2014 Medals & Awards Kirk Bryan Award
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Distribution and Genesis of Degeer Moraines: Insights from the New National Height Model
UNIVERSITY OF GOTHENBURG Department of Earth Sciences Geovetarcentrum/Earth Science Centre Distribution and genesis of DeGeer moraines: insights from the New National Height model Vera Bouvier Gribel ISSN 1400-3821 B850 Master of Science (120 credits) thesis Göteborg 2015 Mailing address Address Telephone Telefax Geovetarcentrum Geovetarcentrum Geovetarcentrum 031-786 19 56 031-786 19 86 Göteborg University S 405 30 Göteborg Guldhedsgatan 5A S-405 30 Göteborg SWEDEN University of Gothenburg |Vera Bouvier Content 1 Introduction -------------------------------------------------------------------------------------------------------- 1 1.1 Aim .............................................................................................................................................. 1 2 Background --------------------------------------------------------------------------------------------------------- 2 2.1 LiDAR .......................................................................................................................................... 2 2.2 DeGeer moraine - the landform ................................................................................................. 3 2.2.1 Terminology ....................................................................................................................... 3 2.2.2 Characteristics .................................................................................................................... 3 2.3 Related Landforms..................................................................................................................... -
Environmental Science Challenge for the Seventies
Environmental Science Challenge for the Seventies NATIONAL SCIENCE BOARD 1971 IVAltIliJiTit4iU1J REPORT OF THE NATIONAL SCIENCE BOARD NATIONAL SCIENCE BOARD NATIONAL SCIENCE FOUNDATION 1971 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price 40 cents LETTER OF TRANSMITTAL January 31, 1971 My Dear Mr. President: It is an honor to transmit to you this Report, prepared in re sponse to Section 4(g) of the National Science Foundation Act, as amended by Public Law 90-407, which requires the National Sci ence Board to submit annually an appraisal of the status and health of science, as well as that of the related matters of manpower and other resources, in reports to be forwarded to the Congress. This is the third report of this series. In choosing environmental science as the topic of this Report, the National Science Board hopes to focus attention on a critical aspect of environmental concern, one that is frequently taken for granted, whose status is popularly considered to be equivalent to that of science generally, and yet one whose contribution to human welfare will assume rapidly growing importance during the decades immediately ahead. The National Science Board strongly supports the many recent efforts of the Executive Branch, the Congress, and other public and private organizations to deal with the bewildering array of environmental problems that confront us all. Many of these prob lems can be reduced in severity through the use of today's science and technology by an enlightened citizenry. This is especially true of many forms of pollution and environmental degradation result ing from overt acts of man. -
Quaternary) Climates in New Mexico
Lucas, S.G., Morgan, G.S. and Zeigler, K.E., eds., 2005, New Mexico’s Ice Ages, New Mexico Museum of Natural History and Science Bulletin No. 28. 115 RIVER RESPONSES TO ICE AGE (QUATERNARY) CLIMATES IN NEW MEXICO FRANK J. PAZZAGLIA Department of Earth and Environmental Science, Lehigh University, 31 Williams, Bethlehem, PA 18015, [email protected] Abstract–Rivers shape landscapes by responding to a range of external forces including climate and climate change. This paper examines the general role that Quaternary climates play in river channel form and process and how rivers in New Mexico have responded specifically to Pleistocene and Holocene climatic changes. The impact of Quaternary climates on New Mexican streams is cast in the context of how channel form and process has evolved through the Phanerozoic and in light of a large and growing data set for measurable changes in channel form and watershed hydrology over human time scales. Changes in channel form and process are commonly equivocal; there is no single unique response that follows from a given change in climate. Neverthe- less, geomorphologists have developed process-response models that limit the range of expected responses and help guide an interpretation of how Quaternary climates ultimately have shaped the New Mexican landscape. Long-term landscape evolution trends like the rate of valley incision and human-scale trends like the arroyo incision-aggradation cycle are discussed in the context of Quaternary climates. The general conclusion is that climate change through the Quaternary has had a major impact on pacing the rate of valley incision and defining the geomorphic thresholds that control arroyo incision, but that other factors, including tectonics and humans, also contribute. -
Introduction to GIA Modeling
Glacial isostatic adjustment - An introduction Holger Steffen With input from Martin Ekman, Martin Lidberg, Rebekka Steffen, Wouter van der Wal, Pippa Whitehouse and Patrick Wu EGSIEM Summer School Potsdam, Germany 13/09/2017 GRACE observation, trend after post-processing 2 1st EGSIEM GIA correction 3 GRACE observation, GIA corrected 4 Question: What word or term do you have in mind when you hear “Glacial Isostatic Adjustment”? Time & length scale of some geodynamic processes GIA vs. the World 8 Plan In case of questions, ask! ° A bit of “GIA” history ° Some physics ° Some applications ° Observations of GIA ° Some applications ° GRACE, of course Reference for historical development ° Cathles, L.M. (1975) The viscosity of the Earth’s mantle, Princeton Univ. Press. ° Lliboutry, L. (1998) The birth and development of the concept of Glacial-Isostasy, and its Modelling up to 1974 in Dynamics of the Ice Age Earth: a modern Perspective, Ed. P.Wu, TTP. ° Ekman, M. (2009) The Changing Level of the Baltic Sea during 300 Years: A Clue to Understanding the Earth, Summer Institute for Historical Geophysics, Åland Islands. Open Access Download: http://www.historicalgeophysics.ax/The%20Changing %20Level%20of%20the%20Baltic%20Sea.pdf ° Krüger, T. (2013) Discovering the Ice Ages. International Reception and Consequences for a Historical Understanding of Climate. Brill, Leiden. Northern Europe ca. 1635 (Source: https://upload.wikimedia.org/wikipedia/commons/7/73/Svecia%2C_Dania_et_ Norvegia%2C_Regna_Europ%C3%A6_Septentrionalia.jpg) Luleå city/harbour relocation -
Union County Glacier
In Memory of Luna B. Leopold e c n e i c S y r a t e n a l P 1915–2006 & h t r a E f o . t p e D y e l e k r e B C U y s e t r u o c o t o h P una Leopold, professor emeritus at the University of Cali- 1972 to 1986 he held the position of professor of earth and plane- fornia, Berkeley, and former chief hydrologist of the U.S. tary science and of landscape architecture at the University of Cal- LGeological Survey died at his home in Berkeley on February ifornia, Berkeley. “He made crucial discoveries about the nature of 23, 2006. The son of conservationist Aldo Leopold, Luna Leopold rivers, especially their remarkable regularity,” William Dietrich, a became widely recognized as one of our country’s most distin- UC Berkeley colleague of Leopold’s and professor of earth and guished earth scientists and will be remembered for his pioneer- planetary science, said in a news release. “He showed that this ing studies of rivers and fluvial geomorphology and for his tire- regularity of form applies to all rivers, whether they are in sand less work toward protecting and restoring rivers, water resources, boxes or draining entire continents, at scales of a laboratory flume and the environment. or the Gulf Stream.” Luna Leopold was born in Albuquerque. His father, Aldo During his time with the U.S. Geological Survey Leopold was Leopold, was pursuing his career with the U.S. -
50Th Annivmtnforpdf
50th Anniversary The Institute of Arctic and Alpine Research 1951–2001 University of Colorado at Boulder 50th Anniversary The Institute of Arctic and Alpine Research 1951–2001 Scott Elias, INSTAAR, examines massive ground ice, Denali National Park,Alaska. Photo by S. K. Short. 50th Anniversary The Institute of Arctic and Alpine Research 1951–2001 University of Colorado at Boulder Contents 1 History of INSTAAR 29 Memories & Vignettes INSTAAR Photographs 57 INSTAAR’s News 81 Fifty Years of INSTAAR Theses credits Many past and present INSTAAR members contributed to this book with history, news, memories and vignettes, and informa- tion. Martha Andrews compiled the thesis list.The book was col- lated, edited, and prepared for publication by Kathleen Salzberg and Nan Elias (INSTAAR), and Polly Christensen (CU Publications and Creative Services). ©2001 Regents of the University of Colorado History of INSTAAR 1951–2001 his history of INSTAAR of arctic and alpine regions. Dr. Marr was has been compiled by Albert W. appointed director by the president of the TJohnson, Markley W.Paddock, university, Robert L. Stearns.Within two William H. Rickard,William S. Osburn, and years IAEE became the Institute of Arctic Mrs. Ruby Marr, as well as excerpts from and Alpine Research (IAAR). the late John W.Marr’s writing, for the pe- riod during which John W.Marr was direc- 1951–1953: The Early Years tor (1951–1967); by Jack D. Ives, former director, for 1967–1979; Patrick J.Webber, The ideas that led to the beginning of the In- former director, for 1979–1986; Mark F. stitute were those of John Marr; he was edu- Meier, former director, for 1986–1994; and cated in the philosophy that dominated plant James P.M. -
ACTA UNIVERSITATIS UPSALIENSIS Skrifter Rörande Uppsala Universitet B
ACTA UNIVERSITATIS UPSALIENSIS Skrifter rörande Uppsala universitet B. INBJUDNINGAR, 189 Redaktör: Per Ström Bild- och uppsatsredaktion: Carl Frängsmyr Layout: Grafisk service Vinjetter: Tryggve Nevéus Omslagsbild: Carl Wilhelmsons inspektorsporträtt av Arvid G. Högbom, Norrlands nation. Jämför sidan 16. Fotograf: Mikael Wallerstedt.. ISSN 0566-3091 ISBN 978-91-513-0525-7 Sättning: Grafisk service, Uppsala universitet Tr yck: DanagårdLiTHO AB, Ödeshög 2019 Kontakt med redaktionen Förfrågningar kring distribution och abonnemang, till exempel rörande levererad upplagas storlek eller önskemål om erhållande av seriens skrifter, riktas till redaktionen under följande e-postadress: [email protected] Promotionsfesten i Uppsala den 25 januari 2019 Innehåll Om Arvid G. Högboms Självbiografiska anteckningar. Av Carl Frängsmyr 7 Självbiografiska anteckningar. AvArvid G. Högbom 15 Personförteckning 73 Program 81 Processionsordning 82 Promotionsarrangemang 83 Rektors hälsningsord 85 Universitetets och fakulteternas inbjudan 87 Promotorernas presentationer Teologiska fakulteten, av Mattias Martinson 89 Juridiska fakulteten, av Minna Gräns 91 Medicinska fakulteten, av Anna Rask-Andersen 93 Farmaceutiska fakulteten, av Per Andrén 95 Historisk-filosofiska fakulteten, avErik Carlson 97 Språkvetenskapliga fakulteten, av Mats Eskhult 99 Samhällsvetenskapliga fakulteten, av Lars Magnusson 101 Utbildningsvetenskapliga fakulteten, av Ann-Carita Evaldsson 103 Teknisk-naturvetenskapliga fakulteten, av Gunilla Kreiss 105 Kortfattat promotionslexikon -
It Is an Honor to Receive the Kirk Bryan Award. I Am Especially Pleased To
Quaternary Geologist & Geomorphologist Newsletter of the Quaternary Geology and Geomorphology Division http://rock.geosociety.org/qgg Spring 2004 Vol. 45, No.1 Glacial lake that drained from head of Grasshopper Glacier, northern Wind River Range, Wyoming, in October, 2003. View is to west. Lake drained beneath glacier to north, and flooded to north then east down the drainage of Grasshopper Creek, to Down’s Fork Creek, and to Dinwoody Creek. Outwash deposits along the Down’s Fork Creek where an ephemeral lake ponded at Down’s Fork Meadows near the confluence of the Down’s Fork and Dinwoody creeks. Dinwoody Lakes are seen at upper left. View is to east. (More details of this event inside on p. 2) Photos provided by Dennis Dahms, courtesy of Liz Oswald, South Zone Hydrologist, Shoshone National Forest, Lander, Wyoming 1 Cover: Jökulhlaup at Grasshopper Glacier, Wind River Mountains, Wyoming A jökulhlaup, or glacial outburst flood, burst from an ice-dammed lake at the head of the Grasshopper Glacier, Wind River Mountains, Wyoming, in early September this year. The 30-acre lake drained an estimated 850 million gallons of water downslope, underneath the glacier, and, charged with subglacial sediment, flooded tributary valleys and into the Dinwoody River valley. The event was recorded at the USGS gage site (USGS 06221400 Dinwoody Creek above Lakes, near Burris, WY) about 20 mi downstream from the ice-dammed lake. The Grasshopper Glacier is situated at the continental divide nested between high-level erosion surfaces and the eastward-facing cirque walls of the mountain front. The glacier, oriented south to north, drops from an elevation of 12,000 ft down a steep (0.11) slope to its snout at about 11,300 ft elevation. -
Interview with Robert P. Sharp
ROBERT P. SHARP (I) (1911-2004) INTERVIEWED BY GRAHAM BERRY December 18, 1979–January 9, 1980 ARCHIVES CALIFORNIA INSTITUTE OF TECHNOLOGY Pasadena, California Subject area Geology Abstract Interview in three sessions in late 1979 and early 1980 with Robert P. Sharp, Sharp Professor of Geology emeritus, who chaired the Division of Geology (later the Division of Geological and Planetary Sciences) at Caltech from 1952 to 1968. Begins with his recollections of growing up in Oxnard and of life during his undergraduate years [1930-1934] at Caltech, including his career as quarterback on Caltech’s football team, and his one graduate year there. In 1936 he moved to Harvard for further graduate study, doing his thesis work on the Ruby/East Humboldt Range in Nevada. From 1938 to 1943 he taught at the University of Illinois; he discusses expeditions in the Grand Canyon (1937) and the Yukon (1941). After three years with the Army Air Force in Alaska, he joined the faculty of the University of Minnesota, then returned to Caltech as a professor in 1947. He discusses the early history of Caltech’s geology division under J. P. Buwalda, the importance of the Seismological Laboratory, and the demise of vertebrate paleontology at Caltech after the death of Chester Stock. Discusses the expansion of the division under his chairmanship into geochemistry and planetary science and other events of his chairmanship; chairing the search committee for a new president upon the retirement of Lee DuBridge; and the advent of Harold http://resolver.caltech.edu/CaltechOH:OH_Sharp_1 Brown. Recalls his participation in the efforts of Eugene Shoemaker and Leon Silver to raise money for a named chair by guiding trips in the Grand Canyon, and his establishment of field trips for the division non-academic staff. -
A Pioneer in Quaternary Geology in Scandinavia
doi:10.5200/baltica.2012.25.01 BALTICA Volume 25 Number 1 June 2012 : 1–22 Gerard De Geer – a pioneer in Quaternary geology in Scandinavia Ingemar Cato, Rodney L. Stevens Cato, I., Stevens, R. L., 2011. Gerard De Geer – a pioneer in Quaternary geology in Scandinavia. Baltica 5 (1), 1–22. Vilnius. ISSN 0067–3064. Abstract The paper presents a pioneer in Quaternary geology, both internationally and in Scandinavia – the Swedish geologist and professor Gerard De Geer (1858–1943). This is done, first by highlighting one of his most important contributions to science – the varve chronology – a method he used to describe the Weichselian land–ice recession over Scandinavia, and secondly by the re–publication of a summary article on Gerard De Geer’s early scientific achievement in 1881–1906 related to the Baltic Sea geology, written by his wife, Ebba Hult De Geer. Keywords Gerard De Geer• Clay varves • Varve chronology • Glacial and Postglacial• Quaternary geology • Baltic Sea Ingemar Cato [[email protected]], Geological Survey of Sweden, PO Box 670, SE-751 28 Uppsala, and University of Gothenburg, Department of Earth Sciences, PO Box 460, SE-405 30 Göteborg, Sweden; Rodney Stevens [stevens@gvc. gu.se], University of Gothenburg, Department of Earth Sciences, PO Box 460, SE-405 30 Göteborg, Sweden. Manuscript submitted 11 November 2011. INTRODUCTION It is unfortunately becoming more common in scientific papers that authors do not cite original sources of the methodology, observations and interpretations that their studies are based on. In many cases, the references are to very recent articles dealing with similar issues, which at best have correct references to the original sources. -
Baron Gerard De Geer, For. Mem. RS
No. 3851, AUGUST 21, 1943 NATURE 209 writing in general. He describes four stages, the first three of which he calls mnemonic, pictorial, and OBITUARIES ideographic, while by the fourth the alphabetic is clearly intended. But he is not justified in describing Baron Gerard de Geer, For.Mem.R.S. them as successive evolutionary stages. The first BARON GERARD JACOB DE GEER, whose death two may no doubt be regarded as ·both contributing occurred on July 24, was born in Stockholm on to the invention of writing, but there is no evolu October 2, 1858. Professor of geology at the Univer tionary series here. The alphabet, again, for all true sity of Stockholin from 1897 until 1924, he ended alphabets seem to have a single souree, though it his days as founder-director of the University's a pictographic origin, does not by any means evolve Geochronological Institute. There is more than one from arl. ideographic form of writing. On the contrary, Baron de Geer in Europe. The originator of the though the Japanese in adopting the Chinese script branch of the family from which the famous geologist may tend to give some of its ideograms a purely arose went to Sweden from what is now Belgium at alphabetic value, Chinese, which is ideographic, has the request of King Gustavus Adolphus early in the no alphabet. The nature of the Mohenjodaro script seventeenth century, and there started a large iron is still undetermined, and it is probably impossible and steel industry. In after years successive de Geers to say whet4er it is pictographic or ideographic. -
Varves in Lake Sediments E a Review
Quaternary Science Reviews 117 (2015) 1e41 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Invited review Varves in lake sediments e a review * Bernd Zolitschka a, , Pierre Francus b, c, Antti E.K. Ojala d, Arndt Schimmelmann e a Geomorphology and Polar Research (GEOPOLAR), Institute of Geography, University of Bremen, Celsiusstraße FVG-M, D-28359 Bremen, Germany b Centre Eau Terre Environnement, Institut National de la Recherche Scientifique, Quebec-City, Quebec G1K 9A9, Canada c GEOTOP Research Center, Montreal, Quebec H3C 3P8, Canada d Geological Survey of Finland, FI-02151 Espoo, Finland e Indiana University, Department of Geological Sciences, 1001 East 10th Street, Bloomington, IN 47405-1405, USA article info abstract Article history: Downcore counting of laminations in varved sediments offers a direct and incremental dating technique Received 13 August 2014 for high-resolution climatic and environmental archives with at least annual and sometimes even sea- Received in revised form sonal resolution. The pioneering definition of varves by De Geer (1912) had been restricted to rhyth- 20 March 2015 mically deposited proglacial clays. One century later the meaning of ‘varve’ has been expanded to include Accepted 22 March 2015 all annually deposited laminae in terrestrial and marine settings. Under favourable basin configurations Available online 11 April 2015 and environmental conditions, limnic varves are formed due to seasonality of depositional processes from the lake's water column and/or transport from the catchment area. Subsequent to deposition of Keywords: Varve topmost laminae, the physical preservation of the accumulating varved sequence requires the sustained Varve formation absence of sediment mixing, for example via wave action or macrobenthic bioturbation.