DOCSLIB.ORG

FINAL 2020 Tours

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
FINAL 2020 Tours REACH 2020 MUSEUM tours OVERVIEW Experience the unique history of the land that surrounds the Mid-Columbia River region through a variety of specially designed tours offered through The REACH Museum. From exploratory hikes to tracing the paths of the Ice Age floods; from kayaking on the Columbia River to strolling through an aromatic lavender farm; or take a tour of a local hop farm, processing plant and microbrewery to imbibe in local draughts. Cost of each tour includes transportation to and from the location and lunch. Participants are requested to arrive at The REACH 15 minutes before the start time so that the tour can depart on time. The provided lunch is a sandwich, small bag of chips, a cookie and a small bottled water. Participants with special dietary requirements are responsible for bringing their own. The REACH prohibits open containers of alcohol during transportation. CANCELLATION POLICY Any cancellation seven (7) days before the tour date will receive a full refund. The REACH will retain 25% of the ticket cost if a cancellation occurs less than seven (7) days before the tour date. Tours are subject to cancellation if there are not enough registered participants to fulfill the minimum requirement. Western Scablands Friday April 10 9am-3pm $99.99 per person Tour guide: Gary Kleinknecht HIGHLIGHTS Yakima Fold Belt Drumheller Channels West Bar Potholes Coulee Frenchman Coulee Transportation/lunch provided In the 1920s, J. Harlen Bretz was the first to coin the term scablands as a variety of channels and rock basins eroded into the native basalt rock of the region. He argued that massive flooding in the past caused the scablands and in the 1950s, his theories were finally vindicated. "They could not More than 40 cataclysmic floods over the last two million years caused the channeled scablands of Eastern Washington. The last flood occurred be more between 18,000 and 14,000 years ago when a glacial dam failed and ancient Lake Missoula in erratically and Montana swept across Idaho, Washington and followed the Columbia River into the Pacific Ocean. impossibly This tremendous water flow was 10 times that of designed." all of the modern rivers of the world and several hundred feet deep. The huge surge of water filled and then moved across normal stream and river valleys. The existing drainage patterns were ineffectual, creating a 100-mile wide pattern of braided channels. Where the water flowed deep and fast, it tore away soil and underlying volcanic bedrock, leaving behind the coulees and scablands seen today. Deposits of gravel, sand, and silt accumulating over millions of years, brought by flooding of tributaries of the Columbia River and ancient lakes including Lake Missoula formed the White Bluffs, no part of the Hanford Reach National Monument. 20 miles The Columbia River cut through the collected sediment to reveal 15 banded slackwater flood rhythmites, which tower to 900 feet at their north of highest point. Any visible gravel must have traveled on icebergs during the flooding at the Richland same time the rhythmites were forming. In recent history, saturated soil from naturally unstable irrigation waters from the Central Columbia Basin Irrigation Project most likely caused the rate of natural erosion to accelerate. Water slowly strains through the silt and sand until it comes to a layer, which the water cannot pass through, leading to extreme slope instability, pockets of water, and deep fissures. White Bluffs Hike Saturday, April 18 9am-3pm $99.99 per person Tour Guide: Bruce Bjornstad Highlights Within the Hanford Reach National Monument Geology/Wildflowers Moderate hike, approximately 5 miles at 300 feet elevation gain. Transportation/lunch provided Wallula Gap Hike Saturday, May 2 9am-3pm $99.99 per person Tour Guide: Bruce Bjornstad HIGHLIGHTS STRENUOUS HIKE NO BATHROOM Twin Sisters Rocks ~7 miles, ~800 ft. elevation gain Transportation/lunch provided When the waters from Lake Missoula swept across Eastern Washington; the channeled scablands led the water into Pasco Basin and escaped out of a single outlet before filling the Columbia Basin Gorge. Since all of the floodwaters had to pass through such a narrow passage, a huge lake formed The Narrow behind Wallula Gap extending to a surface area of approximately 4,500 square miles and a depth of about 900 feet. Passage Although Lake Lewis was only a temporary lake, boulders of various sizes, visible today, highlight the power and size of the Ice Age floods. These iceberg-carried erratics, including granite and diorite, stand out compared to the dark basalt native to the region. Floodwaters from ancient Lake Missoula uncovered basalt underneath a mixture of sediment and created deep canyons, plunge pools and cataracts. The current was so powerful that some of these depressions are more than 200 feet deep. Remnants of Among the widest channels is the Cheney- Palouse Tract, spanning 20 miles wide and 600 Massive feet deep. The south valley wall of the ancestral Palouse River, which flowed through the now Erosional dry Washtucna Coulee and onto the Columbia River, was overtopped. Energy As seen today, the current course of water is from the Snake River to the Palouse Falls. There is an upper fall with a drop around 20 feet, north-northwest of the main drop, 198 feet. Southern Cheney- Palouse Scablands Friday, May 15 8am-3pm $99.99 per person Tour Guide: Gary Kleinknecht HIGHLIGHTS Old Maid Coulee Washtucna Coulee Stair Case Rapids Palouse Falls HU Coulee Devils Coulee Transportation/lunch provided IAF & Lavender Friday,June 5 9am-2pm $99.99 per person Tour Guide: Gary Kleinknecht HIGHLIGHTS Wallula Gap Clastic Dikes Lavender Farm Transportation/lunch provided Clastic dikes are one of many visible elements of the Ice Age Floods (IAF). Formed by water, wind, and gravity, sediment is swept into a fissure, cutting across a different layer of sediment or rock type. This filled crack is identifiable by the usual vertical or near- vertical layer, the length being many times larger than the width. Land The diverse soil makeup of eastern Washington can also be attributed to the Ice Age Floods. Diversity There are more than 300 different crops grown in the state. Lavender, France’s quintessential crop, has been thriving under the Grimaud family’s care on their farm in Lowden, Washington outside of Walla Walla. Nearly all of the planting, weeding, harvesting, drying, and processing is carried out by hand. The Hanford Reach is the longest free-flowing, non-tidal stretch of the Columbia River, located between Priest Rapids Dam and McNary Dam. It flows through the Hanford Reach National The Monument, an area untouched by development or agriculture since 1943.U.S. Department of Fish and Wildlife manages this involuntary Involuntary park, preserving it as a wildlife refuge with an abundance of flora and fauna exemplary of the Park shrub-steppe ecosystem. Additionally, the Hanford Nuclear Reservation is within the Monument. Nine reactors that produced plutonium, left over from World War II and the Cold War era dot along the shoreline, managed by the Department of Energy. Kayak the Reach Ntl. Monument Saturday, August 8 8am-3pm $99.99 per person Tour Guide: US Fish & Wildlife HIGHLIGHTS Wildlife Cliffs B-Reactor Transportation/lunch provided Hops & Beer of the Mid- Columbia Saturday, September 5 9am-3pm $99.99 per person HIGHLIGHTS Carpenter Ranches LLC YCH Hops Varietal Beer Co. Transportation/lunch provided Participants are responsible for beer tasting fees. Washington’s Yakima Valley has the ideal climate and irrigation conditions for hops, making it one of the most productive hop- growing regions in the world. In the United States, 75% of all hop farms are located in the Yakima Valley and they produce 77% of all United States hops. Many of these farms, like Carpenter Ranches LLC, are family owned and operated by third or fourth Ideal Climate generations. Currently, there are approximately 404 breweries in Washington State, with 80% producing less than 1,000 barrels per year. Only 70 breweries in Washington State produce more than 1,000 barrels per year. Varietal Brewing Company in Sunnyside has a 10 barrel (310 gallon) brewhouse for their production. .
Load more

Recommended publications
  • Flood Basalts and Glacier Floods—Roadside Geology
    u 0 by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 WASHINGTON STATE DEPARTMENTOF Natural Resources Jennifer M. Belcher - Commissioner of Public Lands Kaleen Cottingham - Supervisor FLOOD BASALTS AND GLACIER FLOODS: Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 Kaleen Cottingham - Supervisor Division of Geology and Earth Resources WASHINGTON DEPARTMENT OF NATURAL RESOURCES Jennifer M. Belcher-Commissio11er of Public Lands Kaleeo Cottingham-Supervisor DMSION OF GEOLOGY AND EARTH RESOURCES Raymond Lasmanis-State Geologist J. Eric Schuster-Assistant State Geologist William S. Lingley, Jr.-Assistant State Geologist This report is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources P.O. Box 47007 Olympia, WA 98504-7007 Price $ 3.24 Tax (WA residents only) ~ Total $ 3.50 Mail orders must be prepaid: please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources. Front Cover: Palouse Falls (56 m high) in the canyon of the Palouse River. Printed oo recycled paper Printed io the United States of America Contents 1 General geology of southeastern Washington 1 Magnetic polarity 2 Geologic time 2 Columbia River Basalt Group 2 Tectonic features 5 Quaternary sedimentation 6 Road log 7 Further reading 7 Acknowledgments 8 Part 1 - Walla Walla to Palouse Falls (69.0 miles) 21 Part 2 - Palouse Falls to Lower Monumental Dam (27.0 miles) 26 Part 3 - Lower Monumental Dam to Ice Harbor Dam (38.7 miles) 33 Part 4 - Ice Harbor Dam to Wallula Gap (26.7 mi les) 38 Part 5 - Wallula Gap to Walla Walla (42.0 miles) 44 References cited ILLUSTRATIONS I Figure 1.
    [Show full text]
  • Interior Columbia Basin Mollusk Species of Special Concern
    Deixis l-4 consultants INTERIOR COLUMl3lA BASIN MOLLUSK SPECIES OF SPECIAL CONCERN cryptomasfix magnidenfata (Pilsbly, 1940), x7.5 FINAL REPORT Contract #43-OEOO-4-9112 Prepared for: INTERIOR COLUMBIA BASIN ECOSYSTEM MANAGEMENT PROJECT 112 East Poplar Street Walla Walla, WA 99362 TERRENCE J. FREST EDWARD J. JOHANNES January 15, 1995 2517 NE 65th Street Seattle, WA 98115-7125 ‘(206) 527-6764 INTERIOR COLUMBIA BASIN MOLLUSK SPECIES OF SPECIAL CONCERN Terrence J. Frest & Edward J. Johannes Deixis Consultants 2517 NE 65th Street Seattle, WA 98115-7125 (206) 527-6764 January 15,1995 i Each shell, each crawling insect holds a rank important in the plan of Him who framed This scale of beings; holds a rank, which lost Would break the chain and leave behind a gap Which Nature’s self wcuid rue. -Stiiiingfieet, quoted in Tryon (1882) The fast word in ignorance is the man who says of an animal or plant: “what good is it?” If the land mechanism as a whole is good, then every part is good, whether we understand it or not. if the biota in the course of eons has built something we like but do not understand, then who but a fool would discard seemingly useless parts? To keep every cog and wheel is the first rule of intelligent tinkering. -Aido Leopold Put the information you have uncovered to beneficial use. -Anonymous: fortune cookie from China Garden restaurant, Seattle, WA in this “business first” society that we have developed (and that we maintain), the promulgators and pragmatic apologists who favor a “single crop” approach, to enable a continuous “harvest” from the natural system that we have decimated in the name of profits, jobs, etc., are fairfy easy to find.
    [Show full text]
  • Northwest Exposure Winners Revealed!
    Winter weekend getaway in Leavenworth A Publication of Washington Trails Association | wta.org Northwest Exposure Winners Revealed! 10 Trails for This Winter State Parks Centennial 2013 Volunteer Vacations Jan+Feb 2013 Jan+Feb 2013 20 16 32 NW Weekend: Leavenworth » Eli Boschetto NW Explorer An alpine holiday is waiting for you on the east side of the Cascades. Snowshoe, ski, take in the annual Ice Fest Northwest Exposure celebration or just relax away from home. » p.20 Congratulations to the winners of WTA's 2012 Northwest Exposure photo contest. Images from across the state— Tales From the Trail » Craig Romano and a calendar for planning hikes too! » center Guidebook author Craig Romano shares insights and lessons learned from years of hiking experience. » p.24 Nordic Washington » Holly Weiler Hit the tracks this winter on Nordic skis. Destinations Epic Trails » Wonderland » Tami Asars across Washington will help you find your ideal escape at Info and tips to help you plan your own hiking adventure some of the best resorts and Sno-Parks. » p.16 on the classic round-the-mountain trail. » p.32 WTA at Work 2013 marks the 100th anniversary of Trail Work » Sarah Rich Washington's state park system. With Bridge-building in the Methow » p.10 more than 700 miles of hiking trails, Engineering Trails » Janice Van Cleve make a plan to visit one this year. » p.8 Turnpikes—what they are and how they're constructed » p.12 Advocacy » Jonathan Guzzo Budget concerns for 2013 » p.14 Youth on Trails » Krista Dooley Snowshoeing with kids » p.15 Trail Mix Gear Closet » Winter camping essentials » p.22 Nature Nook » Tami Asars Birds, beasts and blooms in the NW » p.25 Cape Disappointment, by Jeremy Horton 2 Washington Trails | Jan+Feb 2013 | wta.org Guest Contributors TAMI ASARS is a writer, photographer and career hiker.
    [Show full text]
  • RCFB April 2021 Page 1 Agenda TUESDAY, April 27 OPENING and MANAGEMENT REPORTS 9:00 A.M
    REVISED 4/8/21 Proposed Agenda Recreation and Conservation Funding Board April 27, 2021 Online Meeting ATTENTION: Protecting the public, our partners, and our staff are of the utmost importance. Due to health concerns with the novel coronavirus this meeting will be held online. The public is encouraged to participate online and will be given opportunities to comment, as noted below. If you wish to participate online, please click the link below to register and follow the instructions in advance of the meeting. Technical support for the meeting will be provided by RCO’s board liaison who can be reached at [email protected]. Registration Link: https://zoom.us/webinar/register/WN_JqkQAGCrRSOwbHLmg3a6oA Phone Option: (669)900-6833 - Webinar ID: 967 5491 2108 Location: RCO will also have a public meeting location for members of the public to listen via phone as required by the Open Public Meeting Act, unless this requirement is waived by gubernatorial executive order. In order to enter the building, the public must not exhibit symptoms of the COVID-19 and will be required to comply with current state law around personal protective equipment. RCO staff will meet the public in front of the main entrance to the natural resources building and escort them in. *Additionally, RCO will record this meeting and would be happy to assist you after the meeting to gain access to the information. Order of Presentation: In general, each agenda item will include a short staff presentation and followed by board discussion. The board only makes decisions following the public comment portion of the agenda decision item.
    [Show full text]
  • Washington Geology Released Since [Project Chief: W
    ·- July 1983 Volume 11 Number 3 Washington Geologic Newsletter · . Lovitt mine, near Wenatchee, Chelan County, Washington, 1977. Photo by Jack Jansons BRIAN J . BOYLE COMMISSIONER OF PUBLIC LANDS ART STEARNS, Supervisor RAYMOND LASMANIS, State Geologist DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGY AND EARTH RESOURCES Marlin Woy - To Porllond n Exit IOs·• [" GEOLOGY ANO /. t Roctl)11onl•t ... Solllh EARTH ~CES i..-<-....<....<c.L..'-'-! !! 0 I u Sound .. C 'Entrance- Moll Elf!H~~• · 0Poulsot\S. Mortin\ s,. : ••••• ,Porklno .....~ :....... ----. ........... .................... • • • • •• • • • • Coll•o• Z ·········o····· ... 4224 6th Ave. S.E., Lacey, Washington in Albortson• MAILING ADDRESS: Department of Natural Resources Division of Geology and Earth Resources Olympia, WA 98504 (206) 459-6372 Field office address: Department of Natural Resources Division of Geology and Earth Resources Spokane County Agricultural Center N. 222 Havana Spokane, WA 99202 ( 509) 458-2038 Lauta Btay, Editor The Washington Geologic Newsletter, a quarterly report of geologlc articles, Ts published by the Division of Geology and Earth Resources, Department of Natural Resources. The newsletter is free upon request. The division also publishes bulletins, information circulars, and geologic maps. A list of these publicatiOflS will be sent upon request. .. THE WENATCHEE GOLD RUSH by Bonnie Bunning* INTRODUCTION from the D ''reef" between 1949 and 1967. For a long time the ore was shipped directly to the Tacoma smelter On March 4, 19831 when Breakwater Resources LLd. where a substantial credit for the siliceous ores (used as and Asamera Minerals, Inc., made their exciting gold find flux in the smelter) helped make t he mine profitable. In public, companies and individuals from Canada and the 1961, Day Mines, Inc., and Lovitt Mining Co.
    [Show full text]
  • A Model for Measuring the Benefits of State Parks for the Washington State Parks And
    6 A Model for Measuring the Benefits of State Parks for the Washington State Parks and january 201 january Recreation Commission Prepared By: Prepared For: Earth Economics Washington State Parks and Tacoma, Washington Recreation Commission Olympia, Washington Primary Authors: Tania Briceno, PhD, Ecological Economist, Earth Economics Johnny Mojica, Research Analyst, Earth Economics Suggested Citation: Briceno, T., Mojica, J. 2016. Statewide Land Acquisition and New Park Development Strategy. Earth Economics, Tacoma, WA. Acknowledgements: Thanks to all who supported this project including the Earth Economics team: Greg Schundler (GIS analysis), Corrine Armistead (Research, Analysis, and GIS), Jessica Hanson (editor), Josh Reyneveld (managing director), Sage McElroy (design); the Washington State Parks and Recreation Commission: Tom Oliva, Katie Manning, Steve Hahn, Steve Brand, Nikki Fields, Peter Herzog and others. We would also like to thank our Board of Directors for their continued guidance and support: Ingrid Rasch, David Cosman, Sherry Richardson, David Batker, and Joshua Farley. The authors are responsible for the content of this report. Cover image: Washington State Department of Transportation ©2016 by Earth Economics. Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holder provided the source is fully acknowledged. Reproduction of this publication for resale or other commercial purposes is prohibited without prior written permission of the copyright holder. Executive Summary Washington’s state parks provide a myriad of benefits to both urban and rural environments and nearby residents. Green spaces within state parks provide direct benefits to the populations living in close proximity. For example, the forests within state parks provide outdoor recreational opportunities, and they also help to store water and control flooding during heavy rainfalls, improve air quality, and regulate the local climate.
    [Show full text]
  • Walla Walla Subbasin Assessment
    Walla Walla Subbasin Assessment General Overview Components Prepared by: Walla Walla Basin Watershed Council Version 2: April 2004 Note: This document was not reviewed or approved by the Subbasin Planning Team, subbasin plan leads, co-managers, or subbasin technical staff. 1 Introduction History and Description of Planning Entity The organization for developing the Walla Walla River Subbasin Plan was comprised of the lead agencies, subcontractors, the Planning Team, the Technical Team, and other governmental and non-governmental organizations that will provide local input. The role of each member group is described below. Lead Agencies and Co-Lead Agency The lead agency for the Oregon portion of the Walla Walla subbasin was the Walla Walla Basin Watershed Council, with the Walla Walla Watershed Foundation serving as its fiscal agent. The co-lead entity for the Washington portion of the subbasin was Walla Walla County. The responsibility of co-leads was to oversee and initiate the planning process and ensure that it was an open and inclusive and there was proper outreach to and input from subbasin stakeholders. Subcontractors The Co-lead entities subcontracted with consultant(s) to perform the following functions: (1) facilitation assistance, (2) public involvement assistance, and (3) report preparation including technical assistance. The consultants’ roles were to facilitate and assist with the coordination of Technical and Planning Team and Working Group meetings. The consultants worked closely with the Technical and Planning Teams and the Working Group, and compiled, edited, and wrote (as appropriate) various sections of all draft and final versions of the assessment, inventory, and management plan components of the subbasin plan.
    [Show full text]
  • Chapter 7. Parks and Recreation Element
    1 Chapter 7. Parks and Recreation Element 2 7.1. Introduction 3 Parks, recreational facilities, and open space are generally considered beneficial resources and 4 essential contributors to a community’s quality of life. Located within the County are a number 5 of different types of parks and recreational facilities. 6 The County has not traditionally served as a provider of park and recreation facilities. Local 7 cities, private agencies, federal agencies, and schools have an established history of furnishing 8 these services. 9 The purpose of this element is to evaluate parks and recreation facilities in the County and to 10 develop goals and policies that guide management and coordination of them. 11 7.1.1. Applicable Growth Management Act Goals 12 GMA planning goals that are applicable to the Parks and Recreation Element include the 13 following: 14 . Open space and recreation. Retain open space, enhance recreational opportunities, conserve 15 fish and wildlife habitat, increase access to natural resource lands and water, and develop 16 parks and recreation facilities (Revised Code of Washington [RCW] 36.70A.020(9)). 17 . Public facilities and services. Ensure that those public facilities and services necessary to 18 support development shall be adequate to serve the development at the time the development 19 is available for occupancy and use without decreasing current service levels below locally 20 established minimum standards (RCW 36.70A.020(12)). 21 . Historic preservation. Identify and encourage the preservation of lands, sites, and structures 22 that have historical or archaeological significance (RCW 36.70A.020(13)). 23 Goals described in the Shoreline Management Act (SMA) also support the Parks and Recreation 24 Element.
    [Show full text]
  • Lake Missoula and Its Floods by Kendall L
    Society for Range Management Lake Missoula and Its Floods By Kendall L. Johnson he city of Spokane lies astride the Spokane River, out of the earth over previous untold centuries. The winds some 40 miles from its origination near Coeur created dune-like deposits of variable orientation and depth d’Alene, Idaho. The convention center and that today make up fertile farmland in southeastern hotel, site of the 65th annual meeting of SRM, are Washington and adjacent Idaho. Bretz’s Flood followed the Tlocated right along the river, creating a beautiful and even path of the many earlier fl oods and recreated the effects over idyllic setting. These qualities make it even harder to imagine thousands of square miles in the Columbia Basin. These can a long-ago day when a miles-wide wall of water, measuring briefl y be considered in four major categories: 1) the chan- as much as 500 feet high, bore down on this site. Hours neled scablands, 2) the river canyon, 3) the Grand Coulee, before, a great ice dam on glacial Lake Missoula (present-day and 4) Lake Lewis. Clark Fork River) had failed. The dam was as much as 2,500 feet in height, impounded a lake up to 2,000 feet deep, The Channeled Scablands extended east in the intermontane valleys for 200 miles, and The enormous depth of the advancing front of water, covered some 3,000 square miles. It probably contained over 500 cubic miles of water, approximating half the volume of measured in the several hundreds of feet, moving at speeds Lake Michigan.
    [Show full text]
  • INTERIOR/GEOLOGICAL SURVEY USGS· INF -72- 2 !R I) - Electric City-Grand Coulee, Washington the CHANNELED SCABLANDS of EASTERN WASHINGTON
    9 INTERIOR/GEOLOGICAL SURVEY USGS· INF -72- 2 !R I) - Electric City-Grand Coulee, Washington THE CHANNELED SCABLANDS OF EASTERN WASHINGTON - The Geologic Story of the Spokane Flood- '(( U.S. GOVERNMENT PRINTING OFFICE , 1976 0 -208-172 F'or sale by the uperint.endent. of Documents, .S. Government Printing Office Washington, D.. 20402- Pric~ 70 cents Lock No. 024 - 001-02507- I nL nlog o. I 19.2: W27/6/974 There is n minimum charge of $1.00 for each mail order A trave ler enterin g th e tal f W as hington fro m th e Eas t crosses a flat-to-rolling country­ sid o f deep, fertil so il commonly sown with w heat. ontinuing wes twa rd , he abruptly nters a d eply scar red land o f bare bl a k ro k ut by labyrin thine ca nyons and chann el , plunge pools and ro k bas in s, ca ca de and ca tara t ledges, and di playi ng ragged buttes and li ffs, alcoves, im­ men e gravel bars, and giant ripple marks. Th e traveler has reached the starkly sceni " Chan­ neled cab lands," and this d ramatic hange in th e landscape may well ca use him to w onder " w hat happ n d here? " Th e answ er- th e grea te t fl ood documented by man. This publica tion, summari zin g th e equence of geologic events that culminated in th e so-call ed ''Spokan Fl ood," w as prepar d in res ponse to a ge neral int re t in geology and a particul ar interes t in th e o ri gin of th e Scab land o ften ex pre sed by th ose ross in g th e State of W as hington.
    [Show full text]
  • PALOUSE to PINES LOOP
    PA LOUSE to PINE S LOOP INDEX Sites Page Sites Page INFO KEY 1 1 Riverside State Park 2 28 Hawk Creek Falls 8 2 Little Spokane River Natural 29 Davenport Cemetery Area 30 Reardan Audubon Lake 31 Iller Creek Conservation Area 3 Lake Spokane Boat Launch 32 Liberty Lake County Park 4 Antoine Peak Conservation 3 33 Slavin Ranch Conservation Area 9 Area 5 Feryn Ranch Conservation 34 Steptoe Butte State Park Area 35 Kamiak Butte Park 6 Mt. Spokane State Park 37 Wawawai County Park 7 Pend Oreille County Park 38 Nisqually John Habitat 8 Calispell Lake 10 Management Unit 9 Usk Bridge 4 39 Greenbelt Trail 10 Tacoma Creek 40 Swallow’s Park 11 Flying Goose Ranch 41 Headgates County Park 12 Yocum Lake 42 Fields Spring State Park 13 Noisy Creek Campground 43 Chief Timothy Habitat Manage- 14 Elk Creek Trail 5 ment Unit 15 Salmo Priest Wilderness 44 WT Wooten Wildlife Area 16 Big Meadow Lake 11 45 Lewis and Clark Trail State Park 17 Little Pend Oreille National 46 Palouse Falls State Park Wildlife Refuge 47 Bassett Park 18 Sherman Creek Wildlife 6 48 Sprague Lake Area 49 Rock Lake 19 Log Flume Heritage Site 50 Smick Meadow 20 Sherman Pass Overlook 12 51 Turnbull National Wildlife 21 Mud Lake Refuge 22 Kettle River Rails-to-Trails 23 Lone Ranch Park 7 24 Lake Beth CREDITS 13 White-headed Woodpecker 25 Swan Lake Campground 26 Swanson Lakes © Ed Newbold, 2009 27 Telford The Great Washington State Birding Trail 1 PALOUSE to PINES LOOP INFO KEY Map ICons Best seasons for birding (spring, summer, fall, winter) Developed camping available, including restrooms; fee required Restroom available at day-use site Handicapped restroom and handicapped trail or viewing access Site located in an Important Bird Area Fee required; passes best obtained prior to travel.
    [Show full text]
  • THE SPOKANE AQUIFER, WASHINGTON: Its Geologic Origin
    THE SPOKANE AQUIFER, WASHINGTON: Its Geologic Origin and Water-Bearing and Water-Quality Characteristics Cover: Aerial view of the Spokane Flood sweep­ ing southwesterly across the study area (outlined in red) and vicinity. THE SPOKANE AQUIFER, WASHINGTON: Its Geologic Origin and Water-Bearing and Water-Quality Characteristics By Dee Molenaar U.S. GEOLOGICAL SURVEY WATER-SUPPLY PAPER 2265 DEPARTMENT OF THE INTERIOR DONALD PAULHODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1988 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 Library of Congress Cataloging in Publication Data Molenaar, Dee. The Spokane aquifer, Washington. (U.S. Geological Survey water-supply paper; 2265) Bibliography: p. Supt.ofDocs.no. : 119.13:2265 1. Aquifers Washington (State) Spokane Region. I. Title. II. Series. GB1199.3.W2M651987 553.7'9'0979737 84-600259 PREFACE: WHY THIS REPORT WAS WRITTEN This report was prepared to provide a non­ The description of the Spokane aquifer technical description and understanding of the includes the geologic story behind its origin Spokane aquifer, one of the world's most pro­ and its part in the Spokane Valley's hydrologic ductive water-bearing formations. Because the setting. Discussed are the relation among pre­ aquifer also has a most fascinating geologic ori­ cipitation over the area (mostly in the head­ gin, a discussion of the geologic story of the waters of the Spokane River basin), the flow of Spokane area is presented. This should enhance the Spokane River, and the movement of the reader's appreciation of the natural proces­ water to, through, and from the aquifer.
    [Show full text]