Rock Glaciers in the Eastern Cascades, Washington
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Mount Rainier National Park
MOUNT RAINIER NATIONAL PARK • WASHINGTON • UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL PARK SERVICE Mount Rainier [WASHINGTON] National Park United States Department of the Interior Harold L. Ickes, Secretary NATIONAL PARK SERVICE Arno B. Cammerer, Director UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1936 Rules and Regulations [BRIEFED] Events kjERVING a dual purpose, park regulations are designed for the comfort and convenience of visitors as well as for the protection of natural beauties OF HISTORICAL IMPORTANCE and scenery. The following synopsis is for the guidance of visitors, who are requested to assist the park administration by observing the rules. Complete rules and regulations may be seen at the superintendent's office 1792 May 8. The first white man to sec "The Mountain" (Capt. and at ranger stations. George Vancouver, of the Royal English Navy) sighted Fires. the great peak and named it Mount Rainier. Light carefully and in designated places. Extinguish COMPLETELY before leaving 1833 September 2. Dr. William Eraser Tolmie of Nisqually camp, even for temporary absence. Do not guess your fire is out—KNOW it. Do not House, a Hudson's Bay post, entered the northwest corner throw burning tobacco or matches on road or trail sides. of what is now the park. He was the first white man to penetrate this region. Camps. Keep your camp clean. As far as possible burn garbage in camp fire, and empty 1857 July. Lieut. A. V. Kautz, of the United States Army garri son at Fort Steilacoom, and four companions made the cans and residue into garbage cans provided. If no can is provided, bury the refuse. -
Local Topography Increasingly Influences the Mass Balance of A
Local topography increasingly influences the mass balance of a retreating cirque glacier Caitlyn Florentine1, 2, Joel Harper2, Daniel Fagre1, Johnnie Moore2, Erich Peitzsch1 1U.S. Geological Survey, Northern Rocky Mountain Science Center, West Glacier, Montana, 59936, USA 5 2Department of Geosciences, University of Montana, Missoula, Montana, 59801, USA Correspondence to: Caitlyn Florentine ([email protected]) Abstract. Local topographically driven processes, such as wind drifting, avalanching, and shading, are known to alter the relationship between the mass balance of small cirque glaciers and regional climate. Yet partitioning such local effects from regional climate influence has proven difficult, creating uncertainty in the climate representativeness of some glaciers. We 10 address this problem for Sperry Glacier in Glacier National Park, USA using field-measured surface mass balance, geodetic constraints on mass balance, and regional climate data recorded at a network of meteorological and snow stations. Geodetically derived mass changes between 1950-1960, 1960-2005, and 2005-2014 document average mass change rates during each period at -0.22±0.12 m w.e. yr-1, -0.18±0.05 m w.e. yr-1, and -0.10±0.03 m w.e. yr-1. A correlation of field- measured mass balance and regional climate variables closely (i.e. within 0.08 m w.e. yr-1) predicts the geodetically 15 measured mass loss from 2005-2014. However, this correlation overestimates glacier mass balance for 1950-1960 by +1.18±0.92 m w.e. yr-1. Our analysis suggests that local effects, not represented in regional climate variables, have become a more dominant driver of the net mass balance as the glacier lost 0.50 km2 and retreated further into its cirque. -
Characteristics of the Bergschrund of an Avalanche-Cone Glacier in the Canadian Rocky Mountains
JOlIl"lla/ o/G/aci%gl'. VoL 29. No. 10 1. 1983 CHARACTERISTICS OF THE BERGSCHRUND OF AN AVALANCHE-CONE GLACIER IN THE CANADIAN ROCKY MOUNTAINS By G ERALD OSBORN (Department of Geology and Geophysics, Uni versity o f Calgary, Calgary, Alberta T2N I N4, Canada) ABSTRACT. Fi eld study of th e bergschrund of a small avalanche-cone glacier at the base of Mt Chephren, in Banff Nati onal Park , has been ca rried out as part of a general ex pl oratory study of glacier-head crevasses in th e Canadi an Roc ki es. The bergsc hrun d consists of a wide. shall ow. partl y bedrock-fl oored gap, und erneath whi ch ex tends a nearl y vertical Ralldklu!I, and a small , offset, subsidi ary crevasse (or crevasses). The fo ll owin g observations rega rdin g the behavior of th e bergsc hruncl and ice adjacent to it are of parti cul ar interest: ( I) topograph y of the subglaeial bedrock is a control on the location of the main bergschrund and subsidi a ry crevasses. (2) th e main bergschrund and subsid ia ry crevasse(s) are conn ected by subglacial gaps betwee n bedrock and ice; th e gaps are part of th e "bergschrund system" , (3) snow/ ice immedi ately down-glacier of the bergschrund system moves nea rl y verticall y dow nwa rd in response to rotational fl ow of the glacier. a ll owin g the bergschrund components to keep the same location and size fro m year to year, (4) an inde pend ent accumul ati on, fl ow. -
1922 Elizabeth T
co.rYRIG HT, 192' The Moootainetro !scot1oror,d The MOUNTAINEER VOLUME FIFTEEN Number One D EC E M BER 15, 1 9 2 2 ffiount Adams, ffiount St. Helens and the (!oat Rocks I ncoq)Ora,tecl 1913 Organized 190!i EDITORlAL ST AitF 1922 Elizabeth T. Kirk,vood, Eclttor Margaret W. Hazard, Associate Editor· Fairman B. L�e, Publication Manager Arthur L. Loveless Effie L. Chapman Subsc1·iption Price. $2.00 per year. Annual ·(onl�') Se,·ent�·-Five Cents. Published by The Mountaineers lncorJ,orated Seattle, Washington Enlerecl as second-class matter December 15, 19t0. at the Post Office . at . eattle, "\Yash., under the .-\0t of March 3. 1879. .... I MOUNT ADAMS lllobcl Furrs AND REFLEC'rION POOL .. <§rtttings from Aristibes (. Jhoutribes Author of "ll3ith the <6obs on lltount ®l!!mµus" �. • � J� �·,,. ., .. e,..:,L....._d.L.. F_,,,.... cL.. ��-_, _..__ f.. pt",- 1-� r�._ '-';a_ ..ll.-�· t'� 1- tt.. �ti.. ..._.._....L- -.L.--e-- a';. ��c..L. 41- �. C4v(, � � �·,,-- �JL.,�f w/U. J/,--«---fi:( -A- -tr·�� �, : 'JJ! -, Y .,..._, e� .,...,____,� � � t-..__., ,..._ -u..,·,- .,..,_, ;-:.. � --r J /-e,-i L,J i-.,( '"'; 1..........,.- e..r- ,';z__ /-t.-.--,r� ;.,-.,.....__ � � ..-...,.,-<. ,.,.f--· :tL. ��- ''F.....- ,',L � .,.__ � 'f- f-� --"- ��7 � �. � �;')'... f ><- -a.c__ c/ � r v-f'.fl,'7'71.. I /!,,-e..-,K-// ,l...,"4/YL... t:l,._ c.J.� J..,_-...A 'f ',y-r/� �- lL.. ��•-/IC,/ ,V l j I '/ ;· , CONTENTS i Page Greetings .......................................................................tlristicles }!}, Phoiitricles ........ r The Mount Adams, Mount St. Helens, and the Goat Rocks Outing .......................................... B1/.ith Page Bennett 9 1 Selected References from Preceding Mount Adams and Mount St. -
Washington Division of Geology and Earth Resources Open File Report 74-1
TEPHRA OF SALMON SPRINGS AGE FROM THE SOUTHEASTERN OLYMPIC PENINSULA, WASHINGTON by R. U. BIRDSEYE and R. J. CARSON North Carolina State University WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 74-1 1974 This report has not been edited or reviewed for conformity with Division of Geology and Earth Resources standards and nomenclature Revised October, 1989 CONTENTS Page Abstract •.•................••......••........•.......•............• 1 Introduction ....................................................... 1 Acknowledgments •••••••••••••••••••••••••••••••••••••••••••••••••••• 1 Pleistocene climate, glaciation, and volcanism ••••••••••••••••••••• 2 The ashes: Their thickness, distribution, and stratigraphic position •••••••••••••••••••••••••••••••••••••••••• 7 Color and texture of the ash ••••••••••••••••••••••••••••••••••••••• 14 Deposition of the ash •••••••••••••••••••••••••••••••••••••••••••••• 14 Atmospheric conditions during deposition of the ash •••••••••••••••• 20 Usefulness of volcanic ash in stratigraphic determination •••••••••• 21 Canel us ion ....•••.•..••••.••..••......•.••••••.••••....•••••...••.. 21 References cited ••••••••••••••••••••••••••••••••••••••••••••••••••• 23 ILLUSTRATIONS Figure 1 - Maximum extent of the Cordilleran ice sheet •••••••••••• 3 Figure 2 - Summary of late Pleistocene events in western Washington ••••••••••••••••••••••••••••••••••••• 4 Figure 3 - Location map showing inferred extent of minimum areas of fallout of volcanic ash from eruptions of Mount Mazama and Glacier Peak ••••••••••••••••••••••• -
Most Impaired" Coral Reef Areas in the State of Hawai'i
Final Report: EPA Grant CD97918401-0 P. L. Jokiel, K S. Rodgers and Eric K. Brown Page 1 Assessment, Mapping and Monitoring of Selected "Most Impaired" Coral Reef Areas in the State of Hawai'i. Paul L. Jokiel Ku'ulei Rodgers and Eric K. Brown Hawaii Coral Reef Assessment and Monitoring Program (CRAMP) Hawai‘i Institute of Marine Biology P.O.Box 1346 Kāne'ohe, HI 96744 Phone: 808 236 7440 e-mail: [email protected] Final Report: EPA Grant CD97918401-0 April 1, 2004. Final Report: EPA Grant CD97918401-0 P. L. Jokiel, K S. Rodgers and Eric K. Brown Page 2 Table of Contents 0.0 Overview of project in relation to main Hawaiian Islands ................................................3 0.1 Introduction...................................................................................................................3 0.2 Overview of coral reefs – Main Hawaiian Islands........................................................4 1.0 Ka¯ne‘ohe Bay .................................................................................................................12 1.1 South Ka¯ne‘ohe Bay Segment ...................................................................................62 1.2 Central Ka¯ne‘ohe Bay Segment..................................................................................86 1.3 North Ka¯ne‘ohe Bay Segment ....................................................................................94 2.0 South Moloka‘i ................................................................................................................96 2.1 Kamalō -
Review Article Magma Loading in the Southern Coast Plutonic Complex, British Columbia and Washington
GeoScienceWorld Lithosphere Volume 2020, Article ID 8856566, 17 pages https://doi.org/10.2113/2020/8856566 Review Article Magma Loading in the Southern Coast Plutonic Complex, British Columbia and Washington E. H. Brown Department of Geology, Western Washington University, USA Correspondence should be addressed to E. H. Brown; [email protected] Received 2 May 2020; Accepted 22 September 2020; Published 10 November 2020 Academic Editor: Tamer S. Abu-Alam Copyright © 2020 E. H. Brown. Exclusive Licensee GeoScienceWorld. Distributed under a Creative Commons Attribution License (CC BY 4.0). The southen end of the 1800 km long Coast Plutonic Complex (CPC), exposed in the Harrison Lake area of British Columbia and in the North Cascades of Washington, bears a record of great crustal thickening -20 to 40 km in localized zones during Late Cretaceous times. During this period, the CPC was positioned at the continental margin during collision/subduction of the Farallon plate. Arc magmatism and regional orogenic contraction were both active as potential crustal thickening processes. Magmatism is favored in this report as the dominant factor based on the delineation of four spatially and temporally separate loading events, the close association of the loaded areas with emplacement of large plutons, and a paucity of evidence of deep regional tectonic contraction. The timing and spatial location of crustal loading events are documented by the following: zircon ages in plutons; an early event of low pressure in pluton aureoles evidenced by andalusite, now pseudomorphed by high- pressure minerals; high pressures in country rock in pluton aureoles measured by mineral compositions in the assemblages garnet-biotite-muscovite-plagioclase and garnet-aluminum silicate-plagioclase; high pressures recorded in plutons by Al-in- hornblende barometry; and uplift ages of plutons derived from K-Ar and Ar-Ar ages of micas and hornblende in plutons. -
Stratigraphy, Age, and Provenance of the Eocene Chumstick Basin
Stratigraphy, age, and provenance of the Eocene Chumstick basin, Washington Cascades; implications for paleogeography, regional tectonics, and development of strike-slip basins Erin E. Donaghy1,†, Paul J. Umhoefer2, Michael P. Eddy1, Robert B. Miller3, and Taylor LaCasse4 1 Department of Earth, Planetary, and Atmospheric Sciences, Purdue University, West Lafayette, Indiana 47907, USA 2 School of Earth Sciences and Sustainability, Northern Arizona University, Flagstaff, Arizona 86011, USA 3 Department of Geology, San Jose State University, San Jose, California 95192, USA 4 Department of Geology, Carleton College, Northfield, Minnesota 55057 USA ABSTRACT tions can be constrained at high temporal Here we present a large provenance data set resolution (0.5–1.5 m.y. scale) for an ancient coupled with new lithofacies mapping from Strike-slip faults form in a wide variety strike-slip basin and permits a detailed re- the Chumstick basin within the framework of a of tectonic settings and are a first-order construction of sediment routing pathways recently developed precise depositional chronol- control on the geometry and sediment accu- and depositional environments. As a result, ogy (Eddy et al., 2016b). This basin formed in mulation patterns in adjacent sedimentary we can assess how varying sediment supply a strike-slip setting in central Washington and basins. Although the structural and depo- and accommodation space affects the depo- provides a unique opportunity to track changes sitional architecture of strike-slip basins is sitional architecture during strike-slip basin in sediment routing systems that are related well documented, few studies of strike-slip evolution. to rapidly changing paleogeography in basin- basins have integrated depositional age, bounding basement blocks. -
Oral to Written Evidence II
File No. OF-Fac-Oil-N304-2010-01 01 Hearing Order OH-4-2011 Enbridge Northern Gateway Pipelines Limited Partnership Northern Gateway Dual Pipelines, Tank Farm, and Supertanker Port Proposal *Supplemental Written Evidence Photographic Evidence Regarding Proposed Liquid Petroleum Pipelines from Nimbus Mountain to the Kitimat River Estuary *Originally intended to be submitted during oral evidence community hearings in Kitamaat, BC, on January 11th, 2012. The Panel, in file number A2K5I2, decided the following photographic evidence is considered written evidence, and should be submitted as such. I reserve the right to present this evidence orally at a later date. Hearing Order OH-4-2011 File No. OF-Fac-Oil-N304-2010-01 01 Submitted by Murray Minchin of DOUGLAS CHANNEL WATCH (All website links as of January 6, 2012) INTRODUCTION i.1) The geologic hazards in the Hoult Creek and upper Kitimat River Valleys, the earthflows in the main Kitimat Valley, and the extreme weather events experienced on the western side of the Coast Mountains on British Columbia's north coast may be the Achille's heel of Northern Gateway Pipeline Limited Partnership's proposal to move liquid petroleum products between Alberta's Tar Sands, and tidewater at Kitimat, BC. i.2) The majority of liquid petroleum pipelines in North America are to be found east of the Rocky Mountains in a relatively benign, rolling landscape. i.3) The Hoult Creek and upper Kitimat River Valleys are over 4,700 feet deep, very narrow, and are subject to long lived and extremely moist weather systems coming off the Pacific Ocean. -
Pasayten Rim Wilderness Evaluation
May-June 2009 Pasayten Rim Wilderness Evaluation WILDERNESS EVALUATION PASAYTEN RIM - 608025 41,349 acres OVERVIEW History The area was originally inventoried as two separate roadless areas totaling approximately 15,400 acres during RARE I. The areas were Sherman Peak (12,000 acres) and Last Chance (3,400 acres). The RARE II process combined the two areas and did not recommend the area for wilderness designation. Due to nonconforming uses such as road construction and logging, 160 acres were removed from previous inventory; 10,839 acres were added to the previous inventory as they met the criteria for a potential wilderness area (PWA) as described in Forest Service Handbook (FSH) 1909.12, Chapter 70. The following chart depicts the 1989 Okanogan Forest Land and Resource Management Plan direction for the 2006 potential wilderness area. Table 1--Management area percentages (rounded) Okanogan National Forest MA32 MA37 MA45 MA46 Recreation/ Mtn. Mineral Timber/ Scenery Goat Exploration Range Habitat 45% 11% 32% 13% Location and Access The area is located northwest of Winthrop in the northern portion of the Okanogan- Wenatchee National Forest, and consists of a long, narrow band of land along the south edge of the Pasayten Wilderness. All lands are located in Okanogan County. From Winthrop, access is provided over State Highway 20, and county and national forest roads in the Chewuch River, Eightmile Creek, Lost River, and Harts Pass areas. Geography and Topography The western portion of the area consists of a long, half mile-wide band of southwest facing slope between the Harts Pass road and the Pasayten Wilderness. -
Washington Geology, V, 21, No. 2, July 1993
WASHINGTON GEOLOGY Washington Department of Natural Resources, Division of Geology and Earth Resources Vol. 21, No. 2, July 1993 , Mount Baker volcano from the northeast. Bagley Lakes, in the foreground, are on a Pleistocene recessional moraine that is now the parking lot for Mount Baker Ski Area. Just below Sherman Peak, an erosional remnant on the left skyline, is Boulder Glacier. Park and Rainbow Glaciers share the area below the main summit (Grant Peak, 10,778 ft) . Boulder, Park, and Rainbow Glaciers drain into Baker Lake, which is out of the photo on the left. Mazama Glacier forms under the ridge that extends to Hadley Peak on the right. (See related article, p. 3 and Fig. 2, p. 5.) Table Mountain, the flat area just above and to the right of center, is a truncated lava flow. Lincoln Peak is just visible over the right shoulder of Mount Baker. Photo taken in 1964. In This Issue: Current behavior of glaciers in the North Cascades and its effect on regional water supplies, p. 3; Radon potential of Washington, p. 11; Washington areas selected for water quality assessment, p. 14; The changing role of cartogra phy in OGER-Plugging into the Geographic Information System, p. 15; Additions to the library, p. 16. Revised State Surface Minin!Jf Act-1993 by Raymond Lasmanls WASHINGTON The 1993 regular session of the 53rd Le:gislature passed a major revision of the surface mine reclamation act as En GEOLOGY grossed Second Substitute Senate Bill No. 5502. The new law takes effect on July 1, 1993. Both environmental groups and surface miners testified in favor of the act. -
WDFW Washington State Recovery Plan for the Lynx
STATE OF WASHINGTON March 2001 LynxLynx RecoveryRecovery PlanPlan by Derek Stinson Washington Department of FISH AND WILDLIFE Wildlife Program Wildlife Diversity Division WDFW 735 In 1990, the Washington Fish and Wildlife Commission adopted procedures for listing and delisting species as endangered, threatened, or sensitive and for writing recovery and management plans for listed species (WAC 232-12-297, Appendix C). The lynx was classified by the Washington Fish and Wildlife Commission as a threatened species in 1993 (Washington Administrative Code 232-12-011). The procedures, developed by a group of citizens, interest groups, and state and federal agencies, require that recovery plans be developed for species listed as threatened or endangered. Recovery, as defined by the U.S. Fish and Wildlife Service, is “the process by which the decline of an endangered or threatened species is arrested or reversed, and threats to its survival are neutralized, so that its long-term survival in nature can be ensured.” This document summarizes the historic and current distribution and abundance of the lynx in Washington, describes factors affecting the population and its habitat, and prescribes strategies to recover the species in Washington. The draft state recovery plan for the lynx was reviewed by researchers and state and federal agencies. This review was followed by a 90 day public comment period. All comments received were considered in preparation of this final recovery plan. For additional information about lynx or other state listed species, contact: Manager, Endangered Species Section Washington Department of Fish and Wildlife 600 Capitol Way N Olympia WA 98501-1091 This report should be cited as: Stinson, D.