Opportunities for Wild & Scenic River Designation In
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GEOLOGIC MAP of the Mccoy PEAK QUADRANGLE, SOUTHERN CASCADE RANGE, WASHINGTON
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Geologic map of the McCoy Peak quadrangle, southern Cascade Range, Washington by Donald A. Swanson1 Open-File Report 92-336 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. 'U.S. Geological Survey, Department of Geological Sciences AJ-20, University of Washington, Seattle, Washington 98195 CONTENTS INTRODUCTION ........................ 1 5. Locations of samples collected in McCoy Peak ACKNOWLEDGMENTS ................... 1 {quadrangle ......................... 6 ROCK TERMINOLOGY AND CHEMICAL 6. Alkali-lime classification diagram for Tertiary CLASSIFICATION .................... 2 rocks in McCoy Peak quadrangle .......... 7 GENERAL GEOLOGY .................... 6 7. Plot of FeO*/MgO vs. SiO2 for rocks from TERTIARY ROCKS OLDER THAN INTRUSIVE McCoy Peak quadrangle ................ 7 SUITE OF KIDD CREEK ............... 7 8. Plot of total alkalis vs. SiO2 for rocks in McCoy Volcaniclastic rocks ................... 7 Peak quadrangle ..................... 8 Chaotic volcanic breccia ................ 8 9. Plot of K2O vs. SiO2 for rocks from McCoy Vitroclastic dacite and andesite breccia ...... 9 Peak quadrangle ..................... 8 Volcanic centers ...................... 10 10. Distrbution of pyroxene andesite and basaltic Regional dike swarm .................. 11 andesite dikes in French Butte, Greenhorn Age .............................. 13 Buttes, Tower Rock, and McCoy Peak INTRUSIVE SUITE OF KIDD CREEK ......... 13 quadrangles ........................ 12 Dikes ............................. 14 11. Rose diagrams of strikes of dikes and beds in Sills .............................. 16 McCoy Peak and other quadrangles ....... 13 Relation of dikes and sills ............... 16 12. Plcts of TiO2, FeO*, and MnO vs. -
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. -
Roadless Rule and Dark Divide the Dark Divide Was Once Much Larger Than Its Current 76,000 Acres
Exploring the PRING S RA Dark Divide I Despite its intimidating name, the Dark Divide is a place of sunny ridges and tremendous wildflower meadows. The region is endangered, however, by threats from off-road vehicle use. Southwest Washington’s threatened gem By Andrew Engelson soils and meadows. The region was A thick layer of ash from the 1980 excluded from the protections of the eruption of Mount St. Helens is still Don’t be afraid of the Dark Divide. 1984 Washington Wilderness Bill. prominent. Even with a somewhat ominous But hikers are slowly reclaiming the The region is home to a variety of name, this spectacular roadless area ridges with their boots. And there are forest ecosystems, all dependent on between Mount St. Helens and Mt. many reasons to go: unique geology, wildfires. Huge wildfires in the early Adams is actually filled with light: sun- abundant wildflowers and wildlife, 1900s left many of the open meadows baked ridges, subalpine forests, and and superb views. and silver-gray snags you’ll find there meadows exploding with wildflowers. The lava flows that are the founda- today. Even so, the region is home to Named for the 19th century miner tion of the 76,000-acre region are huge trees. Just outside the Dark and settler John Dark, the Dark approximately 20 to 25 million years Divide roadless area, you can find the Divide long served as hunting and old. Areas such as Juniper and world’s largest noble fir, near gathering grounds for American Langille Ridge were actually once Yellowjacket Creek. -
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. -
Lewis River ~ Including Clear, Quartz, Siouxon, Pine, Rush, Smith Creeks & the Muddy River
Photo by Susan Saul Wild and Scenic Rivers Support Local Communities The legendary volcanoes in southwestern Washington and the spectacular rivers that originate on their slopes are valuable to the health, economy, and cultural identity of local communities. Rivers like the Green, Cispus, and Lewis provide drinking water to thousands of local residents, world-class recreation, and a high quality of life for local residents. Designating the rivers and key tributaries in Volcano Country under the Wild and Scenic Rivers Act will increase long- term potential for recreation and tourism in the area, ensure cool clean water for fish and people, and protect these natural treasures for future generations. Just a few of the benefits of Wild and Scenic designation include: RECREATION, TOURISM, AND THE ECONOMY: According to the Outdoor Industry Association, outdoor recreation brings in more than $11.7 billion annually to our state, supports an estimated 115,000 jobs, and generates $650 million in annual sales tax revenue. Travel and tourism provide nearly 8000 jobs – or 14 percent of jobs across all economic sectors – in Lewis, Cowlitz, and Skamania counties. In addition to putting a river “on the map” for visitors and outdoor enthusiasts, a Wild and Scenic River designation can lead to access improvements and foster growth in river-based outdoor recreation and tourism. For example, a recent study of the Wild and Scenic section of the Rogue River found that commercial rafting, fishing, and other recreation contributed $30 million a year to the State of Oregon’s economy. The White Salmon and the Klickitat River are two positive examples of Wild and Scenic Rivers in Washington that benefit local recreation economies. -
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. -
Summary of Public Comment, Appendix B
Summary of Public Comment on Roadless Area Conservation Appendix B Requests for Inclusion or Exemption of Specific Areas Table B-1. Requested Inclusions Under the Proposed Rulemaking. Region 1 Northern NATIONAL FOREST OR AREA STATE GRASSLAND The state of Idaho Multiple ID (Individual, Boise, ID - #6033.10200) Roadless areas in Idaho Multiple ID (Individual, Olga, WA - #16638.10110) Inventoried and uninventoried roadless areas (including those Multiple ID, MT encompassed in the Northern Rockies Ecosystem Protection Act) (Individual, Bemidji, MN - #7964.64351) Roadless areas in Montana Multiple MT (Individual, Olga, WA - #16638.10110) Pioneer Scenic Byway in southwest Montana Beaverhead MT (Individual, Butte, MT - #50515.64351) West Big Hole area Beaverhead MT (Individual, Minneapolis, MN - #2892.83000) Selway-Bitterroot Wilderness, along the Selway River, and the Beaverhead-Deerlodge, MT Anaconda-Pintler Wilderness, at Johnson lake, the Pioneer Bitterroot Mountains in the Beaverhead-Deerlodge National Forest and the Great Bear Wilderness (Individual, Missoula, MT - #16940.90200) CLEARWATER NATIONAL FOREST: NORTH FORK Bighorn, Clearwater, Idaho ID, MT, COUNTRY- Panhandle, Lolo WY MALLARD-LARKINS--1300 (also on the Idaho Panhandle National Forest)….encompasses most of the high country between the St. Joe and North Fork Clearwater Rivers….a low elevation section of the North Fork Clearwater….Logging sales (Lower Salmon and Dworshak Blowdown) …a potential wild and scenic river section of the North Fork... THE GREAT BURN--1301 (or Hoodoo also on the Lolo National Forest) … harbors the incomparable Kelly Creek and includes its confluence with Cayuse Creek. This area forms a major headwaters for the North Fork of the Clearwater. …Fish Lake… the Jap, Siam, Goose and Shell Creek drainages WEITAS CREEK--1306 (Bighorn-Weitas)…Weitas Creek…North Fork Clearwater. -
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 ................ -
Cascade Forest Conservancy 2020 Annual Report
Cascade Forest Conservancy 2020 Annual Report Three months and ten days into our 35th year as an organization, the Board of Directors and I decided to ask our staff to work from home. At the time, we all hoped to come back to the office within a month. Two months seemed like a worst-case scenario. As I write this, we are still working remotely. At the beginning of 2020, none of us anticipated how different and how tough the year would be. Yet Cascade Forest Conservancy showed remarkable resilience at every level of our organization. Our staff continued to fight to protect and restore the southern Washington Cascades. Our Board continued to provide direction and leadership. And our community of volunteers, supporters, and donors showed up, again and again, to keep Cascade Forest Conservancy strong. Despite many challenges, we moved forward undeterred. We continued to fight to protect places like the Pumice Plain and the Green River Valley from harmful projects and mining. We expanded some ongoing restoration programs, like beaver reintroduction, and launched new ground-breaking projects like the Instream Wood Bank Network (instreamwoodbanknetwork.com). And we hosted successful online events to build community and support our work at a distance, such as our annual auction and screenings of documentaries and films like The Dark Divide. Many volunteer trips were reimagined to keep volunteers and staff safe from COVID-19. Our 2020 volunteers put on masks, stood far apart, and came out to donate their time and energy to important conservation and restoration initiatives that wouldn’t have been possible without their help.