2000/01 DOQ Acquisition Dates (Pdf)
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Our Staff Compiled a List of Their Favorite Top 3 Local Spots for Each Category. We Hope That You Enjoy Them As Much As We Do!
Pronghorn Staff Top 3 Favorites Our staff compiled a list of their favorite top 3 local spots for each category. We hope that you enjoy them as much as we do! Breakfast Bike Trails 1. The Victorian Cafe 1. Phil’s Trail Complex 2. The Sparrow Bakery 2. Wanoga Trail Complex 3. McKay Cottage 3. Swampy Lakes Area Coffee: Hiking Trails 1. Looney Bean 1. Tumalo Falls 2. Backporch Coffee 2. Broken Top, No Name Lake 3. Thump Coffee 3. Elk Lake Elevated Dining: Non-sport Activities 1. The Blacksmith 1. Summer Concerts 2. Bos Taurus 2. Old Mill & Downtown Bend 3. Arianna 3. Cascade Lakes Highway Drive Casual Dining Outdoor Activities 1. Wild Rose 1. Deschutes River float 2. Spork 2. Mt. Bachelor 3. Brother Jon’s Alehouse 3. Fly fishing Local Breweries Must See 1. 10 Barrel Brewing Co. 1. Smith Rock State Park 2. Deschutes Brewery 2. 360 city view from Pilot Butte 3. Crux Fermentation Project 3. Tumalo Falls Contact our Concierge team for more information. 541.693.5311 | [email protected] “Why We Recommend” & More | Breakfast | Chow | Locally-sourced American cuisine served at an artful & comfortable eatery with a full bar & patio. Rotating menu based on region and sourcing. The Sparrow Bakery | Lively, family-friendly bakery for breakfast & lunch, in industrial-chic digs with a patio. Northwest Crossing location has a larger lunch menu. Eastside location is set in a historic building with a large patio. Famous for their ocean roll. Lemon Tree | Downtown, river-facing. Creative breakfast & lunch fare with craft cocktails, coffee & kombucha on tap plus, a gift shop. -
USGS USGS Geologic Investigations Series I-2569, Pamphlet
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I–2569 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF UPPER EOCENE TO HOLOCENE VOLCANIC AND RELATED ROCKS OF THE CASCADE RANGE, OREGON By David R. Sherrod and James G. Smith INTRODUCTION volcanic-hosted mineral deposits and even to potential volcanic hazards. Since 1979, Earth scientists of the Geothermal Historically, the regional geology of the Cascade Research Program of the U.S. Geological Survey have Range in Oregon has been interpreted through recon carried out multidisciplinary research in the Cascade naissance studies of large areas (for example, Diller, Range. The goal of this research is to understand 1898; Williams, 1916; Callaghan and Buddington, the geology, tectonics, and hydrology of the Cas cades in order to characterize and quantify geothermal 1938; Williams, 1942, 1957; Peck and others, 1964). Early studies were hampered by limited access, resource potential. A major goal of the program generally poor exposures, and thick forest cover, which is compilation of a comprehensive geologic map of flourishes in the 100 to 250 cm of annual precipi the entire Cascade Range that incorporates modern tation west of the range crest. In addition, age control field studies and that has a unified and internally con was scant and limited chiefly to fossil flora. Since sistent explanation. This map is one of three in a series that shows then, access has greatly improved via a well-devel- oped network of logging roads, and isotopic ages— Cascade Range geology by fitting published and mostly potassium-argon (K-Ar)—have gradually solved unpublished mapping into a province-wide scheme some major problems concerning timing of volcan of rock units distinguished by composition and age; ism and age of mapped units. -
Upper Deschutes River · ·Basin Prehistory
Upper Deschutes River · ·Basin Prehistory: A Preliminary Examination of Flaked Stone Tools and Debitage Michael W. Taggart 2002 ·~. ... .. " .. • '·:: ••h> ·';'"' •..,. •.• '11\•.. ...... :f~::.. ·:·. .. ii AN ABSTRACT OF THE THESIS OF Michael W. Taggart for the degree of Master of Arts in Interdisciplinary Studies in Anthropology. Anthropology. and Geography presented on April 19. 2002. Title: Upper Deschutes River Basin Prehistory: A Preliminary Examination of Flaked Stone Tools and Debitage. The prehistory of Central Oregon is explored through the examination of six archaeological sites and two isolated finds from the Upper Deschutes River Basin. Inquiry focuses on the land use, mobility, technological organization, and raw material procurement of the aboriginal inhabitants of the area. Archaeological data presented here are augmented with ethnographic accounts to inform interpretations. Eight stone tool assemblages and three debitage assemblages are analyzed in order to characterize technological organization. Diagnostic projectile points recovered from the study sites indicate the area was seasonally utilized prior to the eruption of ancient Mt. Mazama (>6,845 BP), and continuing until the Historic period (c. 1850). While there is evidence of human occupation at the study sites dating to between >7,000- 150 B.P., the range of activities and intensity of occupation varied. Source characterization analysis indicates that eight different Central Oregon obsidian sources are represented at the sites. Results of the lithic analysis are presented in light of past environmental and social phenomena including volcanic eruptions, climate change, and human population movements. Chapter One introduces the key questions that directed the inquiry and defines the theoretical perspective used. Chapter Two describes the modem and ancient environmental context of study area. -
Lower Sycan Watershed Analysis
Lower Sycan Watershed Analysis Fremont-Winema National Forest 2005 Lower Sycan River T33S,R12E,S23 Lower Sycan Watershed Analysis Table of Contents INTRODUCTION...................................................................................................................................... 1 General Watershed Area.....................................................................................................................................2 Geology and Soils.................................................................................................................................................5 Climate..................................................................................................................................................................6 STEP 1. CHARACTERIZATION OF THE WATERSHED ................................................................... 7 I. Watershed and Aquatics.................................................................................................................................7 Soils And Geomorphology...............................................................................................................................................10 Aquatic Habitat ................................................................................................................................................................10 II. Vegetation.....................................................................................................................................................12 -
Curt Teich Postcard Archives Towns and Cities
Curt Teich Postcard Archives Towns and Cities Alaska Aialik Bay Alaska Highway Alcan Highway Anchorage Arctic Auk Lake Cape Prince of Wales Castle Rock Chilkoot Pass Columbia Glacier Cook Inlet Copper River Cordova Curry Dawson Denali Denali National Park Eagle Fairbanks Five Finger Rapids Gastineau Channel Glacier Bay Glenn Highway Haines Harding Gateway Homer Hoonah Hurricane Gulch Inland Passage Inside Passage Isabel Pass Juneau Katmai National Monument Kenai Kenai Lake Kenai Peninsula Kenai River Kechikan Ketchikan Creek Kodiak Kodiak Island Kotzebue Lake Atlin Lake Bennett Latouche Lynn Canal Matanuska Valley McKinley Park Mendenhall Glacier Miles Canyon Montgomery Mount Blackburn Mount Dewey Mount McKinley Mount McKinley Park Mount O’Neal Mount Sanford Muir Glacier Nome North Slope Noyes Island Nushagak Opelika Palmer Petersburg Pribilof Island Resurrection Bay Richardson Highway Rocy Point St. Michael Sawtooth Mountain Sentinal Island Seward Sitka Sitka National Park Skagway Southeastern Alaska Stikine Rier Sulzer Summit Swift Current Taku Glacier Taku Inlet Taku Lodge Tanana Tanana River Tok Tunnel Mountain Valdez White Pass Whitehorse Wrangell Wrangell Narrow Yukon Yukon River General Views—no specific location Alabama Albany Albertville Alexander City Andalusia Anniston Ashford Athens Attalla Auburn Batesville Bessemer Birmingham Blue Lake Blue Springs Boaz Bobler’s Creek Boyles Brewton Bridgeport Camden Camp Hill Camp Rucker Carbon Hill Castleberry Centerville Centre Chapman Chattahoochee Valley Cheaha State Park Choctaw County -
DOGAMI Open-File Report O-92-09, Preliminary Geologic Map of the Jordan Craters South Quadrangle, Malheur County, Oregon
OPEN-FILE REPORT 0-92-09 PRELIMINARY GEOLOGIC MAP OF THE JORDAN CRATERS SOUTH QUADRANGLE MALHEUR COUNTY, OREGON By M. L. Ferns, and N. S. MacLeod Oregon Department of Geology and Mineral Industries This unpublished Open-File Report has not been reviewed and may not meet all Oregon Department of Geology and Mineral Industries' standards. Field work conducted in 1990/1991 Map Scale: 1:24,000 Funding Statement: Funded jointly by the Oregon Department of Geology and Mineral Industries, the Oregon State Lottery, and the U. S. Geological Survey COGEOMAP Program as part of a cooperative effort to map the west half of the lo by 2O Boise sheet, eastern Oregon. Jordan Craters South A distinctive, densely-welded, high-silica rhyolite ashflow tuff (Ttlg?) comprises the oldest unit exposed in the Jordan Craters South quadrangle. The ashflow is characterized by high silica and low alumina abundance5 and is correlative with tuffs mapped by Plumley (1984) as Leslie Gulch Tuff in The Hole in the Ground quadrangle to the northwest. If his correlation is correct, Ttlg? is part of the outflow sheet erupted during formation of the Mahogany Mountain caldera tn the northeast. The ashflow is overlain by tuffaceous siltstones (Tsts) and aphyric platy andesite flows (Tmv). Tilted fault blocks comprised of all three units from steptoes around which younger basalts (Tbdb, Tbtm, QTb, Qbcb, Qbrb, and Qbjc) have flowed. The youngest of these (Qbjc) erupted at about 3,000 years ago from a small vent north of the quadrangle at Jordan Crater. The surface of the Qbjc flow is free of wind- blown silt and soil and contains many fragile surface features that are characteristic of very young basalt flows. -
Notes from the Desk of the Drc's Executive Director
Summer 2011 VOLUME 5 NUMBER 2 NEWSLETTER OF THE DESCHUTES RIVER CONSERVANCY The mission of the DRC: To restore streamflow and improve water quality in the Deschutes Basin. MARISA CHAPPELL HOSSICK The DRC is beginning to successfully navigate the serpentine nature of water to restore flows to the lower Crooked River while helping North Unit irrigators maintain a viable agricultural economy on the plateaus above. NOTES FROM THE DESK OF THE DRC’S EXECUTIVE DIRECTOR, TOD HEISLER Making a Difference by Working Together sults on Whychus Creek, Lake Creek and districts. The net result will be 50 cfs Here at the Deschutes River Conservancy the Crooked River. In four short years of restored streamflows in the Crooked (DRC) we are living proof that when The Deschutes Collaborative imple- River, $300,000 pumping cost savings people of differing views are brought to mented nearly $20 million dollars of for NUID, improved irrigation infra- a table where the expectation is coopera- integrated projects where they are needed structure, and a more reliable supply tion and forging consensus, significant most for salmonid reintroduction. The of water for commercial farmers. This results achieved include 15 cubic feet per long-lasting results can be achieved in model project would not be possible second (cfs) of streamflow restored, six relatively short timeframes. We know without the cooperation of many part- fish passage barriers eliminated, three this because we are coming off another ners including state and federal agen- fantastic year of results on Whychus miles of stream protected from develop- cies, several irrigation districts, Portland Creek and have laid the groundwork for ment, and five miles of habitat restored. -
MINERAL RESOURCES of the JORDAN CRATERS WILDERNESS STUDY AREA, MALHEUR COUNTY, OREGON By
DEPARTMENT OF THE INTERIOR UNTIED STATES GEOLOGICAL SURVEY MINERAL RESOURCES OF THE JORDAN CRATERS WILDERNESS STUDY AREA, MALHEUR COUNTY, OREGON By J.P. Calzia1, Susan Hubbard-Sharpless2, R.L. Turner3, Andrew Griscorn1, and D.L. Sawatzky3 U.S. Geological Survey and J.M. Linne3 U.S. Bureau of Mines U.S. Geological Survey Open-File Report 88-572 Prepared by the U.S. Geological Survey and the U.S. Bureau of Mines for the U.S. Bureau of Land Management This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey. 1 - Menlo Park, CA 94025 2Blacksburg, VA 24060 3Spokane, WA 99202 1988 STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Area The Federal Land Policy and Management Act (Public Law 94-579, October 21,1976) requires the U.S. Geological Survey and the U.S. Bureau of Mines to conduct mineral surveys on certain areas to determine the mineral values, if any, that may be present Results must be made available to the public and be submitted to the President and the Congress. This report presents the results of a mineral survey of the Jordan Craters Wilderness Study Area (OR-003-128), Malheur County, Oregon. CONTENTS Summary 1 Abstract 1 Character and setting 1 Identified mineral resources and mineral resource potential 1 Introduction 1 Location and physiography 1 Previous studies 3 Present investigations 3 Appraisal of identified resources 3 Assessment of mineral resource potential 3 Geology 3 Geochemistry 4 Geophysics 4 Mineral resource potential 5 References cited 6 Appendixes 8 Definition of levels of mineral resource potential and certainty of assessment 9 Resource/reserve classification 10 Geologic time chart 11 FIGURE 1. -
2.2 State Risk Assessment
Chapter 2: RISK ASSESSMENT | State Risk Assessment | Cultural Resources Summary » Wildfire 2.2 State Risk Assessment Requirement: 44 CFR §201.4(c)(2)(i): The risk assessment shall include… (i) An overview of the type and location of all natural hazards that can affect the State, including information on previous occurrences of hazard events, as well as the probability of future hazard events, using maps where appropriate; The spatial distribution of the facilities within hazard zones is not easily viewed on a statewide map. Therefore, maps depicting hazard zones and facilities within those zones have only been created at the regional scale. Those maps can be found in section 2.3, Regional Risk Assessments. Oregon Natural Hazards Mitigation Plan | September 2020 163 Chapter 2: RISK ASSESSMENT | State Risk Assessment | Coastal Hazards Summary » Wildfire 2.2.1 Coastal Hazards The Pacific Northwest (PNW) coast of Figure 2-29. Erosion at The Capes Oregon is without doubt one of the most Condominiums, Oceanside, Oregon dynamic coastal landscapes in North America, evident by its long sandy beaches, sheer coastal cliffs, dramatic headlands and vistas, and ultimately the power of the Pacific Ocean that serves to erode and change the shape of the coast. It is these qualities along with its various natural resources that have drawn people to live along its narrow shores. However, coastal communities are increasingly under threat from a variety of natural hazards that all come together along the coastal strip. These include wave-induced coastal erosion (both short and long term), wave runup and overtopping (wave-induced flood hazards), inundation Notes: The Capes, a multi-million dollar condominium of homes by wind-blown sand, coastal complex constructed on an old Holocene dune field landslides, earthquakes, and potentially adjacent to Oceanside. -
Comprehensive Plan
Deschutes County Transportation System Plan 2010 - 2030 Adopted by Ordinance 2012-005 August 6, 2012 By The Deschutes County Board of Commissioners EXHIBIT C ORDINANCE 2012-005 Page 1 of 268 TABLE OF CONTENTS Executive Summary ...................................................................................................... 10 Chapter One Introduction ...................................................................................................................................30 1.1 Geographic Setting .......................................................................................................30 1.2 Transportation Planning ..............................................................................................31 Goal 12 .....................................................................................................................31 Transportation Planning Rule (TPR) ..................................................................31 TPR Requirements for Deschutes County ......................................................33 1.3 Major Changes Since the Adoption of the 1998 Plan ...........................................35 Regional Growth and Destination Resorts ......................................................35 Urban Growth and County Coordination .......................................................36 Public Transportation ...........................................................................................36 Financial Impacts ....................................................................................................37 -
History of the National Forest
HISTORY OF THE FREMONT NATIONAL FOREST O Melva M. Bach. O Fremont National Forest Lakeview, Oregon 1981 CAPTAtN JOHN C. FRENONT FOREWORD Gifford Pinchot once said, "The Forest Service is the best organization in the government because of the people in it". In my opinion, the out-door-loving S persons who choose their life work in the Forest Service and other conservation agencies are among the greatest Perhaps this is because these devoted people are more interested in helping to wisely use and perpetuate our natural resources rather than to exploit them. The8emen and women employees of the Forest Service are loyal, dedicated, and hard-working persons They work many hours of unpaid overtime to get the job done They are unselfish, giving a great deal of their own time and effort to community activities, such as the Boy Scouts, Camp Fire Girls, 4-s, United Fund, Rotary, Lions, and other service organizations. The wives of these men are exceptional and fine women who do their part in community af fairs They snow that housing and living conditions in the Forest Service are sometimes undesirable and in isolated places, but they cheerfully accept them It has been very pleasant working for and with the great number of persons who have been on this forest I have appreciated this lengthy opportunity to know and make friends with some very fine people, and thank them for their help and pleasant associations One reason for this long opportunity was a letter I received from MrShirley Buck of the Regional Office when I started to work in Lakeview e said "It is hoped you will stay a considerable length of time" I thought he meant it. -
Oregon's Owyhee Canyonlands
Oregon’s Owyhee Canyonlands Protecting Our Desert Heritage A Citizens Guide to the Wild Owyhee Canyonlands Three Fingers Butte, proposed Wilderness in the Lower Owyhee Canyonlands. Photo: © Mark W. Lisk 2 oregon’s owyhee canyonlands: protecting oregon’s desert heritage At 1.9 million acres, the Owyhee Canyonlands represents one of the largest conservation opportunities in the United States. Welcome to Oregon’s Owyhee Canyonlands—the center of the sagebrush sea and iconic landscape of the arid West. This remote corner of Southeast Oregon calls to those seeking solitude, unconfined space and a self-reliant way of life. Come raft the Wild & Scenic Owyhee River; hunt big game and upland birds; and walk dry streambeds surrounded by geologic formations from another world. We live and visit here because it is truly unique. owyhee canyonlands campaign 3 Greeley Flat–Owyhee Breaks Wilderness Study Area. Photo © Mark W. Lisk The Oregon Owyhee Canyonlands Campaign is working to protect one of the most expansive and dramatic landscapes in the West, featuring rare wildlife, pristine waterways and incredible outdoor recreational opportunities. Stretching from the mountain ranges of the Great Basin to fertile expanses of the Snake River Plain, the Owyhee Desert ecosystem encompasses nearly 9 million acres across three states. Local residents refer to it as ION country, since the Canyonlands lie at the confluence of Idaho, Oregon and Nevada. The name Seventeen Owyhee hearkens back to a time before state lines were drawn, when three Hawaiian trappers were contiguous Wilderness Study killed by local residents. An archaic spelling of their island home (oh-WYE-hee) became the name of this Areas, spanning landscape of deep riverine canyons and sagebrush sea.