Appendix a – Hydrology

Total Page:16

File Type:pdf, Size:1020Kb

Appendix a – Hydrology APPENDIX A – HYDROLOGY HYDROLOGY R EPORT C ATHE R INE C REEK T R IB UTAR Y A SSESSMENT – G R ANDE R ONDE R IVE R B AS IN Tributary Habitat Program, Oregon U.S. Department of the Interior Bureau of Reclamation Pacific Northwest Region Geology and Fluvial Analysis Group Boise, Idaho February 2012 U.S. DEPARTMENT OF THE INTERIOR Protecting America's Great Outdoors and Powering Our Future The U.S. Department of the Interior protects America's natural resources and heritage, honors our cultures and tribal communities, and supplies the energy to power our future. MISSION OF THE BUREAU OF RECLAMATION The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound manner in the interest of the American public. Cover Photograph: View looking east (downstream) along Catherine Creek, Reach 2 at river mile 26.0, in the Cove area, Mt. Fanny (upper left) and Phys Point (upper right) can be seen in the background. Catherine Creek Tributary Assessment- Grande Ronde River Basin-Tributary Habitat Program, Oregon – July 29, 2010. TABLE OF CONTENTS 1. Summary ................................................................................................. 1 2. Introduction ............................................................................................ 1 2.1 Purpose .................................................................................................................... 1 2.2 Physical Setting and Location ................................................................................. 2 2.2.1 Climate .................................................................................................... 10 3. Methods ................................................................................................. 10 3.1 Hydrologic Analysis ............................................................................................. 10 3.1.1 Stream Gages .......................................................................................... 10 3.1.2 Flood Frequency Analyses ..................................................................... 15 3.1.3 Significant Tributary Hydrology ............................................................ 17 3.1.4 Climate Analysis ..................................................................................... 17 4. Historical Conditions ............................................................................. 19 4.1 Historic Changes ................................................................................................... 22 5. Present Conditions ................................................................................ 23 5.1 Hydrologic Results ................................................................................................ 27 5.1.1 Mean Annual Hydrograph ...................................................................... 27 5.1.2 Exceedance Flows .................................................................................. 29 5.1.3 Peak Flow Events ................................................................................... 31 5.1.4 Low Flows .............................................................................................. 33 5.2 Diversion Dams and Inter-basin Transfers ........................................................... 34 5.3 Reclamation Stream Gages ................................................................................... 35 5.4 Climate Results and Climate Change .................................................................... 36 6. Discussion ............................................................................................. 37 7. References ............................................................................................. 39 8. Geospatial Data Source and Description .............................................. 41 List of Figures Figure 1. Catherine Creek watershed with the Tributary Assessment study area identified to encompass the lower 55-miles of Catherine Creek. ............................................ 3 Catherine Creek Tributary Assessment – Hydrology i TABLE OF CONTENTS (CONTINUED) Figure 2. Grande Ronde River and Catherine Creek watersheds. .......................................... 5 Figure 3. Catherine Creek watershed and smaller tributaries, Catherine Creek near Union gage, including Rhinehart Gap. ............................................................................... 7 Figure 4. Springs and creeks draining to reach 1 of Catherine Creek. ................................... 9 Figure 5. Stream gages in the Catherine Creek area. Reclamation gages were installed in 2010. ...................................................................................................................... 11 Figure 6. Catherine Creek watershed/PRISM data – average annual precipitation in the Catherine Creek watershed. .................................................................................. 14 Figure 7. Climate stations in or near the Catherine Creek watershed. ................................. 18 Figure 8. The Grande Ronde Valley endured a large flood in the spring of 1894. The top right picture shows downtown La Grande, Oregon, on April 1st. Oregon State Planning Board Records, Oregon State Planning Board Photograph Box, Grande Ronde Flood Photographs, OPB0002. ..................................................... 22 Figure 9. Land cover classes in the Catherine Creek watershed using the National Land Cover Database (NLCD) (2006). .......................................................................... 25 Figure 10. Estimated mean annual hydrograph (based on daily data and the 50 percent probability exceedance) for Catherine Creek and Grande Ronde River at their confluence with Chinook salmon lifestage usage. Grande Ronde River is estimated using data combined from two USGS gages, Grande Ronde at La Grande (13319000) and Grande Ronde at Perry (13318960). Catherine Creek is estimated from the Catherine Creek near Union gage (13320000). Note – data used to develop Catherine Creek is above most major diversions and does not properly reflect low summer flows which may be zero during the irrigation season. ................................................................................................................... 28 Figure 11. Estimated mean annual hydrograph (based on daily data and the 50 percent probability exceedance) for Catherine Creek with Chinook salmon lifestage usage. Two stream gaging stations are shown, Catherine Creek near Union gage and Catherine Creek at Union gage. Catherine Creek near Union is above most major diversions while the “near Union” stream gage includes substantial diversions. ............................................................................................................. 28 Figure 12. Estimated mean daily flow percent exceedance values for Catherine Creek at the confluence with the Grande Ronde River. Note – the data used to extrapolate this graph are from the Catherine Creek near Union (13320000) stream gage and the data do not account for all water withdrawals, and therefore, overestimate July through October flow. The 50 percent value represents an average annual hydrograph. ............................................................ 30 Figure 13. Estimated mean daily flow percent exceedance values for the Grande Ronde River at Rhinehart Gap. Note – the data used to extrapolate this graphy are from upstream gages (Catherine Creek near Union [13320000] and Grande ii Catherine Creek Tributary Assessment – Hydrology TABLE OF CONTENTS (CONTINUED) Ronde near Perry [13318960]), and the data do not account for all water withdrawals, and therefore, overestimate July through October flows. The 50 percent value represents an average annual hydrograph. ...................................... 30 List of Tables Table 1. Active and discontinued stream gages in the assessment area indicating the type of data available and the range of years the gage was active. (Note – Data may not be continuous; peak data refers to the annual maximum instantaneous discharge; and years are calendar years). .............................................................. 12 Table 2. Watershed characteristics for stream gages. ......................................................... 12 Table 3. Reclamation stream gages installed in 2010. All stream gages measure water stage. The Grande Ronde River at Pierce and Rhinehart Lane measure air temperature while all others measure water temperature. ..................................... 15 Table 4. Peak flow regression equations for northeastern Oregon (OWRD 2006). Area is in square miles and discharge is in cfs. ............................................................. 16 Table 5. Documented historic floods prior to stream gaging (1911) in the Grande Ronde Valley. ................................................................................................................... 21 Table 6. Land cover proportions using NLCD (2006) in the Catherine Creek watershed. 26 Table 7. Annual peak discharges for all historic gages in the study area specified as return intervals. ..................................................................................................... 32 Table 8. Peak flow data for major tributaries and at flow change locations along Catherine Creek. Data extrapolated from Catherine Creek near Union stream gage. Peak flows along Catherine Creek were not adjusted for timing of hydrographs
Recommended publications
  • 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 ...........................................
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Union County Farm Loop Map 2020 Digital
    Copy of Union County Farm Loop 2020 2020 Farm loop signup spreadsheet final.xlsx Avella Orchard Evergreen Family Farm Copy of Union County Farm Loop 2020 Mt Emily Farmstead Elgin Copy of UnionNorthwest County Skillet Company Farm & Loop2020 Farm 2020 loop signup Homestead Springs Farm spreadsheet final.xlsx Union County Farm Loop Mint Condition 2020 Farm loop signup Avella Orchard Farm and Ranch Visitor Etiquette Pick 'n' Patch Watch for the “Open” sign or call first. spreadsheet final.xlsx Evergreen Family Farm Read and obey signs. Listen carefully to instructions. Avella Orchard The Plantworks Mt Emily Farmstead Closely supervise children. Evergreen Family Farm Folly Farm Ask before taking pets out of your car. Summerville Stay out of buildings and off equipment. Mt Emily Farmstead Cove Honey Northwest Skillet Company & Be careful not to step on crops. We welcome your questions! Almosta Farm at Cove Homestead Springs Farm Northwest Skillet Company & Nella Mae's Farm Homestead Springs Farm Mint Condition Imbler Apple Spring Micro Farm Mint Condition Pick 'n' Patch Ascension Camp Pick 'n' Patch The Plantworks The Plantworks Grande Ronde Dairy Folly Farm Folly Farm Hometown Hardware Wallowa Lake Highway Cove Honey Cove Honey Almosta Farm at Cove Almosta Farm at CoveBuffalo Peak Land & Livestock Nella Mae's Farm Union County Museum Nella Mae's Farm 20 Apple Spring Micro Farm Apple Spring Micro Farm Ascension Camp Cove map is enlarged. The Cottage at Union Ascension Camp Buy fresh produce. Meet the growers. Learn about our agricultural heritage. Grande Ronde Dairy Meadows Lower Cove Road The Union County Farm Loop is a perfect way to enjoy the scenery and explore some of the abundant farms and Grande Island Ronde City Dairy ranches that are the heart and soul of the Grande Ronde Valley.
    [Show full text]
  • Riparian Vegetation of the Grande Ronde River by Joseph A
    Riparian Vegetation of the Grande Ronde River by Joseph A. E. Stewart ABSTRACT Riparian Vegetation exists in a unique environment characterized by frequent disturbance, spatial and temporal environmental heterogeneity, and abundant water supply. Riparian areas are important due to their disproportionately strong influences on both in stream and terrestrial ecosystems. Because of the importance of riparian areas, scientists and land managers are interested in understanding their dynamics. Many conceptual frameworks exist for examining longitudinal changes in biological function and diversity along rivers. One of these frameworks, the River Continuum Concept (RCC), postulates that longitudinal sections of river show gradients in the physical environmental factors that determine biotic communities. Another conceptual framework that can be applied to river systems is the intermediate disturbance hypothesis, which hypothesizes that the greatest levels of biodiversity will be found at intermediate levels of disturbance. Due to confounding factors, these conceptual frameworks, particularly the RCC, may not be particularly accurate generalizations of the riparian vegetation of the Grande Ronde River. INTRODUCTION The term Riparian comes from the Latin word Riparius, meaning “of or pertaining to the bank of a river” (Webster’s Revised Unabridged Dictionary). Our word, riparian, refers to biotic communities that occupy the banks of rivers and streams. Riparian areas are the transition zone between the terrestrial environment and rivers. Riparian areas are characterized by elevated levels of vegetative productivity, high biodiversity and disproportionately strong influences on the surrounding environment (Junk et al. 1989, Niaman et al. 1993, Pollock et al. 1998). This paper will discuss riparian vegetation and distribution of riparian vegetation on the Grande Ronde River in northeast Oregon and southeast Washington.
    [Show full text]
  • CHAPTER 10 New Perspectives on The
    CHAPTER 10 New Perspectives on the Stockhoff Quarry: Toolstone Procurement at a Quarry Complex in the Blue Mountains of Northeastern Oregon Nicholas Smits Archaeological Investigations Northwest, Inc. ([email protected]) Sara J. Davis Historical Research Associates, Inc. ([email protected]) Introduction The term “Stockhoff basalt” is familiar to many archaeologists who work in the Pacific Northwest. One of the largest recorded archaeological sites in Oregon, the Stockhoff Quarry site (35UN52) encompasses over 3,400 acres of land on the western flank of Craig Mountain, located about 16 km southeast of La Grande in Union County (Figures 10-1 and 10-2). The Stockhoff Quarry is named for Gene Stockhoff, who owned the land in 1955 when Alan Bryan and Donald Tuohy initiated the first archaeological investigations at the site. Working in advance of construction of a natural gas pipeline, Bryan and Tuohy (1960:489-490) conducted limited testing within the pipeline right- of-way, where they found stone tools and hundreds of flakes of “fine-grained glassy basalt.” The dark gray to black, fine-grained volcanic (FGV) toolstone local to the Craig Mountain vicinity has since been known colloquially as “Stockhoff basalt” for ease of reference, even as our knowledge of the compositional variability of FGV materials in archaeological contexts has increased over the last two decades (e.g., Bakewell 1993, 1996, 2005; Bakewell and Irving 1994). Accordingly, terms such as “FGV” and “vitrophyre,” which have been proposed as alternatives to the catchall term “basalt,” will be used here for the sake of accuracy. Figure 10-1. General study area showing Craig In 2009 and 2010, archaeologists employed by Mountain in relation to prominent features of Archaeological Investigations Northwest, Inc.
    [Show full text]
  • Download This
    NFS Form 10-900 (342) OMB No. 1024-0018 Expires 10-31-87 United States Department of the Interior National Park Service For NFS us* only National Register off Historic Places received MAY 2 7 1987 Inventory—Nomination Form date entered An o See instructions in How to Complete National Register Forms Type all entries—complete applicable sections_______________ 1. Name historic Sumpter Valley Railway Historic District Number of contributing features: 18 (main line roadbed; 4 spur roadbeds, and or common Same 6 station sites, 2 mill sites, 4 items or Historic rolling stock, l water tower Number of noncontributing features: 2 Historic right-of-way of the Sumpter Valley Railway and street & number its, 5JaJ?r . sP"rs though the Blue Mountains between B and Prairie City in Baker and Grant Counties 8 Oregon fo r pub,lcatlon (Nominated area does not start or end at Baker and Prairie City) city, town Sumpter ^/Avicinity of Second Congressional Baker 001 state Oregon code 41 county Grant code 023 3. Classification Category Ownership Status Present Use X district public occupied X agriculture museum building(s) private X unoccupied commercial _«_park __ structure x both work in progress educational private residence site Public Acquisition Accessible entertainment religious object N ' 4n process X yes: restricted government scientific _N/4jeing considered "noyes: unrestricted industrial transportation military _JL other: recreation name see continuation sheets, item 4 street & number N/A city, town N/ vicinity of state 5. Location off Legal Description courthouse, registry of deeds, etc. Baker County Grant County street & number Courthouse Courthouse 97820 city, town Baker, OR 97814 Canyon City, OR state 6.
    [Show full text]