Sustaining the Science Impact of Summit Station, Greenland a White Paper Produced from the Summit Station Science Summit
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Geologic Map of the Frisco Quadrangle, Summit County, Colorado
Geologic Map of the Frisco Quadrangle, Summit County, Colorado By Karl S. Kellogg, Paul J. Bartos, and Cindy L. Williams Pamphlet to accompany MISCELLANEOUS FIELD STUDIES MAP MF-2340 2002 U.S. Department of the Interior U.S. Geological Survey Geologic Map of the Frisco Quadrangle, Summit County, Colorado By Karl S. Kellogg, Paul J. Bartos, and Cindy L. Williams DESCRIPTION OF MAP UNITS af Artificial fill (recent)—Compacted and uncompacted rock fragments and finer material underlying roadbed and embankments along and adjacent to Interstate 70. Also includes material comprising Dillon Dam dt Dredge tailings (recent)—Unconsolidated, clast-supported deposits containing mostly well- rounded to subrounded, cobble- to boulder-size clasts derived from dredging of alluvium for gold along the Blue and Swan Rivers; similar dredge tailings along Gold Run Gulch are too small to show on map. Dredge tailings were mapped from 1974 air photos; most tailings have now been redistributed and leveled for commercial development Qal Alluvium (Holocene)—Unconsolidated clast-supported deposits containing silt- to boulder-size, moderately sorted to well-sorted clasts in modern floodplains; includes overbank deposits. Clasts are as long as 1 m in Blue River channel; clasts are larger in some side-stream channels. Larger clasts are moderately rounded to well rounded. Includes some wetland deposits in and adjacent to beaver ponds along Ryan Gulch. Maximum thickness unknown, but greater than 10 m in Blue River channel Qw Wetland deposits (Holocene)—Dark-brown to black, organic-rich sediment underlying wetland areas, commonly containing standing water and dense willow stands. Maximum thickness estimated to be about 15 m Qav Avalanche deposits (Holocene)—Unsorted, unstratified hummocky deposits at the distal ends of avalanche-prone hillside in Sec. -
The High Deccan Duricrusts of India and Their Significance for the 'Laterite
The High Deccan duricrusts of India and their significance for the ‘laterite’ issue Cliff D Ollier1 and Hetu C Sheth2,∗ 1School of Earth and Geographical Sciences, The University of Western Australia, Nedlands, W.A. 6009, Australia. 2Department of Earth Sciences, Indian Institute of Technology (IIT) Bombay, Powai, Mumbai 400 076, India. ∗e-mail: [email protected] In the Deccan region of western India ferricrete duricrusts, usually described as laterites, cap some basalt summits east of the Western Ghats escarpment, basalts of the low-lying Konkan Plain to its west, as well as some sizeable isolated basalt plateaus rising from the Plain. The duricrusts are iron-cemented saprolite with vermiform hollows, but apart from that have little in common with the common descriptions of laterite. The classical laterite profile is not present. In particular there are no pisolitic concretions, no or minimal development of con- cretionary crust, and the pallid zone, commonly assumed to be typical of laterites, is absent. A relatively thin, non-indurated saprolite usually lies between the duricrust and fresh basalt. The duricrust resembles the classical laterite of Angadippuram in Kerala (southwestern India), but is much harder. The High Deccan duricrusts capping the basalt summits in the Western Ghats have been interpreted as residuals from a continuous (but now largely destroyed) laterite blan- ket that represents in situ transformation of the uppermost lavas, and thereby as marking the original top of the lava pile. But the unusual pattern of the duricrusts on the map and other evidence suggest instead that the duricrusts formed along a palaeoriver system, and are now in inverted relief. -
Dr. Nicolas Cullen, Department of Geography, University of Otago, Dunedin, New Zealand Dr
CV: K. Steffen 1 CURRICULUM VITAE : KONRAD STEFFEN Swiss Federal Research Institute WSL Zürcherstr. 111, CH-8903 Birmendorf, Switzerland Tel: +41 44 739 24 55; [email protected], [email protected] US and Swiss Citizen, married and two kids EDUCATION Dr.sc.nat.ETH,1984 Surface temperature distribution of an Arctic polynya: North Water in winter; advisor Prof. Dr. Atsumu Ohmura, ETH-Zürich. Dipl.nat.ETH, 1977 Snow distribution on tundra and glaciers on Axel Heiberg Island, NWT, Canada; advisor Prof. Dr. Fritz Müller, ETH-Zürich. PROFESSIONAL EXPERIENCES 2017-present Science Director, Swiss Polar Institute 2012-present Director, Swiss Federal Research Institute WSL 2012-present Professor, Inst. Atmosphere & Climate, ETH-Zürich 2012-present Professor, Architecture, Civil and Environmental Engineering, EPF-Lausanne 2005- 2012 Director, Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado (CU) 2004-2005 Interim Director, CIRES, University of Colorado (CU) 2003-2004 Deputy Director, CIRES, University of Colorado (CU) 2002-2003 Interim Director, CIRES, University of Colorado (CU) 1998-2005 Associate Director Cryosphere and Polar Processes, CIRES 1997-2012 Professor at Dept. of Geography, University of Colorado at Boulder 1993-2012 Faculty, Program in Atmospheric and Oceanic Sciences 1991-1997 Associate Professor at Dept. of Geography, University of Colorado 1991-2012 Fellow CIRES, University of Colorado at Boulder Sept.-Oct. 1987 Visiting Professor at Dept. of Geography, McGill University, Montreal 1986-1988 Visiting Fellow at Cooperative Institute for Research in Environmental Sciences (CIRES), on leave from ETH for two years 1985-1990 Oberassistent (Lecturer) at Climate Research Group, ETH, Zürich, Switzerland 1983-1985 Assistant at Climate Research Group, ETH, Zürich, Switzerland RECENT GRADUATE STUDENTS Dr. -
Sublimation on the Greenland Ice Sheet from Automated Weather Station Observations
BOX AND STEFFEN: SUBLIMATION ON THE GREENLAND ICE SHEET 1 PDF Version of Accepted Paper (Note some symbol errors may exist, i.e. delta symbol is converted to ?) Sublimation on the Greenland ice sheet from automated weather station observations Jason E. Box and Konrad Steffen Cooperative Institute for Research in Environmental Sciences University of Colorado, Boulder, Colorado, USA Abstract. Greenland Climate Network (GC-Net) surface meteorological observations are used to estimate net surface water vapor flux at ice sheet sites. Results from aerodynamic profile methods are compared with eddy correlation and evaporation pan measurements. Two profile method types are applied to hourly data sets spanning 1995.4 to 2000.4. One method type is shown to accurately gauge sublimation using two humidity and wind speed measurement levels. The other “bulk” method type is shown to underestimate condensation, as it assumes surface saturation. General climate models employ bulk methods and, consequently, underestimate deposition. Loss of water vapor by the surface predominates in summer at lower elevations, where bulk methods agree better with two-level methods. Annual net water vapor flux from the two-level method is as great as -87 ±27 mm at 960 m elevation and -74 ±23 mm at equilibrium line altitude in western Greenland. At an undulation trough site, net deposition is observed (+40 mm ±12). At the adjacent crest site 6 km away and at 50 m higher elevation, net sublimation predominates. At high-elevation sites, the annual water vapor flux is positive, up to +32 ±9 mm at the North Greenland Ice core Project (NGRIP) and +6 ±2 mm at Summit. -
On the Glaciology of Edgegya and Barentsgya, Svalbard
On the glaciology of Edgegya and Barentsgya, Svalbard JULIAN A. DOWDESWELL and JONATHAN L. BAMBER Dowdeswell J. A. & Bamber. J. L. 1995: On the glaciology of Edgeoya and Barentsoya, Svalbard. Polar Research 14(2). 105-122. The ice masses on Edgeoya and Barentsdya are the least well known in Svalbard. The islands are 42-47% ice covered with the largest ice cap, Edge0yjokulen. 1365 km2 in area. The tidewater ice cliffs of eastern Edgedya are over 80 km long and produce small tabular icebergs. Several of the ice-cap outlet glaciers on Edgeoya and Barentsoya are known to surge, and different drainage basins within the ice caps behave as dynamically separate units. Terminus advances during surging have punctuated more general retreat from Little Ice Age moraines, probably linked to Twentieth Century climate warming and mass balance change. Airborne radio-echo sounding at 60 MHz along 340 km of flight track over the ice masses of Edgeoya and Barentsldya has provided ice thickness and elevation data. Ice is grounded below sea level to about 20 km inland from the tidewater terminus of Stonebreen. Ice thickens from <lo0 rn close to the margins, to about 250 m in the interior of Edgeeiyj~kulen.The maximum ice thickness measured on Barentsjokulen was 270111. Landsat MSS images of the two islands, calibrated to in-band reflectance values, allow synoptic examination of snowline position in late July/early August. Snow and bare glacier ice were identified. and images were digitally stretched and enhanced. The snowline was at about 300111 on the east side of Edgeoyjbkulen, and 50-100 m higher to the west. -
Investigating the Influence of Surface Meltwater on the Ice Dynamics of the Greenland Ice Sheet
INVESTIGATING THE INFLUENCE OF SURFACE MELTWATER ON THE ICE DYNAMICS OF THE GREENLAND ICE SHEET by William T. Colgan B.Sc., Queen's University, Canada, 2004 M.Sc., University of Alberta, Canada, 2007 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirement for the degree of Doctor of Philosophy Department of Geography 2011 This thesis entitled: Investigating the influence of surface meltwater on the ice dynamics of the Greenland Ice Sheet, written by William T. Colgan, has been approved for the Department of Geography by _____________________________________ Dr. Konrad Steffen (Geography) _____________________________________ Dr. Waleed Abdalati (Geography) _____________________________________ Dr. Mark Serreze (Geography) _____________________________________ Dr. Harihar Rajaram (Civil, Environmental, and Architectural Engineering) _____________________________________ Dr. Robert Anderson (Geology) _____________________________________ Dr. H. Jay Zwally (Goddard Space Flight Center) Date _______________ The final copy of this thesis has been examined by the signatories, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above mentioned discipline. Colgan, William T. (Ph.D., Geography) Investigating the influence of surface meltwater on the ice dynamics of the Greenland Ice Sheet Thesis directed by Professor Konrad Steffen Abstract This thesis explains the annual ice velocity cycle of the Sermeq (Glacier) Avannarleq flowline, in West Greenland, using a longitudinally coupled 2D (vertical cross-section) ice flow model coupled to a 1D (depth-integrated) hydrology model via a novel basal sliding rule. Within a reasonable parameter space, the coupled model produces mean annual solutions of both the ice geometry and velocity that are validated by both in situ and remotely sensed observations. -
From Decades to Epochs: Spanning the Gap Between Geodesy and Structural Geology of Active Mountain Belts
Journal of Structural Geology 31 (2009) 1409–1422 Contents lists available at ScienceDirect Journal of Structural Geology journal homepage: www.elsevier.com/locate/jsg From decades to epochs: Spanning the gap between geodesy and structural geology of active mountain belts Richard W. Allmendinger a,*, John P. Loveless b, Matthew E. Pritchard a, Brendan Meade b a Department of Earth & Atmospheric Sciences Cornell University, Ithaca, NY 14853-1504, United States b Department of Earth & Planetary Sciences, Harvard University, Cambridge, MA, United States article info abstract Article history: Geodetic data from the Global Navigation Satellite System (GNSS), and from satellite interferometric Received 25 March 2009 radar (InSAR) are revolutionizing how we look at instantaneous tectonic deformation, but the signifi- Received in revised form cance for long-term finite strain in orogenic belts is less clear. We review two different ways of analyzing 31 July 2009 geodetic data: velocity gradient fields from which one can extract strain, dilatation, and rotation rate, and Accepted 9 August 2009 elastic block modeling, which assumes that deformation is not continuous but occurs primarily on Available online 14 August 2009 networks of interconnected faults separating quasi-rigid blocks. These methods are complementary: velocity gradients are purely kinematic and yield information about regional deformation; the calcula- Keywords: Geodesy tion does not take into account either faults or rigid blocks but, where GNSS data are dense enough, GPS active fault zones and stable blocks emerge naturally in the solution. Block modeling integrates known Active tectonics structural geometry with idealized earthquake cycle models to predict slip rates on active faults. Future technological advances should overcome many of today’s uncertainties and provide rich new data to mine by providing denser, more uniform, and temporally continuous observations. -
Lesson 1: Mount Everest Lesson Plan
Lesson 1: Mount Everest Lesson Plan Use the Mount Everest PowerPoint presentation in conjunction with this lesson. The PowerPoint presentation contains photographs and images and follows the sequence of the lesson. If required, this lesson can be taught in two stages; the first covering the geography of Mount Everest and the second covering the successful 1953 ascent of Everest by Sir Edmund Hillary and Tenzing Norgay. Key questions Where is Mount Everest located? How high is Mount Everest? What is the landscape like? How do the features of the landscape change at higher altitude? What is the weather like? How does this change? What are conditions like for people climbing the mountain? Who were Edmund Hillary and Tenzing Norgay? How did they reach the summit of Mount Everest? What did they experience during their ascent? What did they do when they reached the summit? Subject content areas Locational knowledge: Pupils develop contextual knowledge of the location of globally significant places. Place knowledge: Communicate geographical information in a variety of ways, including writing at length. Interpret a range of geographical information. Physical geography: Describe and understand key aspects of physical geography, including mountains. Human geography: Describe and understand key aspects of human geography, including land use. Geographical skills and fieldwork: Use atlases, globes and digital/computer mapping to locate countries and describe features studied. Downloads Everest (PPT) Mount Everest factsheet for teachers -
Hydrology Specialist Report
Motorized Travel Plan Hydrology Specialist Report Hydrology Specialist Report Motorized Travel Plan Dixie National Forest Reeds Valley, Cedar City Ranger District Prepared by Bill Goodman, East Zone Hydrologist and Chris Butler, West Zone Hydrologist May 2008 Updated March 2009 1 March 2009 Motorized Travel Plan Hydrology Specialist Report Table of Contents 3.0 Affected Environment.............................................................................................................2 3.1 Existing Conditions ............................................................................................................2 4.0 Environmental Consequences ...............................................................................................9 4.1 Direct and Indirect Effects..................................................................................................9 4.2 Cumulative Effects ...........................................................................................................17 5.0 Project Design Criteria Common to All Action Alternatives..................................................22 6.0 Compliance with Other Laws and Regulations ....................................................................23 6.1 Clean Water Act...............................................................................................................23 6.2 Executive Order 11988 (Protection of Floodplains) of May 24, 1977...............................23 6.3 Executive Order 11990 (Protection of Wetlands) of May 24, 1977..................................23 -
E-Book on Dynamic Geology of the Northern Cordillera (Alaska and Western Canada) and Adjacent Marine Areas: Tectonics, Hazards, and Resources
Dynamic Geology of the Northern Cordillera (Alaska and Western Canada) and Adjacent Marine Areas: Tectonics, Hazards, and Resources Item Type Book Authors Bundtzen, Thomas K.; Nokleberg, Warren J.; Price, Raymond A.; Scholl, David W.; Stone, David B. Download date 03/10/2021 23:23:17 Link to Item http://hdl.handle.net/11122/7994 University of Alaska, U.S. Geological Survey, Pacific Rim Geological Consulting, Queens University REGIONAL EARTH SCIENCE FOR THE LAYPERSON THROUGH PROFESSIONAL LEVELS E-Book on Dynamic Geology of the Northern Cordillera (Alaska and Western Canada) and Adjacent Marine Areas: Tectonics, Hazards, and Resources The E-Book describes, explains, and illustrates the have been subducted and have disappeared under the nature, origin, and geological evolution of the amazing Northern Cordillera. mountain system that extends through the Northern In alphabetical order, the marine areas adjacent to the Cordillera (Alaska and Western Canada), and the Northern Cordillera are the Arctic Ocean, Beaufort Sea, intriguing geology of adjacent marine areas. Other Bering Sea, Chukchi Sea, Gulf of Alaska, and the Pacific objectives are to describe geological hazards (i.e., Ocean. volcanic and seismic hazards) and geological resources (i.e., mineral and fossil fuel resources), and to describe the scientific, economic, and social significance of the earth for this region. As an example, the figure on the last page illustrates earthquakes belts for this dangerous part of the globe. What is the Northern Cordillera? The Northern Cordillera is comprised of Alaska and Western Canada. Alaska contains a series of parallel mountain ranges, and intervening topographic basins and plateaus. From north to south, the major mountain ranges are the Brooks Range, Kuskokwim Mountains, Aleutian Range, Alaska Range, Wrangell Mountains, and the Chugach Mountains. -
Catalogue of Place Names in Northern East Greenland
Catalogue of place names in northern East Greenland In this section all officially approved, and many Greenlandic names are spelt according to the unapproved, names are listed, together with explana- modern Greenland orthography (spelling reform tions where known. Approved names are listed in 1973), with cross-references from the old-style normal type or bold type, whereas unapproved spelling still to be found on many published maps. names are always given in italics. Names of ships are Prospectors place names used only in confidential given in small CAPITALS. Individual name entries are company reports are not found in this volume. In listed in Danish alphabetical order, such that names general, only selected unapproved names introduced beginning with the Danish letters Æ, Ø and Å come by scientific or climbing expeditions are included. after Z. This means that Danish names beginning Incomplete documentation of climbing activities with Å or Aa (e.g. Aage Bertelsen Gletscher, Aage de by expeditions claiming ‘first ascents’ on Milne Land Lemos Dal, Åkerblom Ø, Ålborg Fjord etc) are found and in nunatak regions such as Dronning Louise towards the end of this catalogue. Å replaced aa in Land, has led to a decision to exclude them. Many Danish spelling for most purposes in 1948, but aa is recent expeditions to Dronning Louise Land, and commonly retained in personal names, and is option- other nunatak areas, have gained access to their al in some Danish town names (e.g. Ålborg or Aalborg region of interest using Twin Otter aircraft, such that are both correct). However, Greenlandic names be - the remaining ‘climb’ to the summits of some peaks ginning with aa following the spelling reform dating may be as little as a few hundred metres; this raises from 1973 (a long vowel sound rather than short) are the question of what constitutes an ‘ascent’? treated as two consecutive ‘a’s. -
Winter Camp: a Blog from the Greenland Summit Lora Koenig, NASA Goddard Space Flight Center, [email protected]
The Earth Observer March - April 2009 Volume 21, Issue 2 13 Winter Camp: A Blog from the Greenland Summit Lora Koenig, NASA Goddard Space Flight Center, [email protected] When temperatures turn cold, some people travel to a tropical destination to stay warm. Instead, Lora Koenig —a remote- sensing glaciologist at NASA’s Goddard Space Flight Center—donned layer upon layer of extra clothes to brave the harsh Arctic at the National Science Foundation’s (NSF) Greenland Summit Camp. Koenig lived and worked at the research station from November 2008–February 2009, making ground-truth measurements of the Greenland Ice Sheet to validate data collected by NASA’s Aqua, Terra, and Ice, Clouds, and land Elevation Satellite (ICESat) satellites. Koenig described her experience at Summit in a weekly blog, with excerpts from the first seven weeks of her stay presented here. Look for Part II of the story ofKoenig’s “Journey to Greenland’s Frozen Summit” in the May–June 2009 issue of The Earth Observer. The complete blog with color photos, along with a question & answer by Koenig, is available at: earthobservatory.nasa. gov/Features/GreenlandBlogKoenig/. Week One Introduction November 3, 2008 Hello! I’m a remote sensing glaciologist in the Cryospheric Sciences Branch at the NASA Goddard Space Flight Center (GSFC). My research uses satellites to monitor ice sheets and compares measurements from space to those taken on the ground. These interests have led me to spend this winter at Summit, Greenland (Latitude 72.5°N, Longitude 38.5°W). Over the course of this weekly blog, I will tell you about my life and science, in the middle of the Greenland Ice Sheet, in the middle of the winter.