Glossary of Glacier Mass Balance and Related Terms
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Emplacement of a Silicic Lava Dome Through a Crater Glacier: Mount St Helens, 2004–06
14 Annals of Glaciology 45 2007 Emplacement of a silicic lava dome through a crater glacier: Mount St Helens, 2004–06 Joseph S. WALDER, Richard G. LaHUSEN, James W. VALLANCE, Steve P. SCHILLING United States Geological Survey, Cascades Volcano Observatory, 1300 Southeast Cardinal Court, Vancouver, Washington WA 98683-9589, USA E-mail: [email protected] ABSTRACT. The process of lava-dome emplacement through a glacier was observed for the first time after Mount St Helens reawakened in September 2004. The glacier that had grown in the crater since the cataclysmic 1980 eruption was split in two by the new lava dome. The two parts of the glacier were successively squeezed against the crater wall. Photography, photogrammetry and geodetic measure- ments document glacier deformation of an extreme variety, with strain rates of extraordinary magnitude as compared to normal alpine glaciers. Unlike normal temperate glaciers, the crater glacier shows no evidence of either speed-up at the beginning of the ablation season or diurnal speed fluctuations during the ablation season. Thus there is evidently no slip of the glacier over its bed. The most reasonable explanation for this anomaly is that meltwater penetrating the glacier is captured by a thick layer of coarse rubble at the bed and then enters the volcano’s groundwater system rather than flowing through a drainage network along the bed. INTRODUCTION ice bodies have been successively squeezed between the Since October 2004, a lava dome has been emplaced first growing lava dome and the crater walls. through, and then alongside, glacier ice in the crater of Several examples of lava-dome emplacement into ice Mount St Helens, Washington state, US. -
Surface Mass Balance of Small Glaciers on James Ross Island
Journal of Glaciology (2018), 64(245) 349–361 doi: 10.1017/jog.2018.17 © The Author(s) 2018. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited. Surface mass balance of small glaciers on James Ross Island, north-eastern Antarctic Peninsula, during 2009–2015 ̌ ̌ ̌ ZBYNEK ENGEL,1* KAMIL LÁSKA,2 DANIEL NÝVLT,2 ZDENEK STACHON2 1Department of Physical Geography and Geoecology, Faculty of Science, Charles University, Praha, Czech Republic 2Department of Geography, Faculty of Science, Masaryk University, Brno, Czech Republic *Correspondence: Zbyněk Engel <[email protected]> ABSTRACT. Two small glaciers on James Ross Island, the north-eastern Antarctic Peninsula, experi- enced surface mass gain between 2009 and 2015 as revealed by field measurements. A positive cumulative surface mass balance of 0.57 ± 0.67 and 0.11 ± 0.37 m w.e. was observed during the 2009–2015 period on Whisky Glacier and Davies Dome, respectively. The results indicate a change from surface mass loss that prevailed in the region during the first decade of the 21st century to predominantly positive surface mass balance after 2009/10. The spatial pattern of annual surface mass-balance distribution implies snow redistribution by wind on both glaciers. The mean equilibrium line altitudes for Whisky Glacier (311 ± 16 m a.s.l.) and Davies Dome (393 ± 18 m a.s.l.) are in accordance with the regional data indicating 200–300 m higher equilibrium line on James Ross and Vega Islands compared with the South Shetland Islands. -
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. -
The Dynamics and Mass Budget of Aretic Glaciers
DA NM ARKS OG GRØN L ANDS GEO L OG I SKE UNDERSØGELSE RAP P ORT 2013/3 The Dynamics and Mass Budget of Aretic Glaciers Abstracts, IASC Network of Aretic Glaciology, 9 - 12 January 2012, Zieleniec (Poland) A. P. Ahlstrøm, C. Tijm-Reijmer & M. Sharp (eds) • GEOLOGICAL SURVEY OF D EN MARK AND GREENLAND DANISH MINISTAV OF CLIMATE, ENEAGY AND BUILDING ~ G E U S DANMARKS OG GRØNLANDS GEOLOGISKE UNDERSØGELSE RAPPORT 201 3 / 3 The Dynamics and Mass Budget of Arctic Glaciers Abstracts, IASC Network of Arctic Glaciology, 9 - 12 January 2012, Zieleniec (Poland) A. P. Ahlstrøm, C. Tijm-Reijmer & M. Sharp (eds) GEOLOGICAL SURVEY OF DENMARK AND GREENLAND DANISH MINISTRY OF CLIMATE, ENERGY AND BUILDING Indhold Preface 5 Programme 6 List of participants 11 Minutes from a special session on tidewater glaciers research in the Arctic 14 Abstracts 17 Seasonal and multi-year fluctuations of tidewater glaciers cliffson Southern Spitsbergen 18 Recent changes in elevation across the Devon Ice Cap, Canada 19 Estimation of iceberg to the Hansbukta (Southern Spitsbergen) based on time-lapse photos 20 Seasonal and interannual velocity variations of two outlet glaciers of Austfonna, Svalbard, inferred by continuous GPS measurements 21 Discharge from the Werenskiold Glacier catchment based upon measurements and surface ablation in summer 2011 22 The mass balance of Austfonna Ice Cap, 2004-2010 23 Overview on radon measurements in glacier meltwater 24 Permafrost distribution in coastal zone in Hornsund (Southern Spitsbergen) 25 Glacial environment of De Long Archipelago -
Beneath the Forest Is a Biannual Newsletter Published by the Forest Service of the U.S
Volume 11, Issue 2 Fall 2018 Beneath the Forest is a biannual newsletter published by the Forest Service of the U.S. Department of Agriculture. Edited by Johanna L. Kovarik, Minerals and Geology Management Inside this Issue…and much more! Page Special Feature Article Part II, Case Study: Evolution of Cave and Karst Management on the Tongass National Forest 4 Peppersauce Cave Graffiti Removal Project, Coronado National Forest 9 Avalanche Cave and Karst Field Visit, Tahoe National Forest 13 Mount Saint Helens Glacier Cave Project, Gifford Pinchot National Forest 16 Arnold Ice Cave Stair Removal, Deschutes National Forest 20 Beneath the Forest 1 Editor’s Notes: CAVE AND KARST I am pleased to present our 21st issue of Beneath the Forest, the Forest Service cave and karst newsletter, CALENDAR OF EVENTS published twice a year in the spring and in the fall. ------------------------------------------------------------------------------- This is our tenth full year! Special thanks go to Phoebe Ferguson, our GeoCorps Participant in the National Cave Rescue Commission MGM WO, for the celebratory artwork on the logo of this issue. National NCRC Weeklong Seminar 11 - 18 May 2019 Articles for the Spring 2019 issue are due on April 1 Camp Riverdale/ Mitchell, Indiana 2019 in order for the issue to be out in May. We welcome contributions from stakeholders and New this year - you will be certified! volunteers as well as forest employees. Please —————————————————— encourage resource managers, cavers, karst scientists, National Speleological Society Convention and other speleological enthusiasts who do work on your forest to submit articles for the next exciting 17 - 21 June 2019 issue! Cookeville, Tennessee —————————————————— Cover art: Jewel Cave reaches 200 miles! WKU Karst Field Studies Program Cavers L– R: Dan Austin, Adam Weaver, Rene Ohms, Chris Pelczarski, Garrett June and July 2019 Jorgenson, Stan Allison Hamilton Valley Field Station/ Cave City, Kentucky Image: Dan Austin Courses available on a wide range of cave and karst- related topics. -
Learning to Speak Like a Glaciologist
Conversational Glaciology Answers Learning to speak like a glaciologist Matching Exercise A sharp knife-edge ridge of high ground that forms between arête two corries where they are cutting back into the rock A form of erosion that is caused by rocks and sediment at the abrasion base of glaciers grinding along the ground beneath acting like a giant sand-paper file to scrape and smooth rocks below Sediment material that is dragged along the base of a glacier bedload or ice sheet, acting to erode the ground beneath A mixture of sands, clays and boulders carried by a glacier and boulder then deposited over a large area clay (till) As ice slowly moves forward it pushes material forwards ahead bulldozing of it like a bulldozer The process whereby blocks of ice collapse and fall from the calving snout of the glacier, often into a glacial lagoon An armchair-shaped rounded hollow in a mountainside that is formed by a combination of glacial erosion, rotational slip and corrie /cwm / freeze-thaw weathering. When the ice melts it leaves a cirque depression in the rock A deep crack found in the surface of an ice-sheet or glacier, crevasse these are often buried under snow and can be incredibly dangerous if unseen A hill landform that is formed by the deposition of glacial till (boulder clay) as a glacier moves, they are usually oval in shape drumlin and their long axis is parallel to the direction of ice The imaginary boundary line between the ablation zone (where equilibrium ice is lost) and accumulation zone (where ice is gained) line The process of material being broken down and worn away, erosion which can happen in various ways, e.g. -
Rapid Glacial Retreat on the Kamchatka Peninsula During the Early 21St Century” by Colleen M
The Cryosphere Discuss., doi:10.5194/tc-2016-42-RC2, 2016 TCD © Author(s) 2016. CC-BY 3.0 License. Interactive comment Interactive comment on “Rapid glacial retreat on the Kamchatka Peninsula during the early 21st Century” by Colleen M. Lynch et al. Anonymous Referee #2 Received and published: 16 May 2016 STRENGTHS: Positively 1 - A huge amount of work behind the paper Positively 2 - A good review of associated publications, including Russian authors WEAKNESSES: - The paper is too long. The text contains lots of unnecessary naturally clear details and numbers which hinder its perception. Most numbers should be removed and put in the tables. Printer-friendly version - The authors don’t seem to take into account the uniqueness of Kamchatka region Discussion paper as an area where Holocene volcanism exists along with glaciation and can not help affecting it. The accomplished analysis is of a “standard” (formal) type, the same as for C1 non-volcanic regions. TCD However, along with tephra of recent eruptions (mentioned in the paper) many glaciers in Kamchatka (or their tongues) which motion is permanently destroying the friable slopes of Holocene volcanoes appear to be buried under a thick layer of deposits and Interactive continue flowing with it. comment At the same time they are nothing to do with rock glaciers having usually a snow- covered accumulation zone and a high flow velocity. In other words, they keep all glacial features but have a thick cover of deposits on themselves which exceeds obviously 5 cm, the threshold used in the paper for digitizing of glacial margins, which seems to be totally invalid for glacial mapping in Kamchatka. -
Mount St. Helens National Volcanic Monument: Preserved to Change the Real Treasure of the Mount St
OLCANO REVIEW VA VISITOR’S GUIDE TO MOUNT ST. HELENS NATIONAL VOLCANIC MONUMENT Mount St. Helens National Volcanic Monument: Preserved to Change The real treasure of the Mount St. Helens National Volcanic Monument is not the volcano or the surrounding landscape; it lies in the idea that this monument should be protected so that nature can work at its own pace to renew the land. Most protected areas are managed to keep them as they once were so that future generations will have an experience similar to what early visitors to the site would have had. Mount St. Helens National Volcanic Monument was set aside in the hopes that the next generation will have an experience markedly different than the one we have today. The Forest Service has worked hard to protect this valued place while ensuring public safety and providing recreational, educational and research opportunities. This precarious task can only be successful through partnering with our local communities. Join us in helping to provide a unique experience for future generations by sharing nature’s monumental achievements at Mount St. Helens National Volcanic Monument. Photo by Gavin Farrell U.S. Forest Service Gifford Pinchot National Forest Take Care of Your Pet and WELCOME Help Protect the Monument To protect plant and animal life and provide for visitor safety, pets are prohibited at all recreation sites and trails here is a lot going on within the monument’s restricted area (see yellow shaded section at the Monument of map on page 7). Pets are permitted only in designated pet Tthis summer. -
Mount St. Helens, 1980 to Now—What's Going
U.S. GEOLOGICAL SURVEY and the U.S. FOREST SERVICE—OUR VOLCANIC PUBLIC LANDS Mount St. Helens, 1980 to Now—What’s Going On? ount St. Helens seized M the world’s attention in 1980 when the largest historical landslide on Earth and a powerful explosive eruption reshaped the volcano, created its distinctive cra- ter, and dramatically modified the surrounding landscape. An enor- mous lava dome grew episodically in the crater until 1986, when the volcano became relatively quiet. A new glacier grew in the crater, wrapping around and partly burying the lava dome. From 1987 to 2003, sporadic earthquake swarms and small steam explosions indicated that magma (molten rock) was be- ing replenished deep underground. In 2004, steam-and-ash explosions heralded the start of another erup- More is going on than meets the eye in this south-facing photo of Mount St. Helens taken on June 8, 2005. tion. A quieter phase of continuous An unrelenting flow of semi-solid magma rises from a vent on the crater floor at a rate of about 10 feet per lava extrusion followed and lasted day, pushing up skyscraper-size spines. The spines collapse to form a steaming mound of lava called a lava until 2008, building a new dome dome. Split in two by the growing dome, Crater Glacier has started to flow more quickly northward. When the and doubling the volume of lava eruption ended in early 2008, the two arms of the glacier had met again after encircling both the new dome on the crater floor. Scientists with and an earlier one that grew from 1980 to 1986. -
Chapter 7 Glaciers
CHAPTER 7 GLACIERS 1. INTRODUCTION 1.1 Before the era of universal air travel, which commenced less than half a century ago, few of the world’s population had seen a glacier. I suspect that majority of class members in this course have seen a glacier—if not close up, then out of a jetliner window. In the Canadian Rockies, you can drive to within almost a stone’s throw of the terminus of the Athabasca Glacier, a classic active valley glacier. In many other parts of the world, valley glaciers are accessible to even casual day hikers. The great ice sheets of the world, in Antarctica and Greenland, remain much less accessible. 1.2 In the broad context of geologic history, the Earth is in an “icehouse” time, with recurrent major ice-sheet advances across the Northern Hemisphere continents. (There have been several other such icehouse periods in Earth history, separated by long intervals of ice-free times, called “greenhouse” periods, with no evidence of glaciation.) The Earth has only recently emerged from the latest episode of continental glaciation. Does it surprise you to learn that a mere twenty thousand years ago the Boston area was beneath a mile of glacier ice moving slowly southward toward its terminus south of what is now the south coast of New England? 1.3 The Earth is in many senses a glacial planet: • 10% of the Earth is covered with glacier ice (about 15 million square kilometers). • About 40% of the Northern Hemisphere in winter is covered with solid water at any given time (land and sea). -
Observations of Seasonal and Diurnal Glacier Velocities at Mount Rainier, Washington, Using Terrestrial Radar Interferometry
The Cryosphere, 9, 2219–2235, 2015 www.the-cryosphere.net/9/2219/2015/ doi:10.5194/tc-9-2219-2015 © Author(s) 2015. CC Attribution 3.0 License. Observations of seasonal and diurnal glacier velocities at Mount Rainier, Washington, using terrestrial radar interferometry K. E. Allstadt1,a, D. E. Shean1,2, A. Campbell1, M. Fahnestock3, and S. D. Malone1 1University of Washington, Department of Earth and Space Sciences, Washington, USA 2University of Washington, Applied Physics Lab Polar Science Center, Washington, USA 3University of Alaska Fairbanks, Geophysical Institute, Fairbanks, Alaska, USA anow at: USGS Geologic Hazards Science Center, Golden, CO, USA Correspondence to: K. E. Allstadt ([email protected]) Received: 16 June 2015 – Published in The Cryosphere Discuss.: 31 July 2015 Revised: 11 November 2015 – Accepted: 16 November 2015 – Published: 1 December 2015 Abstract. We present surface velocity maps derived from re- 1 Introduction peat terrestrial radar interferometry (TRI) measurements and use these time series to examine seasonal and diurnal dy- namics of alpine glaciers at Mount Rainier, Washington. We Direct observations of alpine glacier velocity can help im- show that the Nisqually and Emmons glaciers have small prove our understanding of ice dynamics. Alpine glacier slope-parallel velocities near the summit (< 0.2 m day−1), surface velocities are typically dominated by basal sliding, high velocities over their upper and central regions (1.0– which is tightly coupled to subglacial hydrology (Anderson 1.5 m day−1), and stagnant debris-covered regions near the et al., 2014; Bartholomaus et al., 2007). However, the spatial terminus (< 0.05 m day−1). -
Alphabetical Glossary of Geomorphology
International Association of Geomorphologists Association Internationale des Géomorphologues ALPHABETICAL GLOSSARY OF GEOMORPHOLOGY Version 1.0 Prepared for the IAG by Andrew Goudie, July 2014 Suggestions for corrections and additions should be sent to [email protected] Abime A vertical shaft in karstic (limestone) areas Ablation The wasting and removal of material from a rock surface by weathering and erosion, or more specifically from a glacier surface by melting, erosion or calving Ablation till Glacial debris deposited when a glacier melts away Abrasion The mechanical wearing down, scraping, or grinding away of a rock surface by friction, ensuing from collision between particles during their transport in wind, ice, running water, waves or gravity. It is sometimes termed corrosion Abrasion notch An elongated cliff-base hollow (typically 1-2 m high and up to 3m recessed) cut out by abrasion, usually where breaking waves are armed with rock fragments Abrasion platform A smooth, seaward-sloping surface formed by abrasion, extending across a rocky shore and often continuing below low tide level as a broad, very gently sloping surface (plain of marine erosion) formed by long-continued abrasion Abrasion ramp A smooth, seaward-sloping segment formed by abrasion on a rocky shore, usually a few meters wide, close to the cliff base Abyss Either a deep part of the ocean or a ravine or deep gorge Abyssal hill A small hill that rises from the floor of an abyssal plain. They are the most abundant geomorphic structures on the planet Earth, covering more than 30% of the ocean floors Abyssal plain An underwater plain on the deep ocean floor, usually found at depths between 3000 and 6000 m.