30 Day Notice of Availability – Draft Integrated Detailed Project Report and Environmental Assessment
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Geologic Map of the Simcoe Mountains Volcanic Field, Main Central Segment, Yakama Nation, Washington by Wes Hildreth and Judy Fierstein
Prepared in Cooperation with the Water Resources Program of the Yakama Nation Geologic Map of the Simcoe Mountains Volcanic Field, Main Central Segment, Yakama Nation, Washington By Wes Hildreth and Judy Fierstein Pamphlet to accompany Scientific Investigations Map 3315 Photograph showing Mount Adams andesitic stratovolcano and Signal Peak mafic shield volcano viewed westward from near Mill Creek Guard Station. Low-relief rocky meadows and modest forested ridges marked by scattered cinder cones and shields are common landforms in Simcoe Mountains volcanic field. Mount Adams (elevation: 12,276 ft; 3,742 m) is centered 50 km west and 2.8 km higher than foreground meadow (elevation: 2,950 ft.; 900 m); its eruptions began ~520 ka, its upper cone was built in late Pleistocene, and several eruptions have taken place in the Holocene. Signal Peak (elevation: 5,100 ft; 1,555 m), 20 km west of camera, is one of largest and highest eruptive centers in Simcoe Mountains volcanic field; short-lived shield, built around 3.7 Ma, is seven times older than Mount Adams. 2015 U.S. Department of the Interior U.S. Geological Survey Contents Introductory Overview for Non-Geologists ...............................................................................................1 Introduction.....................................................................................................................................................2 Physiography, Environment, Boundary Surveys, and Access ......................................................6 Previous Geologic -
1961 Climbers Outing in the Icefield Range of the St
the Mountaineer 1962 Entered as second-class matter, April 8, 1922, at Post Office in Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and December by THE MOUNTAINEERS, P. 0. Box 122, Seattle 11, Wash. Clubroom is at 523 Pike Street in Seattle. Subscription price is $3.00 per year. The Mountaineers To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of Northwest America; To make expeditions into these regions in fulfillment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor Zif e. EDITORIAL STAFF Nancy Miller, Editor, Marjorie Wilson, Betty Manning, Winifred Coleman The Mountaineers OFFICERS AND TRUSTEES Robert N. Latz, President Peggy Lawton, Secretary Arthur Bratsberg, Vice-President Edward H. Murray, Treasurer A. L. Crittenden Frank Fickeisen Peggy Lawton John Klos William Marzolf Nancy Miller Morris Moen Roy A. Snider Ira Spring Leon Uziel E. A. Robinson (Ex-Officio) James Geniesse (Everett) J. D. Cockrell (Tacoma) James Pennington (Jr. Representative) OFFICERS AND TRUSTEES : TACOMA BRANCH Nels Bjarke, Chairman Wilma Shannon, Treasurer Harry Connor, Vice Chairman Miles Johnson John Freeman (Ex-Officio) (Jr. Representative) Jack Gallagher James Henriot Edith Goodman George Munday Helen Sohlberg, Secretary OFFICERS: EVERETT BRANCH Jim Geniesse, Chairman Dorothy Philipp, Secretary Ralph Mackey, Treasurer COPYRIGHT 1962 BY THE MOUNTAINEERS The Mountaineer Climbing Code· A climbing party of three is the minimum, unless adequate support is available who have knowledge that the climb is in progress. -
Indian Artifacts of the Columbia River Priest
IINNDDIIAANN AARRTTIIFFAACCTTSS OOFF TTHHEE CCOOLLUUMMBBIIAA RRIIVVEERR PPRRIIEESSTT RRAAPPIIDDSS TTOO TTHHEE CCOOLLUUMMBBIIAA RRIIVVEERR GGOORRGGEE IIIDDDEEENNNTTTIIIFFFIIICCCAAATTTIIIOOONNN GGGUUUIIIDDDEEE VVVOOOLLLUUUMMMEEE 111 DDDaaavvviiiddd HHHeeeaaattthhh Copyright 2003 All rights reserved. This publication may only be reproduced for personal and educational use. SSSCCCOOOPPPEEE This document is used to define projectile point typologies common to the Columbia Plateau, covering the region from Priest Rapids to the Columbia Gorge. When employed, recognition of a specified typology is understood as define within the body of this document. This document does not intend to cover, describe or define all typologies found within the region. This document will present several recognized typologies from the region. In several cases, a typology may extend beyond the Columbia Plateau region. Definitions are based upon research and records derived from consultation with; and information obtained from collectors and authorities. They are subject to revision as further experience and investigation may show is necessary or desirable. This document is authorized for distribution in an electronic format through selected organizations. This document is free for personal and educational use. RRREEECCCOOOGGGNNNIIITTTIIIOOONNN A special thanks for contributions given to: Ben Stermer - Technical Contributions Bill Jackson - Technical Contributions Joel Castanza - Images Mark Berreth - Images, Technical Contributions Randy McNeice - Images Rodney Michel -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
Chapter 11. Mid-Columbia Recovery Unit Yakima River Basin Critical Habitat Unit
Bull Trout Final Critical Habitat Justification: Rationale for Why Habitat is Essential, and Documentation of Occupancy Chapter 11. Mid-Columbia Recovery Unit Yakima River Basin Critical Habitat Unit 353 Bull Trout Final Critical Habitat Justification Chapter 11 U. S. Fish and Wildlife Service September 2010 Chapter 11. Yakima River Basin Critical Habitat Unit The Yakima River CHU supports adfluvial, fluvial, and resident life history forms of bull trout. This CHU includes the mainstem Yakima River and tributaries from its confluence with the Columbia River upstream from the mouth of the Columbia River upstream to its headwaters at the crest of the Cascade Range. The Yakima River CHU is located on the eastern slopes of the Cascade Range in south-central Washington and encompasses the entire Yakima River basin located between the Klickitat and Wenatchee Basins. The Yakima River basin is one of the largest basins in the state of Washington; it drains southeast into the Columbia River near the town of Richland, Washington. The basin occupies most of Yakima and Kittitas Counties, about half of Benton County, and a small portion of Klickitat County. This CHU does not contain any subunits because it supports one core area. A total of 1,177.2 km (731.5 mi) of stream habitat and 6,285.2 ha (15,531.0 ac) of lake and reservoir surface area in this CHU are proposed as critical habitat. One of the largest populations of bull trout (South Fork Tieton River population) in central Washington is located above the Tieton Dam and supports the core area. -
Suggested Fishing Destinations in Central Washington the Yakima
Suggested Fishing Destinations in Central Washington Always refer to the WDFW Fishing Regulation Pamphlet prior to fishing any of these streams. Most of these are within an easy drive of Red’s Fly Shop, or even a day trip from the Puget Sound area. The east slopes of the Cascades are regarded as the best small stream fishing in Washington State and a GREAT place to start as a beginner! Most of the fisheries here offer small trout in abundance, which is great adventure and perfect for learning the art of fly fishing. The Yakima River Canyon The Canyon near Red’s Fly Shop is best wade fished when the river flows are below 2,500 cfs. September and October are the best months for wading, but February and March can offer great bank access as well. Spring and summer are more challenging but still possible. Yakima County Naches River – Trout tend to be most abundant upstream from the Tieton River junction. The best wade fishing season is July – October Tieton River – It runs fairly dirty in June, but July – mid August is excellent. Rattlesnake Creek – This is a great hike in adventure and offers wonderful small stream Cutthroat fishing for anyone willing to get off the beaten path. Little Naches River – Easy access off of USFS Road 19, July – October is the best time. American River/Bumping Rivers – These are in the headwaters of the Naches drainage. Be sure to read the WDFW Regulations if you fish the American River. Ahtanum Creek – Great small stream fishing. June – October Wenas Creek – Small water, small fish, but a great adventure. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
Caves, Denuded Caves and Collapse Dolines As Past Hydrological Pattern Indicators of the Grabovica Plateau, the Dinaric Karst (Bosnia and Herzegovina)
RAZPRAVE Dela 49 ● 2018 ● 95–111 CAVES, DENUDED CAVES AND COLLAPSE DOLINES AS PAST HYDROLOGICAL PATTERN INDICATORS OF THE GRABOVICA PLATEAU, THE DINARIC KARST (BOSNIA AND HERZEGOVINA) Uroš Stepišnik*, PhD., Aleš Grlj** *Department of Geography, Faculty of Arts, University of Ljubljana, Aškerčeva 2, 1000 Ljubljana ** Institute of Anthropological and Spatial Studies, ZRC SAZU, Novi trg 2, SI-1000 Ljubljana e-mail: [email protected], [email protected] Original scientific article COBISS 1.01 DOI: 10.4312/dela.49.95-111 Abstract The Grabovica Plateau is a corrosion plain in southern Bosnia and Herzegovina. The whole area is characterised by a through-flow karst system, where subsurface streams submerging at Duvanjsko polje are directed towards springs at Livanjsko polje. In this study, we conducted morphographic and morphometric investigation of surface and sub- surface features, especially collapse dolines, denuded caves along with active and inactive cave systems. We interpreted morphogenesis and past hydrologic pattern within the area. Keywords: collapse doline, denuded cave, geomorphology, speleology, hydrology JAME, DENUDIRANE JAME IN UDORNICE KOT KAZALNIKI NEKDA- NJEGA HIDROLOŠKEGA DELOVANJA PLANOTE GRABOVICA (BO- SNIA IN HERCEGOVINA) Izvleček Planota Grabovica je korozijska uravnava v južnem delu Bosne in Hercegovine. Za celot- no območje je značilen pretočni kras, kjer podzemni tokovi, ki ponikajo na Duvanjskem polju, odtekajo v smeri izvirov na Livanjskem polju. V tej raziskavi smo izdelali mor- fografske in morfometrične analize površinskih in podzemskih oblik, predvsem udornic, denudiranih jam ter aktivnih in reliktnih jamskih sistemov. Interpretirali smo morfogene- zo in preteklo hidrološko delovanje proučevanega območja. Ključne besede: udornica, denudirana jama, geomorfologija, speleologija, hidrologija 95 Dela_49_FINAL.indd 95 21.12.2018 11:16:28 Uroš Stepišnik, Aleš Grlj / Dela 49 ● 2018 ● 95–111 1 INTRODUCTION The Dinaric Alps are located in the western Balkan Peninsula almost parallel to the east- ern Adriatic coast. -
Cosmogenic Age Constraints on Post-LGM Catastrophic Rock Slope Failures in the Tatra Mountains (Western Carpathians)
Catena 138 (2016) 52–67 Contents lists available at ScienceDirect Catena journal homepage: www.elsevier.com/locate/catena Cosmogenic age constraints on post-LGM catastrophic rock slope failures in the Tatra Mountains (Western Carpathians) Tomáš Pánek a,ZbyněkEngelb, Pavel Mentlík c,⁎, Régis Braucher d,MichalBřežný a, Václav Škarpich a,AlbertZondervane a Department of Physical Geography and Geoecology, Faculty of Science, University of Ostrava, Chittussiho 10, 710 00 Ostrava, Czech Republic b Department of Physical Geography and Geoecology, Charles University in Prague, Albertov 6, 12843 Praha, Czech Republic c Centre of Biology, Geoscience and Environmental Education, University of West Bohemia, Plzeň, Czech Republic d Aix-Marseille Université, CEREGE, CNRS UM 34, F-13545 Aix-en-Provence, France e Environment and Materials Division, GNS Science, Lower Hutt, New Zealand article info abstract Article history: Although deglaciation is one of the crucial factors controlling the stability of slopes in high mountains, the chro- Received 30 June 2015 nological response of rock slope failure (RSF) to glacier retreat still remains poorly known. Here we provide the Received in revised form 19 October 2015 first cosmogenic (10Be) age constraints on prominent rock avalanches and rockfalls (collectively termed ‘rock Accepted 10 November 2015 slope failures’–RSFs) from the Tatra Mountains, the highest mountain range with the most pronounced glacier Available online xxxx morphology within the Carpathians. Six representative RSFs were selected for surface exposure dating in the Keywords: mountain range. Two sites are situated in the western part with less pronounced local relief and gentler slope Rock slope failures gradient, and four come from the highest eastern part with oversteepened rock slopes. -
A Guide to the Geology of Rocky Mountain National Park, Colorado
A Guide to the Geology of ROCKY MOUNTAIN NATIONAL PARK COLORADO For sale by the Superintendent of Documents, Washington, D. C. Price 15 cents A Guide to the Geology of ROCKY MOUNTAIN NATIONAL PARK [ COLORADO ] By Carroll H. Wegemann Former Regional Geologist, National Park Service UNITED STATES DEPARTMENT OF THE INTERIOR HAROLD L. ICKES, Secretary NATIONAL PARK SERVICE . NEWTON B. DRURY, Director UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1944 Table of Contents PAGE INTRODUCTION in BASIC FACTS ON GEOLOGY 1 THE OLDEST ROCKS OF THE PARK 2 THE FIRST MOUNTAINS 3 The Destruction of the First Mountains 3 NATURE OF PALEOZOIC DEPOSITS INDICATES PRESENCE OF SECOND MOUNTAINS 4 THE ROCKY MOUNTAINS 4 Time and Form of the Mountain Folding 5 Erosion Followed by Regional Uplift 5 Evidences of Intermittent Uplift 8 THE GREAT ICE AGE 10 Continental Glaciers 11 Valley Glaciers 11 POINTS OF INTEREST ALONG PARK ROADS 15 ROAD LOGS 18 Thompson River Entrance to Deer Ridge Junction 18 Deer Ridge Junction to Fall River Pass via Fall River .... 20 Fall River Pass to Poudre Lakes 23 Trail Ridge Road between Fall River Pass and Deer Ridge Junction 24 Deer Ridge Junction to Fall River Entrance via Horseshoe Park 29 Bear Lake Road 29 ILLUSTRATIONS LONGS PEAK FROM BEAR LAKE Front and back covers CHASM FALLS Inside back cover FIGURE PAGE 1. GEOLOGIC TIME SCALE iv 2. LONGS PEAK FROM THE EAST 3 3. PROFILE SECTION ACROSS THE ROCKY MOUNTAINS 5 4. ANCIENT EROSIONAL PLAIN ON TRAIL RIDGE 6 5. ANCIENT EROSIONAL PLAIN FROM FLATTOP MOUNTAIN ... 7 6. VIEW NORTHWEST FROM LONGS PEAK 8 7. -
Oregon Geography
Oregon Geography 4th Grade Social Studies Medford School District 549c Created by: Anna Meunier and Sarah Flora Oregon Geography 4th Grade Social Studies Medford School District 549c Table of Contents Oregon Geography Unit Syllabus ........................................................................ 1 Oregon Geography Unit Objectives ..................................................................... 2 Oregon Geography Unit Lesson Plans.................................................................. 3 Print Shop Order ................................................................................................. 4 Oregon Geography Unit Lessons ......................................................................... 6 Oregon Geography Daily Lessons ...................................................................... 19 Lesson #1 ........................................................................................................................................ Lessons #2 & #3 .............................................................................................................................. Lesson #4 ........................................................................................................................................ Lesson #5 ........................................................................................................................................ Lesson #6 ....................................................................................................................................... -
A Geomorphic Classification System
A Geomorphic Classification System U.S.D.A. Forest Service Geomorphology Working Group Haskins, Donald M.1, Correll, Cynthia S.2, Foster, Richard A.3, Chatoian, John M.4, Fincher, James M.5, Strenger, Steven 6, Keys, James E. Jr.7, Maxwell, James R.8 and King, Thomas 9 February 1998 Version 1.4 1 Forest Geologist, Shasta-Trinity National Forests, Pacific Southwest Region, Redding, CA; 2 Soil Scientist, Range Staff, Washington Office, Prineville, OR; 3 Area Soil Scientist, Chatham Area, Tongass National Forest, Alaska Region, Sitka, AK; 4 Regional Geologist, Pacific Southwest Region, San Francisco, CA; 5 Integrated Resource Inventory Program Manager, Alaska Region, Juneau, AK; 6 Supervisory Soil Scientist, Southwest Region, Albuquerque, NM; 7 Interagency Liaison for Washington Office ECOMAP Group, Southern Region, Atlanta, GA; 8 Water Program Leader, Rocky Mountain Region, Golden, CO; and 9 Geology Program Manager, Washington Office, Washington, DC. A Geomorphic Classification System 1 Table of Contents Abstract .......................................................................................................................................... 5 I. INTRODUCTION................................................................................................................. 6 History of Classification Efforts in the Forest Service ............................................................... 6 History of Development .............................................................................................................. 7 Goals