DOCSLIB.ORG

Study Weekend, 2020

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Study Weekend, 2020 Washington Native Plant Society Study Weekend, 2020 Descriptions of Field Trips and Workshops Beginning with Saturday, June 6th Choosing from the weekend’s events: This year we have an exciting new opportunity: In addition to field trips, we are offering three half-day workshops designed to help our members advocate for native plants - one on Saturday and two on Sunday. They are in the list below and you can sign up for them just like you would sign up for field trips. So, if you sign up for a half day trip that is specifically marked, and you are returning to the Lazy F, you should be back in time for an afternoon’s advocacy workshop. Please note the start times for these workshops and keep in mind that they are typically two hour events. The botanical drawing workshop however is three to five hours depending on how long individual participants wish to stay. When deciding on a Sunday activity, keep in mind that many drivers may elect to go directly home without returning to the Lazy F. So, if you plan to ride with someone else to Study Weekend, be sure to speak with your driver about planning your trip home, and how it may affect the choice of the Sunday activity. Photo by Ben Legler Name of Workshop: 101: Advocacy; How to be WDNR LIDAR Aerial View of the Mounds an Advocate for Native Plants Leaders: Becky Chaney, WNPS Conservation Trip Title: 102: Mima Mounds, Umptanum Road Chair and Josh Morris, Seattle Audubon Trip Leader: Ed Lisowski Duration: 2 hours Duration: Half day, Saturday Beginning: 2:00 pm (Saturday) 3 miles Number of Participants: 60 Distance: Elevation gain: 300 feet Difficulty: easy Have you ever wondered what you can do Driving Time: 30 minutes personally to help protect Washington’s native Number of Participants: 12 plants? Where do you start? This workshop is for you! Becky and Josh provide an interactive, Note: This trip can be combined with the start-to-finish how-to for the WNPS native plant advocacy workshop 101. advocate, covering steps necessary to advocate individually and on behalf of WNPS. This The Manastash Mima mounds were workshop explores how to keep abreast of documented by CWU Geography professor threats to native plants and the opportunities to Martin Kaatz in 1959. LIDAR (light detection and protect them, complete and submit a WNPS ranging) is a remote sensing technology that Information Sheet, take action, and follow-up can be used to create topographic resolution on outcomes. We’ll also discuss the new WNPS especially useful for remote sensing of Mima policy on ‘direct action advocacy.’ This mounds. The WDNR LIDAR portal creates bare workshop is relevant for all WNPS members, earth and vegetation canopy views. regardless of your advocacy experience or specific advocacy interests. Roald Fryxell has noted distinctive plant communities in such areas: Artemisia tridentata /Agropyron spicatum association of Daubenmire is restricted to the more mesic mounds and the Artemisia rigida/Poa secunda association occurs on intermound areas with shallow soil and prolonged periods of drying. Expect to see shrub-steppe vegetation associated with the Mima mound field. Photo by Jane Ely Photo by Keyna Bugner Name of Workshop: 104: Botanical Drawing Trip Title: 103: Osborn Point Meadows Leader: Crystal Shin Trip Leader: Keyna Bugner Duration: 3 to 5 hours 9:00 am (Saturday) Duration: Half day, Saturday Beginning: Number of Participants: 11 Distance: about 2 miles Elevation gain: less than 200 feet Learn and practice the basics of botanical drawing. Difficulty: easy Botanical drawing requires careful observation, Driving Distance or Time: 1 hr., 10 min. measurement, attention to details, and Number of Participants: 12 understanding in some basic plant morphology. We Note: No restrooms, NW Forest Pass required. will learn and practice the unique requirements of botanical drawing and also learn about pencil drawing techniques. Botanical drawing can help you Note: This trip can be combined with the understand plants and develop eyes to see details. advocacy workshop 101. You can choose to draw a single leaf, a leaflet, a single flower head or a whole plant, depending on We will explore the meadows at Osborn Point which your drawing experiences and interests. All levels are is located on South Cle Elum Ridge in Kittitas County. welcome. Attendees may opt out at 2:00 PM or The plant list includes 163 species found along FS earlier in order to attend the advocacy workshop. road 3350 past Osborn Point to its junction with FS road 3352 near Taneum Point. Crystal Shin, A Botanical Artist and Natural Science Illustrator – Crystal studied botanical illustration at This area is the only known location of Lomatium Gage Academy of Art and the Center for Urban knokei. It is a narrowly endemic species of apparent Horticulture, and earned Scientific Illustration critical conservation concern on seasonally wet soils. Certificate from University of Washington. She We will also find species of Eriogonum, Penstemon as well as Sidalcea oregana var. oregana. worked as a primary illustrator on the second edition of “Flora of the Pacific Northwest” at the University Participants on this trip may be back in time for all or of Washington Herbarium from 2015 to 2018, part of the afternoon’s advocacy workshop. generating 882 new illustrations. She works in graphite, pen and ink, color pencils, and watercolor. Photo by Richard Droker Photo by Ben Legler Trip Title: 105: Camas Meadows Natural Area Trip Title: 106: Cowiche Canyon Lichen Walk SOLD OUT Trip Leader: Katherine Glew, Richard Droker Leader: David Wilderman, Joan Ponzetti Duration: Full Day, Saturday Duration: Full day, Saturday Length: 5-6 miles Distance: 3 miles Elevation gain: Minimal Elevation gain: 300 feet Difficulty: Easy Difficulty: Easy Number of Participants: 12 Note: Discover Pass needed Driving Distance or Time: 1 hour, 20 min. Number of Participants: 12 Cowiche Canyon Trail is a 5-6 mile out and back walk Driving Distance or Time: 1 ½ hours located near Tieton, Washington. The trail follows the Cowiche Creek with spectacular views of basalt The nearly 2000-acre Camas Meadows Natural Area cliffs. This area is a fabulous example of shrub- Preserve is located off of Hwy 97 between Blewett steppe landscape, made up of grasslands, sagebrush, Pass and Cashmere, Washington. The site is situated and oak woodlands in a geologically unique basin within the Wenatchee Our objective will be to admire and identify some of Mts. -- a floristically diverse part of the east the many species of lichens, foliose (leafy, including Cascades supporting a number of endemic plants. umbilicate) and crustose (crusty, almost 2- The flat floor of the basin has extensive areas of dimensional) forms, particularly those growing on seasonally wet meadows and aspen groves with basalt (mafic volcanic rock). In addition we will camas (Camassia quamash ssp. breviflora), Mule’s- discuss the ecological importance of lichens in ears (Wyethia amplexicaulis), bistort (Bistorta eastern Washington and their role in air quality. bistortoides), elk thistle (Cirsium scariosum), and many others. Surrounding slopes support mixed Crustose genera that we will be viewing conifer forest, riparian habitats, and rocky openings include Asplicillia, Caloplaca, and Lecanora. Foliose hosting a variety of interesting plants, such as genera will include: Cladonia, Leptogium, and mountain lady slipper (Cypripedium montanum) and Umbilicaria. See plant list at: Oregon anemone (Anemone oregana). Occurring https://www.wnps.org/plant- here are large populations of two locally-endemic lists/list?Cowiche_Canyon&County=Yakima&ListID=6 plant taxa - the Wenatchee Mts. checkermallow 59 (Sidalcea oregana var. calva) and Wenatchee larkspur (Delphinium viridescens). Photo by Ben Legler Trip Title: 107: Cowiche Canyon and Snow Mountain. Photo by Richard Droker Trip Leader: Terri Knoke Duration: Full day, Saturday Trip Title: 108: Giant Ripples on the Columbia Distance: 3.5 miles Trip Leader Clay Antieau, three Assistants Full day, Saturday Elevation gain: 100-200 feet Duration: Distance: Up to 3 miles Difficulty: Moderate Elevation gain: Minimal Number of Participants: 12 Difficulty: Easy to moderate Driving Distance or Time: 1 hour. Number of Participants: 12 1 hr., 15 min. We will drive from Lazy F Ranch, via I-84 and SR-12 Driving Distance or Time: West, to the upper Cowiche Canyon Trailhead on Note: EXTRA COST: $20/person at the ferry. Scenic Drive, in Yakima. Once there, we will meet Cy Philbrick, Education and Community Outreach West Bar is a gravel point bar on the Columbia River person for Cowiche Canyon Conservancy. He’ll give along Lake Wanapum near Trinidad. Unusual, huge us a brief overview of the 35 year history of how the current ripples were created by the last of the conservancy was formed, what they’ve achieved catastrophic Bretz floods from Glacial Lake Missoula. from grassroots advocacy and what new projects lay This landform is considered the largest and best ahead. I will talk about the importance of example of giant current ripples on Earth and has conductivity for migration and how CCC lands are not been fully explored botanically. This trip will only part of the work in this area and that a recent record the flora of dunal, wetland, scabland, and DNR land purchase will enhance the north/south riparian habitats found on and near West Bar. corridor that the Arid Lands Initiative identified as a critical pathway. Also, the recent land purchase by For this exploration, participants will carpool from CCC and the newly proposed wildflower trail at the the Lazy F Camp to Crescent Bar Resort in Trinidad. Canyon. We will make a short circuit around the From Crescent Bar Resort, participants will then be crest, dropping briefly into one of the populations of ferried across Lake Wanapum to West Bar by Lomatium columbianum.
Load more

Recommended publications
  • Periodically Spaced Anticlines of the Columbia Plateau
    Geological Society of America Special Paper 239 1989 Periodically spaced anticlines of the Columbia Plateau Thomas R. Watters Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington, D. C. 20560 ABSTRACT Deformation of the continental flood-basalt in the westernmost portion of the Columbia Plateau has resulted in regularly spaced anticlinal ridges. The periodic nature of the anticlines is characterized by dividing the Yakima fold belt into three domains on the basis of spacings and orientations: (1) the northern domain, made up of the eastern segments of Umtanum Ridge, the Saddle Mountains, and the Frenchman Hills; (2) the central domain, made up of segments of Rattlesnake Ridge, the eastern segments of Horse Heaven Hills, Yakima Ridge, the western segments of Umtanum Ridge, Cleman Mountain, Bethel Ridge, and Manastash Ridge; and (3) the southern domain, made up of Gordon Ridge, the Columbia Hills, the western segment of Horse Heaven Hills, Toppenish Ridge, and Ahtanum Ridge. The northern, central, and southern domains have mean spacings of 19.6,11.6, and 27.6 km, respectively, with a total range of 4 to 36 km and a mean of 20.4 km (n = 203). The basalts are modeled as a multilayer of thin linear elastic plates with frictionless contacts, resting on a mechanically weak elastic substrate of finite thickness, that has buckled at a critical wavelength of folding. Free slip between layers is assumed, based on the presence of thin sedimentary interbeds in the Grande Ronde Basalt separating groups of flows with an average thickness of roughly 280 m.
    [Show full text]
  • Splay-Fault Origin for the Yakima Fold-And-Thrust Belt, Washington State 2 3 Thomas L
    1 Splay-fault origin for the Yakima fold-and-thrust belt, Washington State 2 3 Thomas L. Pratt, United States Geological Survey, School of Oceanography, Box 357940, 4 University of Washington, Seattle, WA 98115 5 6 ABSTRACT 7 The Yakima fold-and-thrust belt (YFTB) is a set of anticlines above reverse faults in the 8 Miocene Columbia River Basalt (CRB) flows of Washington State. The YFTB is bisected by the 9 ~1100-km-long Olympic-Wallowa geomorphic lineament (OWL). There is considerable debate 10 about the origin and earthquake potential of the YFTB and OWL, which lie near six major dams 11 and a large nuclear waste storage site. Here I show that the trends of the YFTB anticlines relative 12 to the OWL match remarkably well the trends of the principal stresses determined from Linear 13 Elastic Fracture Mechanics (LEFM) modeling of the end of a vertical strike-slip fault. From this 14 comparison and the termination of some YFTB anticlines at the OWL, I argue that the YFTB 15 formed as splay faults caused by an abrupt decrease in the amount of strike-slip motion along the 16 OWL. If this hypothesis is correct, the OWL and YFTB are likely interconnected, deeply-rooted 17 structures capable of large earthquakes. 18 19 20 INTRODUCTION 21 The Yakima fold and thrust belt (YFTB) of central Washington State is a set of 22 prominent anticlines in the Miocene Columbia River Basalt flows (CRB; figure 1). The YFTB 23 anticlines form three distinct sets (Riedel et al., 1989 and 1994; Watters, 1989).
    [Show full text]
  • Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington
    Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey Cover. Palouse Falls, Washington. The Palouse River originates in Idaho and flows westward before it enters the Snake River near Lyons Ferry, Washington. About 10 kilometers north of this confluence, the river has eroded through the Wanapum Basalt and upper portion of the Grande Ronde Basalt to produce Palouse Falls, where the river drops 60 meters (198 feet) into the plunge pool below. The river’s course was created during the cataclysmic Missoula floods of the Pleistocene as ice dams along the Clark Fork River in Idaho periodically broke and reformed. These events released water from Glacial Lake Missoula, with the resulting floods into Washington creating the Channeled Scablands and Glacial Lake Lewis. Palouse Falls was created by headward erosion of these floodwaters as they spilled over the basalt into the Snake River. After the last of the floodwaters receded, the Palouse River began to follow the scabland channel it resides in today. Photograph by Stephen P. Reidel. Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington By Victor E. Camp, Stephen P. Reidel, Martin E. Ross, Richard J. Brown, and Stephen Self Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S.
    [Show full text]
  • Wagon Roads Map Download
    SEATTLE WALLA WALLA Union Gap Pioneer Cemetery: An early settler in the Red Mountain Wine Region: Though its 4,040 acres Pasco: Located at the confluence of the Snake and L’Ecole No. 41: Founded by Baker and Jean Seattle 13 Yakima Valley, Dr. Lewis H. Goodwin, lost his wife 16 of scrubby desert-dry sandy loam slopes may not 20 Columbia rivers and at the junction of the Northern 23 Ferguson in 1983, L’Ecole No. 41 is the third- Lake Sammamish State Park Priscilla in 1865. He donated the land, at the end of East constitute what some consider an actual “mountain,” the Red Pacific and Oregon Railway & Navigation Company rail oldest winery in the Walla Walla Valley and is known Ahtanum Road, around her burial site near the Yakima River Mountain appellation looms large in the world of North- lines, Pasco has long been a transportation hub. It replaced for sustainably produced wines with an international to the city for use as a cemetery. Many early Yakima Valley west wine. Even before the Yakima River-bordered area was Ainsworth, established two miles down the Columbia in 1879, reputation. Originally built in 1915 as part of the Fall City settlers are buried here. granted official AVA status in 2001, the exceptional grapes as a construction camp for the Northern Pacific Railway. The Frenchtown settlement along the Walla Walla River, Issaquah 1 grown in its windy vineyards had earned a towering reputa- town grew as freight and passengers connected there with the historic schoolhouse that houses the tasting room Battle of Two Buttes: On November 9, 1855, U.S.
    [Show full text]
  • Yakima Fold Belt Text
    w u 0 by Robert D. Bentley, Newell P. Campbell, and John E. Powell Open File Report 93·3 August 1993 WASHINGTON STATE DEPARTMENTOF Natural Resources Jennifer M. Belcher- Commissioner of Public Lands Kaleen Cottingham - Supervisor Division of Geology and Earth Resources LIBRARY DEPT. OF ~JATURAL RESOURCES GEOLOGY & EARTH RESOURCES DIVISION OL Yi'J!PIA, WA. 98504-7007 GEOLOGIC MAPS OF PART OF THE YAKIMA FOLD BELT, NORTHEASTERN YAKIMA COUNTY, WASHINGTON by Robert D. Bentley, Newell P. Campbell, and John E. Powell WASHINGTON STATE DEPARTMENT OF Natural Resources Jennifer M Belcher-Commissioner of Public Lands Kaleen Cottingham -Supervisor Washington Division of Geology and Earth Resources Open File Report 93-3 August 1993 WASHINGTON DEPARTMENT OF NATURAL RESOURCES Jennifer M. Belcher - Commissioner of Public Lands Kaleen Cottingham - Supervisor DIVISION OF GEOLOGY AND EARTH RESOURCES Ray Lasmanis, State Geologist This publication is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources PO Box 47007 Olympia WA 98504-7007 For more information or a list of publications, call (206) 902-1450. GEOLOGIC MAPS OF PART OF THE YAKIMA FOLD BELT, NORTHEASTERN YAKIMA COUNTY, WASHINGTON Robert D. Bentley, Newell P. Campbell, and John E. Powell INTRODUCTION The maps that make up this report cover four adjoining 15-minute quadrangles (Fig. 1), three in the Toppenish basin on the south and one in the Moxee basin to the north. Detailed discussions of the major geologic structural features of the Yakima Fold Belt, which encompasses these basins, are available in Reidel and Hooper (1989), Campbell and Bentley (1981), and Brown and Ellis (1977).
    [Show full text]
  • Differential Uplift and Incision of the Yakima River Terraces, Central
    PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE Differential uplift and incision of the Yakima River 10.1002/2015JB012303 terraces, central Washington State Key Points: Adrian M. Bender1, Colin B. Amos1, Paul Bierman2, Dylan H. Rood3,4, Lydia Staisch5, • 26 10 Al- Be isochron burial ages and lidar 6 5 data constrain bedrock incision rates Harvey Kelsey , and Brian Sherrod • Incision rates spanning ~2.9 Myr imply 1 2 differential rock uplift over two folds Geology Department, Western Washington University, Bellingham, Washington, USA, Department of Geology and 3 • Modest uplift and shortening imply Rubenstein School of the Environment and Natural Resources, University of Vermont, Burlington, Vermont, USA, Department that other regional structures are of Earth Science and Engineering, Imperial College London, London, UK, 4Scottish Universities Environmental Research Centre, also active East Kilbride, UK, 5U.S. Geological Survey Earthquake Science Center, Department of Earth and Space Sciences, University of Washington, Seattle, Washington, USA, 6Geology Department, Humboldt State University, Arcata, California, USA Supporting Information: • Texts S1–S3, Tables S1 and S2, and Figures S1–S12 Abstract The fault-related Yakima folds deform Miocene basalts and younger deposits of the Columbia Plateau in central Washington State. Geodesy implies ~2 mm/yr of NNE directed shortening across the folds, Correspondence to: but until now the distribution and rates of Quaternary deformation among individual structures has been A. M. Bender, [email protected] unclear. South of Ellensburg, Washington, the Yakima River cuts a ~600 m deep canyon across several Yakima folds, preserving gravel-mantled strath terraces that record progressive bedrock incision and related rock uplift.
    [Show full text]
  • Natural Gas Storage in Basalt Aquifers of the Columbia Basin, Pacific Northwest USA: a Guide to Site Characterization
    PNNL-13962 Natural Gas Storage in Basalt Aquifers of the Columbia Basin, Pacific Northwest USA: A Guide to Site Characterization prepared for United States Department of Energy National Energy Technology Laboratory 626 Cochrans Mill Road Pittsburgh, Pennsylvania 15236 August 2002 DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. Available to the public from the National Technical Information Service, U.S. Department of Commerce, 5285 Port Royal Road, Springfield, VA 22161; phone orders accepted at (703) 487-4650. This document was printed on recycled paper. (8/00) PNNL-13962 Natural Gas Storage in Basalt Aquifers of the Columbia Basin, Pacific Northwest USA: A Guide to Site Characterization S. P. Reidel V. G. Johnson F. A. Spane August 2002 Prepared for the U.S. Department of Energy under Contract DE-AC06-76RL01830 Pacific Northwest National Laboratory Richland, Washington 99352 Executive Summary Increasing domestic and commercial demand for natural gas in the Pacific Northwest requires development of adequate storage facilities.
    [Show full text]
  • Hanford Reach National Monument Rattlesnake Mountain Unit Public Access Scoping Report
    Hanford Reach National Monument Rattlesnake Mountain Unit Public Access Scoping Report April 18, 2016 U.S. Fish and Wildlife Service Hanford Reach National Monument Rattlesnake Mountain Unit Public Access Scoping Report Table of Contents 1. Introduction ........................................................................................................................................ 1 1.1 Purpose and Need ......................................................................................................................... 1 1.2 Description of Planning Area ....................................................................................................... 1 1.2.1 Hanford Reach National Monument Background.................................................................. 1 1.2.2 Administration as a National Wildlife Refuge ....................................................................... 3 1.2.3 Monument Purposes ............................................................................................................... 3 1.2.4 Area under Consideration ...................................................................................................... 4 2. Description of Scoping Process ......................................................................................................... 7 2.1 Outreach ....................................................................................................................................... 7 2.2 Rattlesnake Mountain Unit Access Tribal Working Group ........................................................
    [Show full text]
  • RHO-BWI-C-21: Preliminary Geology of Eastern Umtanum Ridge, South-Central Washington
    RHO-BWI-C-21 Li . f .: CE?t... nTr '1 ... GE1.. 0 ,.. Preliminary Geology Of Eastern Umtanum Ridge, South-Central Washington Fraser E. Goff Prepared for the United States Department of Energy Under Contract DE-AC06-77RL01030 QE176 84 Rockwell International G612p 1981 Rockwell Hanford Operations copy 2 Energy Systems Group Richland, WA 99352 Rockwell International Rockwell Hanford Operations Energy Systems Group Rich land, WA 99352 DISC LAIMER This report was prepared as sn sccount of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsi­ bility for the accuracy, completeness, or usefulness of any n~orn,ation apparatus, product, or process disclosed, or represents that its use would not infr nge privately owned rights. Refer­ ence rierein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise, does not necessar Iv const,tut~ or imply •ts endorsement, recom­ m<'ndat,on, or favoring by the United States Government or any agency thereof. The views and op1n1ons of authors expressed here n do not necessarily state or reflect those of the United States Government or any agency thereof. )0( BD-930 0-09 0 .2 ( R -1 -80) RHO-BWI-C-21 PRELIMINARY GEOLOGY OF EASTERN UMTANUM RIDGE, SOUTH-CENTRAL WASHINGTON Fraser E. Goff Consulting Geologist 2837 Ni eke 1 St. Los Alamos, NM 87544 January 1981 Prepared for Rockwell Hanford Operations, A Prime Contractor to U.S.
    [Show full text]
  • 1St INLAND NORTHWEST JURIED LANDSCAPE ART EXHIBITION
    CLOSE IN: 1st INLAND NORTHWEST JURIED LANDSCAPE ART EXHIBITION JUNDT ART MUSEUM MAY 26 THROUGH AUGUST 11, 2018 COVER: AARON JOHNSON (MOSCOW, ID) PALOUSE FARM (DETAIL), 2016 GOUACHE ON ILLUSTRATION BOARD RIGHT: DAVID MARTIN (CLEARWATER, IDAHO) SMOTHERED (DETAIL), 2017 PIGMENT BASED PRINT ON ARCHIVAL PAPER CLOSE IN: 1st INLAND NORTHWEST JURIED LANDSCAPE ART EXHIBITION JUNDT ART MUSEUM RAY ESPARSEN (LEWISTON, IDAHO) PRAYER FOR THE PALOUSE, 2016 OIL, METAL, AND WOOD NORA EGGER (SPOKANE, WASHINGTON) SPRING GRAZING LAND, 2014 OIL ON CANVAS DEL LUSK (SPOKANE, WASHINGTON) SPRING ON THE COEUR D’ALENE RIVER , 2006 PHOTOGRAPH ON PAPER DENNIS DEHART (PULLMAN, WASHINGTON) THE SALMON RUN: REMIXED, 2016 ARCHIVAL PIGMENT PRINT JEN ERICKSON (HAYDEN, IDAHO) SILENT HILL, 2018 WATERCOLOR AND GRAPHITE ON PANEL MEGHAN FLYNN (YAKIMA, WASHINGTON) TRUTH OR CONSEQUENCES, 2016 EGG TEMPERA ON PAPER JEN ERICKSON (HAYDEN, IDAHO) SILENT HILL, 2018 WATERCOLOR AND GRAPHITE ON PANEL MAJA SHAW (RICHLAND, WASHINGTON) YAKIMA RIVER CANYON, 2016 WATERCOLOR/ CUT PAPER ON PAPER MELISSA COLE (SPOKANE, WASHINGTON) , 2018 FLIGHT OVER WOODLAND ACRYLIC ON WOOD PANEL WITH FUSED GLASS ACCENTS SHEILA GRUBB (SPOKANE, WASHINGTON) PASSING STORM, 2018 OIL ON WOOD PANEL MICHAEL LEWIS (OTHELLO, WASHINGTON) UMTANUM RIDGE STORM, 2016 OIL ON LINEN CHRIS HEARD (ELLENSBURG, WASHINGTON) ALONG THE YAKIMA #3, 2017 ARCHIVAL PIGMENT PRINT ON PAPER WITH ACRYLIC VARNISH JACQUELINE TRUJILLO (ELLENSBURG, WASHINGTON) CONNECTION, 2017 OIL ON MASONITE ERIC JENSEN (ROSLYN, WASHINGTON) CLEALUM, 2017 OIL ON
    [Show full text]
  • Structure and Evolution of the Horse Heaven Hills in South-Central Washington
    Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1985 Structure and evolution of the Horse Heaven Hills in south-central Washington Michael Curtis Hagood Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons Let us know how access to this document benefits ou.y Recommended Citation Hagood, Michael Curtis, "Structure and evolution of the Horse Heaven Hills in south-central Washington" (1985). Dissertations and Theses. Paper 3600. https://doi.org/10.15760/etd.5484 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. AN ABSTRACT OF THE THESIS OF Michael Curtis Hagood for the Master of Science in Geology presented February 21, 1985. Title: Structure and Evolution of the Horse Heaven Hills in South-Central Washington. APPROVED BY MEMBERS OF THE THESIS COMMITTEE: M~. Mkhae l L. Cummings ··~ · · i1 llfert p e P. Reidel The Horse Heaven Hills uplift in south-central Washington con­ sists of distinct northwest and northeast trends which merge in the lower Yakima Valley. The northwest trend is adjacent to and parallels the Rattlesnake-Wallula alignment (RAW; a part of the Olympic-Wallowa lineament). The northwest trend and northeast trend consist of aligned or en echelon anticlines and monoclines whose axes are gener- ally oriented in the direction of the trend. At the intersection, 2 folds in the northeast trend plunge onto and are terminated by folds of the northwest trend.
    [Show full text]
  • Stratigraphy of South-Central Washington
    t l WHC-SA-1764-FP _OV09 199_ Late Cenozoic Structure and o s T/ Stratigraphy of South-Central Washington S. P. Reidel N. P. Campbell K. R. Fecht K. A. Lindsey To bepublishedin SecondSymposiumonthe GeologyofWasaington Prepared for the U.S. Department of Energy Office of Environmental Restoration and Waste Management WHanfon;IestinlCompany[llouse RP,O,lchlandBox, _W.97oashington 99352 HanfordOpera0onsand EngmeenngCono'aclorfor _e U.S. 0epartmentot EnergyunclerContractOE.AC06.87RL10930 i i . - CopyrightLloen_e9ya==_mceo_In,=an=e.¢_emX=ih_ariaor, t=_po___ cneU.S.Gov_rvnent'r,gr,= to retaina non=clul_,, royUy-_reet=enl4 _narmto anyooPyngm¢ovettngmmI_. Approved for Public Release _l__lt_ DIIS!RtBU]'ION OF ]HIS DOCUMP-.N]" IS UNLIMITE_ J LEGALDISCLAIMER Thisreportwaspreparedas an accountof worksponsoredby an agencyof theUnitedStatesGovernment,Neitherthe UnitedStatesGovernmentnorany agencythereof,noranyof theiremployees,nor anyof theircontractors,subcontractors ortheiremployees,makesanywarranty,expressorimplied, orassumesanylegalliabilityorresponsibilityfor the accuracy,completeness,or anythirdparty'suseor theresults ofsuch useof anyinformation,apparatus,product,orprocess disclosed,orrepresentsthatits usewouldnotinfringe privatelyownedrights. Referencehereintoanyspecific commercialproduct,process,orserviceby tradename, trademark,manufacturer,orotherwise,doesnotnecessarily constituteor implyils endorsement,recommendationo,r favoringbytheUnitedStatesGovernmentorany agency thereoforits contractorsorsubcontractors.Theviewsand opinionsof authorsexpressedhereindo
    [Show full text]