Lewis River ~ Including Clear, Quartz, Siouxon, Pine, Rush, Smith Creeks & the Muddy River
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Anthropological Study of Yakama Tribe
1 Anthropological Study of Yakama Tribe: Traditional Resource Harvest Sites West of the Crest of the Cascades Mountains in Washington State and below the Cascades of the Columbia River Eugene Hunn Department of Anthropology Box 353100 University of Washington Seattle, WA 98195-3100 [email protected] for State of Washington Department of Fish and Wildlife WDFW contract # 38030449 preliminary draft October 11, 2003 2 Table of Contents Acknowledgements 4 Executive Summary 5 Map 1 5f 1. Goals and scope of this report 6 2. Defining the relevant Indian groups 7 2.1. How Sahaptin names for Indian groups are formed 7 2.2. The Yakama Nation 8 Table 1: Yakama signatory tribes and bands 8 Table 2: Yakama headmen and chiefs 8-9 2.3. Who are the ―Klickitat‖? 10 2.4. Who are the ―Cascade Indians‖? 11 2.5. Who are the ―Cowlitz‖/Taitnapam? 11 2.6. The Plateau/Northwest Coast cultural divide: Treaty lines versus cultural 12 divides 2.6.1. The Handbook of North American Indians: Northwest Coast versus 13 Plateau 2.7. Conclusions 14 3. Historical questions 15 3.1. A brief summary of early Euroamerican influences in the region 15 3.2. How did Sahaptin-speakers end up west of the Cascade crest? 17 Map 2 18f 3.3. James Teit‘s hypothesis 18 3.4. Melville Jacobs‘s counter argument 19 4. The Taitnapam 21 4.1. Taitnapam sources 21 4.2. Taitnapam affiliations 22 4.3. Taitnapam territory 23 4.3.1. Jim Yoke and Lewy Costima on Taitnapam territory 24 4.4. -
A Learning Guide on the Geology of the Cispus Environmental Center Area, Lewis County, Washington
A Learning Guide on the GEOLOGY OF THE CISPUS ENVIRONMENTAL CENTER AREA LEWIS COUNTY, WASHINGTON By J. ERIC SCHUSTER, GeoJo i t DEPARTMENT OF NATURAL RESOURCES DIVISION OF MINES AND GEOLOGY Prepar d in coop ration with the Superintendent o Public Instruction 1973 CONTENTS Page Introd uctio n ................................................................... 1 Geo logic hi story ....................................•.......................... Genera I • . • . • . • . • . • . • . • . • . • . • • . • . • . • • • 1 Tower Rock . • . 4 Rock descriptions . • . • . • . • . • . • . • 5 0 hanapecosh Formation •... ... ................•...•...••.•.•....••••••• , 5 Fifes Peak Formation . • . 7 Tatoosh? pluton........................................................ 7 Quaternary rocks • . • . • . • . • . • . • • • • • • • 8 Suggested exercises • . • . • . • . • • • • 10 Explanation of terms •...............................•...•....•...•........•••••• 13 Appendix A-Occurrences of metallic minera ls •................••..........••••••. 19 Appendix B-Occurrences of nonmetallic minerals •.................•......•••••••• 39 I LLUST RA Tl O NS Page Figure 1.-The formation of an angular unconformity 2 2.-Tower Rock as seen from the oppo site side of the Cispus River valley. View is toward the southeast ••......•.........•..• ;............ 4 3.-Line drawing showing alignment of mineral grains due to flow in mo I ten rock • . • • • .. • • • 6 4.-Line drawing of quartz and heulandite filling vesicles in flow rock. • • • • • • • • 6 5.- Geologic map and cross -
GEOLOGIC MAP of the MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE of SOUTHERN WASHINGTON by Wes Hildreth and Judy Fierstein
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2460 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE OF SOUTHERN WASHINGTON By Wes Hildreth and Judy Fierstein When I climbed Mount Adams {17-18 August 1945] about 1950 m (6400') most of the landscape is mantled I think I found the answer to the question of why men by dense forests and huckleberry thickets. Ten radial stake everything to reach these peaks, yet obtain no glaciers and the summit icecap today cover only about visible reward for their exhaustion... Man's greatest 2.5 percent (16 km2) of the cone, but in latest Pleis experience-the one that brings supreme exultation tocene time (25-11 ka) as much as 80 percent of Mount is spiritual, not physical. It is the catching of some Adams was under ice. The volcano is drained radially vision of the universe and translating it into a poem by numerous tributaries of the Klickitat, White Salmon, or work of art ... Lewis, and Cis pus Rivers (figs. 1, 2), all of which ulti William 0. Douglas mately flow into the Columbia. Most of Mount Adams and a vast area west of it are Of Men and Mountains administered by the U.S. Forest Service, which has long had the dual charge of protecting the Wilderness Area and of providing a network of logging roads almost INTRODUCTION everywhere else. The northeast quadrant of the moun One of the dominating peaks of the Pacific North tain, however, lies within a part of the Yakima Indian west, Mount Adams, stands astride the Cascade crest, Reservation that is open solely to enrolled members of towering 3 km above the surrounding valleys. -
Gifford Pinchot
THE FORGOTTEN FOREST: EXPLORING THE GIFFORD PINCHOT A Publication of the Washington Trails Association1 7A 9 4 8 3 1 10 7C 2 6 5 7B Cover Photo by Ira Spring 2 Table of Contents About Washington Trails Association Page 4 A Million Acres of outdoor Recreation Page 5 Before You Hit the Trail Page 6 Leave No Trace 101 Page 7 The Outings (see map on facing page) 1. Climbing Mount Adams Pages 8-9 2. Cross Country Skiing: Oldman Pass Pages 10-11 3. Horseback Riding: Quartz Creek Pages 12-13 4. Hiking: Juniper Ridge Pages 14-15 5. Backpacking the Pacific Crest Trail: Indian Heaven Wilderness Pages 16-17 6. Mountain Biking: Siouxon Trail Pages 18-19 7. Wildlife Observation: Pages 20-21 A. Goat Rocks Wilderness B. Trapper Creek Wilderness C. Lone Butte Wildlife Emphasis Area 8. Camping at Takhlakh Lake Pages 22-23 9. Fly Fishing the Cowlitz River Pages 24-25 10. Berry Picking in the Sawtooth Berry Fields Pages 26-27 Acknowledgements Page 28 How to Join WTA Page 29-30 Volunteer Trail Maintenance Page 31 Important Contacts Page 32 3 About Washington Trails Association Washington Trails Association (WTA) is the voice for hikers in Washington state. We advocate protection of hiking trails, take volunteers out to maintain them, and promote hiking as a healthy, fun way to explore Washington. Ira Spring and Louise Marshall co-founded WTA in 1966 as a response to the lack of a political voice for Washington’s hiking community. WTA is now the largest state-based hiker advocacy organization in the country, with over 5,500 members and more than 1,800 volunteers. -
White Pass Scenic Byway Road Trip Map
To Buckley To Enumclaw To Puyallup To Tacoma Mt. Rainier NP Carbon River Entrance North Crystal k Scenic Bywa 161 Mountain hinoo y Al Sunrise C (closed in l-A Mowich Lake wi m Mt. Rainier NP nte e r) ri White River ca Entrance n MOUNT RAINIER R S o Eatonville NATIONAL PARK Chinook Pass a 7 e Tr d 410 id ip ) S r Cayuse Pass S e t n i Mount Rainier w Bumping Lake Loop8 A n i d Paradise e 123 s o l c P y ( Elbe Ashford Mt. Rainier NP a Nisqually Mt. Rainier NP WENATCHEE E 706 Entrance T Stevens Canyon e r Entrance Alder Lake id ip NATIONAL FOREST T w S Oak Creek I Mineral Lake H y Wildlife Area W Mineral 3 Naches S Loop Mt. Rainier NP B k a Ohanapecosh c te i C Campground r n ( ee e clo k c se R S d i o n a To Olympia, Tacoma and Seattle T w d de ri in i p te S r) Rimrock Lake Rimrock Centralia Retreat Chehalis 7 2 To Yakima Loop e Tr id ip Packwood White Pass Clear Lake S Ike Kinswa Bevin Lake 7 State Park Loop Matilda Jackson Morton Rest Area Packwood Lake Exit 68 State Park Mayfield Randle To the Salkum Lake To Seattle Pacific Coast Ethel 12 21 164 169 Mossyrock Dam 131 161 REGION Tacoma Enumclaw C Lewis and Clark Cowlitz T h de ri i n Mayfield Glenoma Falls i p Puyallup o o 5 State Park Mossyrock S Greenwater k 97 Ellensburg To Lake Park Park MAP S c e Cowlitz Falls n i Mayfield Dam Mossyrock Taidnapam 7 c B 23 5 Olympia y w a Park Park Campground Loop The White y Riffe Lake Pass Scenic 161 410 Cowlitz Falls Dam Eatonville MOUNT RAINIER 25 Byway connects 5 NATIONAL PARK Toledo e Tr Elbe Ashford 123 id ip 76 Eastern and S e Tr Skate Naches d i Western Centralia Cr i p eek S Walupt Lake Ro 12 Washington, Chehalis ad T Packwood Prosser To 1 de ri Morton Randle Loop i p and is midwayYAKAMA B y w a y Yakima S GIFFORD PINCHOT 6 12 n i c 505 23 c e Loop between Puget Toledo Mossyrock 25 S NATIONAL FOREST INDIAN Coast Pacific and Olympic the Peninsula To W s s 4 Sound and the 505 h i t e P a 76 Loop (Most roads in this area are 23 MOUNT ST. -
Elk Pass Obsidian and Pre-Contact Band Territory in the Southern Washington Cascades
CHAPTER 7 Elk Pass Obsidian and Pre-contact Band Territory in the Southern Washington Cascades Rick McClure U.S. Forest Service, Gifford Pinchot National Forest ([email protected]) At the landscape level, the embedded procurement strategies of hunter-gatherer-foragers may produce archaeological distributions of toolstone material COPPER RIDGE that reflect the home ranges or territories of a specific group or band. Over the past decade, a AGNES CREEK number of studies have addressed this subject, CHELAN BUTTE among them the work of Jones and Beck (2003), STRAY GULCH looking at obsidian as an indicator of foraging PARKE CREEK territory in the Great Basin. Another study, by CLEMAN MNT Brantingham (2003), proposed that the maximum ELK PASS NASTY CREEK transport distances of given raw material types are INDIAN ROCK SATUS CREEK equivocally related to the geographic range of a HOSKO BICKLETON RIDGE forager group. The utilization range of obsidian from the Elk Pass geochemical source in Figure 7-1. Washington obsidian sources. Washington State provides a case study and Adapted from “Washington Obsidian Sources” application of these principles from the by Northwest Research Obsidian Studies southwestern section of the Plateau region of the Laboratory (2009). Base orthophoto courtesy U.S. Pacific Northwest. U.S. Geological Survey. Located in the southern Washington Cascade Mountain Range, 125 km southeast of Seattle, the 1999). In contrast, the archaeological distribution Elk Pass source location is one of only 12 of obsidian from the Elk Pass source is limited to a documented geological sources of obsidian distance of only 52 km from the geological source. -
Geologic Map of the Blue Lake Quadrangle, Southern Cascade Range, Washington
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Geologic map of the Blue Lake quadrangle, southern Cascade Range, Washington by Donald A. Swanson1 Open-File Report 93-297 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1U.S. Geological Survey, Department of Geological Sciences AJ-20, University of Washington, Seattle, Washington 98195 CONTENTS INTRODUCTION ....................... 1 3. Total alkali-silica classification diagram for ACKNOWLEDGMENTS .................. 1 rocks in Blue Lake quadrangle .......... 3 ROCK TERMINOLOGY AND CHEMICAL 4. Plot of phenocryst assemblage vs. SiO2 for CLASSIFICATION .................... 3 rocks in Blue Lake quadrangle .......... 4 GEOLOGIC OVERVIEW OF QUADRANGLE . 7 5. Locations of samples collected in Blue Lake TERTIARY ROCKS OLDER THAN INTRUSIVE quadrangle ........................ 4 SUITE OF KIDD CREEK ............... 8 6. Alkali-lime classification diagram for Tertiary Volcaniclastic rocks .................... 8 rocks in Blue Lake quadrangle .......... 4 Diamictite below Castle Butte ........... 8 7. Plot of FeO*/MgO vs. SiO2 for rocks from Blue Depositional environment ............. 10 Lake quadrangle .................... 7 Lava flows ......................... 11 8. Plot of total alkalies vs. SiO2 for rocks from Intrusive andesite and basaltic andesite ...... 11 Blue Lake quadrangle ................ 7 Dikes ........................... 12 9. Plot of KjO vs. SiO2 for rocks from Blue Lake INTRUSIVE SUITE OF KIDD CREEK ....... 14 quadrangle ........................ 7 STRUCTURE ......................... 16 10. Distribution of pyroxene andesite and basaltic Folds ............................. 16 andesite dikes in Blue Lake, French Butte, Faults and shear zones ................ -
Forest Development Following Mudflow Deposition, Mount St. Helens, Washington
437 Forest development following mudflow deposition, Mount St. Helens, Washington Marc H. Weber, Keith S. Hadley, Peter M. Frenzen, and Jerry F. Franklin Abstract: Volcanic mudflows are locally important disturbance agents in the Pacific Northwest rarely studied within the context of forest succession. We describe 18 years (1981–1999) of forest development on the Muddy River mud- flow deposit following the 1980 eruption of Mount St. Helens using permanent plot data collected along two transects traversing the Cedar Flats river terrace. We analyze changing forest structure over the study period and compare results with mudflow deposition using correlation and pairwise comparisons, as well as ordination (detrended correspondence analysis) and cluster analysis. Our results show a statistically significant relationship between mudflow deposition and forest change. Following mudflow deposition, the site consisted of patches of high tree mortality caused by deep mudflow deposits in abandoned river channels as well as patches of accelerated regeneration of surviving understory trees in areas of more shallow mudflow deposition and partial overstory mortality. Mudflow deposition at the site initiated multiple stages of stand development with (1) early-colonizing red alder (Alnus rubra Bong.) dominating deep deposition sites with fewer surviving trees, (2) gap recruitment and establishment by western hemlock (Tsuga heterophylla (Raf.) Sarg.) and Douglas- fir (Pseudotsuga menziesii (Mirb.) Franco) on intermediate to deep deposition sites with more postburial surviving trees, and (3) late-seral conditions and accelerated succession on shallow burial sites, where tree mortality was low. The initia- tion of differing succession trajectories, as well as variability in the extent and timing of tree mortality following mudflow deposition, demonstrates a dynamic response to disturbance in relation to small-scale gradients of mudflow deposition. -
(Washington Geology), V. 15, No. 4, October 1987
WASHINGTON GEOLOGIC NEWSLETTER Volume 15 Number 4 October 1987 Washington State Department of Natural Resources Division of Geology and Earth Resources View west of a climber descending the 8,365-foot summit of Mount St. Helens. The mountain was recent ly re-opened to mountaineers by the U.S . Forest Service. Clouds of ash from debris avalanches obscure the crater walls. (See article, p. 3.) IN THIS ISSUE Geologic guide to the Monitor Ridge climbing route, Mount St. Helens.................................................... p. 3 Pacific Northwest AGU Meeting ................................ p. 15 New U.S. Geological Survey projects in Washington ............................................................ p. 18 WASHINGTON Mount St. Helens Scientific Advisory Board GEOLOGIC NEWSLETTER by Ray Lasmanis The Washington Geologic Newsletter is published quarterly by the Division of Geology and Earth Resources, Department of Natural Resources. The newsletter is The Mount St. Helens Scientific Advisory Board was es free upon request. The Division also publishes bulletins, information circulars, re tablished in 1983 to comply with Section 7 of Public Law ports of investigations, and geologic maps. A list of these publications will be sent upon request. 97-243, an act passed by the 97th Congress, designating the Mount St. Helens National Volcanic Monument. The DEPARTMENT Brian J. Boyle provisions of Section 7 are: OF Commissioner of Public Lands NATURAL Art Stearns Sec. 7. (a) There is hereby established the Mount St. RESOURCES Supervisor Helens S cientijic Advisory Board ( hereinafter referred to as the "Board"). The Secretary [of Agriculture] shall consult Raymond Lasmanis DIVISION OF with and seek the advice and recommendations of the GEOLOGY AND State Geologist EARTH RESOUH.CES J. -
High Lakes Loop Road Trip Itinerary
Itinerary: High Lakes Loop Length: 79 miles Time to Allow: 4 hours Open Season: The route is usually snow-free by the end of May and remains open through October. The road closes each year due to winter snowfall from November to May. Driving Directions: From Randle, travel south on State Route (SR) 131 for 1 mile to FR23. Stay left on FR23. Follow FR23 31.2 miles to FR2329 and turn left on FR2329. Follow FR2329 9.8 miles to FR5603 and turn left on FR5603. Follow FR5603 5.2. miles to FR 56 and turn right on FR56. Follow FR56 7 miles to FR2160. From here turn right for a 7 mile round trip drive to Walupt Lake and back. Turn left on 2160 and follow FR2160 1.8 miles to FR21 and turn right. Follow FR21 15.9 miles north to US 12, about 3 miles west of Packwood and 13.6 miles east of the beginning of the route in Randle. Discover the numerous majestic alpine lakes that create this unique and beautiful landscape. Towering Mt. Adams and the Gifford Pinchot National Forest provide the backdrop for this scenic drive offering opportunities for fabulous hiking and great fishing along the way . Start: This journey begins in the small mountain community of Randle located on Highway 12. Restaurants, vehicle and RV services, and campgrounds are available. Stop 1: Cispus River Valley Meandering along FR23, stop in at the densely forested North Fork Campground Day Use Area situated on the North Cispus River. Providing access to the Cispus River Valley, this is a popular area for hiking, biking, and fishing. -
Lahar Deposits
Chapter 3—Lahar Deposits CHAPTER 3 Lahar Deposits L. C. Bliss leans against a surviving Douglas fir on the edge of the Muddy River Lahar. The scour marks are 8 m above the deposit (July 1980). What is a lahar? caught in the path, and severely erodes the canyon mar- Lahars, from a Javanese (Indonesia) designation, are pre- gins. Similar events can occur by heating from within, as ferred to the inelegant English term “mudflow” when re- hot magma moves into the cone. As a lahar ebbs, it usually ferring to events on volcanoes. Lahars include any rapidly leaves a deposit of sediments sorted by distance from its flowing masses of earth saturated by water flowing under origin. the force of gravity. They can be triggered when natural A lahar can also form as a debris avalanche hurtles from rubble dams collapses to unleash a pent-up lake trapped a volcano entraining everything in its path. As it becomes behind it. Lahars are mudflows formed in several ways by increasingly liquid, leaving larger materials behind, the de- volcanism. When hot tephra falls onto a cone laden with bris avalanche becomes a less turbulent and continues to snow and ice, the rapid melting causes lahars that flow flow as a lahar. While lahars usually stay confined to the down canyons. Slurries entrain soil, rocks and anything river channel, they can overflow their constraints and spread 27 Chapter 3—Lahar Deposits ago, the flanks of Mt. Rainier collapsed producing a cata- clysmic event. There was no eruption, but over the millen- nia, the summit rock of the then much higher cone was re- peatedly heated and cooled, becoming “rotten” (or as geol- ogists say, hydrothermally altered). -
Roadside Geology of Mount St. Helens National Volcanic Monument and Vicinity
ROADSIDE GEOLOGY OF MOUNT ST. HELENS NATIONAL VOLCANIC MONUMENT AND VICINITY by Patrick T. Pringle WASHINGTON DEPARTMENT OF NATURAL RESOURCES Division of Geology and Earth Resources Information Circular 88 1993 [Revised Edition 2002] Shaded relief map of the Mount St. Helens area showing areas affected by1980 eruption processes. The image was created from 30 m digital elevation data. ROADSIDE GEOLOGY OF MOUNT ST. HELENS NATIONAL VOLCANIC MONUMENT AND VICINITY by Patrick T. Pringle WASHINGTON STATE DEPARTMENTOF Natural Resources Doug Sutherland - Commissioner of Public Lands Washington Division of Geology and Earth Resources Information Circular 88 1993 [Revised Edition 2002) WASHINGTON DEPARTMENT OF NATURAL RESOURCES Doug Sutherland-Commissioner of Public Lands DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere-State Geologist This publication is available from: Publication Sales 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 (360) 902-1450 or e-mail [email protected]. Also see our website at http://www.wa.gov/dnr/htdocs/ger / This book is also available through the Mount St. Helens visitors centers courtesy of the Mount St. Helens Institute. For more information on how you can get involved in ongoing support of research and education at Mount St. Helens, contact: Mount St. Helens Institute PO Box 820762 Vancouver, WA 98682-0017 (360) 891-5206 www.mshinstitute.org Front Cover. Mount St. Helens from the north shore of Spirit Lake, about 7 mi (11 km) north-northeast of the crater. Photo taken in 1982 by Lyn Topinka, U.S.