparian Vegetation and Topographic Features....................................... -
Baker County Community Sensitivity and Resilience
Baker County Community Sensitivity and Resilience This section documents the community’s sensitivity factors, or those community assets and characteristics that may be impacted by natural hazards, (e.g., special populations, economic factors, and historic and cultural resources). It also identifies the community’s resilience factors, or the community’s ability to manage risk and adapt to hazard event impacts (e.g., governmental structure, agency missions and directives, and plans, policies, and programs). The information in this section represents a snapshot in time of the current sensitivity and resilience factors in the community when the plan was developed. The information documented below, along with the findings of the risk assessment, should be used as the local level rationale for the risk reduction actions identified in Section 6 – Mission, Goals, and Action Items. The identification of actions that reduce a community’s sensitivity and increase its resilience assists in reducing the community’s overall risk, or the area of overlap in Figure G.1 below. Figure G.1 Understanding Risk Source: Oregon Natural Hazards Workgroup, 2006. Northeast Oregon Natural Hazard Mitigation Plan Page G-1 Community Sensitivity Factors The following table documents the key community sensitivity factors in Baker County. Population • Baker County has eight distinct geographic populations, as well as eight unincorporated communities. Incorporated cities are: Baker City, Greenhorn, Haines, Halfway, Huntington, Richland, Sumpter, and Unity. Unincorporated communities include: Durkee, Hereford, Pinetown, McEwen, Keating, Sparta, New Bridge, and Oxbow. Communities are geographically dispersed with little communication or interconnection. If communities need to be warned of an event, or require disaster assistance, distance and dispersal will be communication barriers. -
Or Wilderness-Like Areas, but Instead Declassified Previously Protected Wildlands with High Timber Value
48 OREGON WILD A Brief Political History of Oregon’s Wilderness Protections Government protection should be thrown around every wild grove and forest on the Although the Forest Service pioneered the concept of wilderness protection in the mountains, as it is around every private orchard, and trees in public parks. To say 1920s and 1930s, by the late 1940s and 1950s, it was methodically undoing whatever nothing of their values as fountains of timber, they are worth infinitely more than all good it had done earlier by declassifying administrative wilderness areas that contained the gardens and parks of town. any commercial timber. —John Muir1 Just prior to the end of its second term, and after receiving over a million public comments in support of protecting national forest roadless areas, the Clinton Administration promulgated a regulation (a.k.a. “the Roadless Rule”) to protect the Inadequacies of Administrative remaining unprotected wildlands (greater than 5,000 acres in size) in the National Forest System from road building and logging. At the time, Clinton’s Forest Service Protections chief Mike Dombeck asked rhetorically: here is “government protection,” and then there is government protection. Mere public ownership — especially if managed by the Bureau of Is it worth one-quarter of 1 percent of our nation’s timber supply or a fraction of a Land Management — affords land little real or permanent protection. fraction of our oil and gas to protect 58.5 million acres of wild and unfragmented land T National forests enjoy somewhat more protection than BLM lands, but in perpetuity?2 to fully protect, conserve and restore federal forests often requires a combination of Wilderness designation and additional appropriate congressional Dombeck’s remarks echoed those of a Forest Service scientist from an earlier era. -
MINING in BAKER COUNTY, 1861 to 1959* by Norman S
Vol.21, No.3 THE ORE.- BIN 21 March 1959 Portland, Oregon STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Head Office: 1069 State Office Bldg., Portland I, Oregon Telephone: CApitol 6-2161, Ext. 488 Field Offices 2033 First Street 239 S. E. "H"Street Baker Grants Pass *************************** MINING IN BAKER COUNTY, 1861 to 1959* By Norman S. Wagner** Introduction Baker County mining began with the discovery of gold in 'Griffin Gulch in 1861. This and the develop ment which followed at Auburn represent gold mining at its historic best. Since 1861, much water has flowed down the sluice boxes with respect to mineral resource development within the county. As a result, the dis covery story is left for historians to tell, and the following paragraphs are devoted to the high points of the many kinds of mining endeavors that occurred in Baker County between 1861 and 1959. Hydraulic and sluicing operations All of the earlier placer operations have one thing in common with Griffin Gulch and Auburn. This is that they were carried out by means of ground sluicing and hydraul icking, using generous amounts of hand labor. These means of handl ing placer ground continued in exclusive use throughout the first forty years of Baker County mining history. It wasn't until the present century that the more familiar bucket-line dredges and other kinds of mechanized digging and washing plants made their appearance. Even yet the old methods are still employed on a small scale in circumstances where ground conditions permit. The Rye Valley placers on Dixie Creek represent a notable example of an early discovery made shortly after 1862. -
Bull Trout Recovery Plan App Introduction
Chapter 13 - Hells Canyon INTRODUCTION Recovery Unit Designation The Hells Canyon Complex Recovery Unit is 1 of 22 recovery units designated for bull trout in the Columbia River basin (Figure 1). The Hells Canyon Complex Recovery Unit includes basins in Idaho and Oregon, draining into the Snake River and its associated reservoirs from below the confluence of the Weiser River downstream to Hells Canyon Dam. This recovery unit contains three Snake River reservoirs, Hells Canyon, Oxbow, and Brownlee. Major watersheds are the Pine Creek, Powder River, and Burnt River drainages in Oregon, and the Indian Creek and Wildhorse River drainages in Idaho. Inclusion of bull trout in the Oregon tributaries (i.e., Pine Creek and Powder River) in one recovery unit is based in part on a single gene conservation unit (i.e., roughly the major drainages in Oregon inhabited by bull trout) recognized by the Figure 1. Bull trout recovery units in the United States. The Hells Canyon Complex Recovery Unit is highlighted. 1 Chapter 13 - Hells Canyon Oregon Department of Fish and Wildlife (Kostow 1995), which is supported by the genetic analysis conducted by Spruell and Allendorf (1997). Although the genetic composition of bull trout in the two tributaries in Idaho has not been extensively studied, the streams were included in the recovery unit due to their close proximity to the tributaries in Oregon containing bull trout, and the likelihood that bull trout from all tributaries were able to interact historically. Administratively, the Oregon Department of Fish and Wildlife established a working group to develop bull trout conservation strategies in Pine Creek, and the streams in Idaho were included in the Hells Canyon Key Watersheds in the Idaho Bull Trout Conservation Plan (Grunder 1999). -
North Burnt River Fuel & Forest Health Project
NORTH BURNT RIVER FUEL & FOREST HEALTH PROJECT Environmental Assessment # DOI-BLM-OR-V050-2009-015 Introduction: The Vale District Bureau of Land Management (BLM), Baker Resource Area proposes the treatment of approximately 700 acres of forested BLM-administered lands within the Ebell Creek, Alder Creek, Hill Creek and Deer Creek drainages. The legal description of the project area is as follows: T. 11 S., R. 41 E., Section 7: NW ¼ NE ¼, E ½ NE ¼; Section 8: W ½ SW ¼, SE ¼ SW ¼; Section 11: W ½ NW ¼; Section 14: NW ¼ NW ¼, SE ¼ SW ¼; Section 23: N ½ NE ¼ SE ¼ NE ¼; Section 24: S ½ NW ¼, S ½ NE ¼ and T. 11 S., R. 42 E., Section 17 N ½ SW ¼; Section 18 NE ¼ SE ¼; Section 19 S ½ NW ¼. The project objective is to apply a three-tiered approach (e.g., a combination of Commercial Thinning (CT), Precommercial Thinning (PCT), and Prescribed Burning) to reduce fire fuels and restoring forest health, which includes the reduction of ground, ladder, and crown fuels. Proposed Action: The Baker Field Office of the Vale District, BLM proposes to remove fuels and improve forest health in the North Burnt River Area on lands administered by the BLM. Type of Statement: Environmental Assessment (EA) Agency: Bureau of Land Management, Department of Interior For further information: Bureau of Land Management Baker Field Office 3285 11th St. Baker City, OR 97814 (541) 523-1339 E-Mail: [email protected] Contents Finding of No Significant Impact (FONSI) Introduction Chapter 1.0 Purpose of and Need for Action 1.1 Conformance with Existing Land Use Plans 1.1.a -
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. -
Vol. 23, No. the ORE.-BIN January 1961 STATE of OREGON Portland
THE ORE BIN Volume 23, 1961 Vol. 23, No. THE ORE.-BIN January 1961 STATE OF OREGON Portland, Oregon DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Head Office: 1069 State Office Bldg., Portland 1, Oregon Telephone: CApitol 6-2161, Ext. 488 State Governing Board Hollis M. Dole, Director William Kennedy, Chairman, Portland Harold Banta Baker Stoff Earl S. Mollard Riddle R. G. Bowen Geologist Field Offices R. E. Corcoran Geologist 2033 First Street, Boker L. L. Hoogland Assayer and Chemist N. S. Wagner, Field Geologist Rolph S. Mason Mining Engineer H. C. Brooks, Field Geologist T. C. Matthews Spectroscopist 239 S. E. "H" Street, Grants Pass V. C. Newton, Jr. Petroleum Engineer Len Ramp, Field Geologist H. G. Schlicker Geologist Norman Peterson, Field Geologist M. L. Steere Geologist * * * * * * * * * * * * * * * * * * OREGON MINERAL PRODUCTION IN 1960 By Ralph S. Mason* Oregon's mineral industry produced its second highest value of row minerals in 1960. Following a nation-wide economic trend during the year, the industry was off approximately $3 million from lost year's record-breaking high of $49.8 million, according to preliminary estimates mode by the U. S. Bureau of Mines. The heavy construction commodities, crushed stone and sand and grovel, reflected construction log and were responsible for most of the change from lost year. Metal mining, aside from nickel, was quiet. The state's only uronium mine and one of the two mercury producers shut down. Industrial mineral products showed both gains and losses as compared to the previous year. Cement production was up 12 percent while clays declined 15 percent and diatomite 3 percent. -
Detailed Descriptions of Mining Districts
CHAPTER VI. DE~l'AILED DESCRIPTIONS OF MINING DISTIUCTS (CONTINUED). VIRTUE DISTRICT. GENERAL l!~EATURES. The Virtue mining district, one of the ,oldest in eastern Oregon, is situated about 7 miles east of !Baker City, and extends for about 12 miles in a northwesterly direction, the width varying between 3 and 6 miles. It covers a region of low arid hills rising in the gi·eat bend of Powder River, and may be considered as the no.rthwesterly continua tion of the Lookout complex. The elevations range from 3,400 to 5,000 feet. The hills rise rather abruptly from Baker Valley and slope gently eastward toward the lower Powder River Valley. Most of the drainage is toward the latter. A rather remarkable feature within the hills is Virtue Flat, a desolate, sage-covered depression extending 8 miles east and west by 2 miles north and south. The water supply is very scant, the only :flowing stream being Ruckles Creek, practically outside of the district. GEOLOGY. The predominating roek of ,the northern part of the district is a lighter or darker greenish-gray dioritic rock of granular texture, which nearly always bears evidence of Rtrong crushing, but rarely of schis tosity. Frequently the rock is a veritable breccia, the diff~rent frag ments being eemented by seams of feldspar or zoisite. The feldspars are largely converted into a :flinty white mass resembling saussurite, and the hornblende seems uralitic. The microscope shows, in fact, that the rock is rather a saussuritic uralite-gabbro than a true diorite. This rock decomposes to a very light-colored dusty soil. -
Record of Late Pleistocene Glaciation and Deglaciation in the Southern Cascade Range
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by DigitalCommons@University of Nebraska University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 2004 Record of Late Pleistocene Glaciation and Deglaciation in the Southern Cascade Range. I. Petrological Evidence from Lacustrine Sediment in Upper Klamath Lake, Southern Oregon Richard L. Reynolds US Geological Survey Joseph G. Rosenbaum US Geological Survey Josh Rapp US Geological Survey Michael W. Kerwin US Geological Survey J. Platt Bradbury US Geological Survey See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Earth Sciences Commons Reynolds, Richard L.; Rosenbaum, Joseph G.; Rapp, Josh; Kerwin, Michael W.; Bradbury, J. Platt; Adam, David; and Colman, Steven, "Record of Late Pleistocene Glaciation and Deglaciation in the Southern Cascade Range. I. Petrological Evidence from Lacustrine Sediment in Upper Klamath Lake, Southern Oregon" (2004). USGS Staff -- Published Research. 255. https://digitalcommons.unl.edu/usgsstaffpub/255 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors Richard L. Reynolds, Joseph G. Rosenbaum, Josh Rapp, Michael W. Kerwin, J. Platt Bradbury, David Adam, and Steven Colman This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/ usgsstaffpub/255 Journal of Paleolimnology 31: 217–233, 2004. 217 # 2004 Kluwer Academic Publishers. -
Eastern Oregon Before the Oregon Trail: the First White Men in Oregon* by Gary Dielman
Eastern Oregon before the Oregon Trail: The First White men in Oregon* by Gary Dielman Last time I spoke to you, I brought lots of photos from the McCord Collection. This time I have no photos, but instead will paint a mental picture of this area before white men arrived. First we must use an eraser on the present picture. Erase the towns, the farms houses and outbuildings, the asphalt and dirt roads, and with them all the vehicles and every other modern convenience. And let's not forget to take out all the dams, so that the rivers once again run wild and salmon again spawn in the upper reaches of Powder River above Sumpter. Now that we have erased all evidence of modern civilization, let's look at our new picture of Baker Valley beginning in the foothills of the northwest corner on Pilcher Creek where, until a few moments ago, there was a dam and reservoir. Now it is restored to a large oblong grass-covered meadow with a little creek flowing thru it. It's summer time and although down in the valley it is hot, up here in the meadow it is cooler and the water runs fresher and there are camas roots in the meadow and huckleberries to gather on the surrounding slopes. And of course the deer and elk are nearby. That's probably why there is a small band of Indians camped here and why they have been coming here to spend the warm part of the year for thousands and thousands of years. -
Historical Snowdepth Comparison Along the Cascade Range This Compilation Is ©2002-2005 Amar Andalkar
Page 1 of 5 Historical Snowdepth Comparison along the Cascade Range This compilation is ©2002-2005 Amar Andalkar www.skimountaineer.com Snowdepths in inches for the listed period of record, measured at snow courses, snow stakes, and automated gauges Data provided by: throughout the length of the Cascade Range. Note that snowfall data is available for only a few of these sites. BCRFC British Columbia River Forecast Centre NWAC Northwest Weather & Avalanche Center NRCS Natural Resources Conservation Service WRCC Western Regional Climate Center Updated through the 2003-2004 season. Italicized numbers are estimated based on limited available data. CCSS California Cooperative Snow Surveys NPS National Park Service See the end of the chart for an explanation of the Depth and Variability classification codes. WBSR Whistler Blackcomb Ski Resort ECNCA Environment Canada National Climate Archive BRITISH COLUMBIA Jan 1 Feb 1 Mar 1 Apr 1 May 1 Depth Variab 350 Bridge Glacier, N of Mt Meager (4600 ft) 350 Tenquille Lake, E of Mt Meager (5500 ft) Bridge Glacier (Lower) Average 47 61 65 69 61 Avg Snowfall — L LV 300 300 4600 ft (15 miles north of Mt Meager) Minimum 32 48 40 47 43 Max Snowfall — 250 250 BCRFC, monthly, 1995–present Maximum 63 88 117 108 87 Max Depth 117 (1999) 200 200 This fairly new measurement site is located at the eastern end of the Lillooet Icefield, in the next drainage north of the Mount Meager 171 150 150 Volcanic Complex. Snowdepths are relatively low but quite consistent due to its northerly location and icefield margin microclimate.