Early Season Activities in the US Antarctic Program
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY of the SCOTT GLACIER and WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA
This dissertation has been /»OOAOO m icrofilm ed exactly as received MINSHEW, Jr., Velon Haywood, 1939- GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA. The Ohio State University, Ph.D., 1967 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Velon Haywood Minshew, Jr. B.S., M.S, The Ohio State University 1967 Approved by -Adviser Department of Geology ACKNOWLEDGMENTS This report covers two field seasons in the central Trans- antarctic Mountains, During this time, the Mt, Weaver field party consisted of: George Doumani, leader and paleontologist; Larry Lackey, field assistant; Courtney Skinner, field assistant. The Wisconsin Range party was composed of: Gunter Faure, leader and geochronologist; John Mercer, glacial geologist; John Murtaugh, igneous petrclogist; James Teller, field assistant; Courtney Skinner, field assistant; Harry Gair, visiting strati- grapher. The author served as a stratigrapher with both expedi tions . Various members of the staff of the Department of Geology, The Ohio State University, as well as some specialists from the outside were consulted in the laboratory studies for the pre paration of this report. Dr. George E. Moore supervised the petrographic work and critically reviewed the manuscript. Dr. J. M. Schopf examined the coal and plant fossils, and provided information concerning their age and environmental significance. Drs. Richard P. Goldthwait and Colin B. B. Bull spent time with the author discussing the late Paleozoic glacial deposits, and reviewed portions of the manuscript. -
A NEWS BULLETIN Published Quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC)
A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) An English-born Post Office technician, Robin Hodgson, wearing a borrowed kilt, plays his pipes to huskies on the sea ice below Scott Base. So far he has had a cool response to his music from his New Zealand colleagues, and a noisy reception f r o m a l l 2 0 h u s k i e s . , „ _ . Antarctic Division photo Registered at Post Ollice Headquarters. Wellington. New Zealand, as a magazine. II '1.7 ^ I -!^I*"JTr -.*><\\>! »7^7 mm SOUTH GEORGIA, SOUTH SANDWICH Is- . C I R C L E / SOUTH ORKNEY Is x \ /o Orcadas arg Sanae s a Noydiazarevskaya ussr FALKLAND Is /6Signyl.uK , .60"W / SOUTH AMERICA tf Borga / S A A - S O U T H « A WEDDELL SHETLAND^fU / I s / Halley Bav3 MINING MAU0 LAN0 ENOERBY J /SEA uk'/COATS Ld / LAND T> ANTARCTIC ••?l\W Dr^hnaya^^General Belgrano arg / V ^ M a w s o n \ MAC ROBERTSON LAND\ '■ aust \ /PENINSULA' *\4- (see map betowi jrV^ Sobldl ARG 90-w {■ — Siple USA j. Amundsen-Scott / queen MARY LAND {Mirny ELLSWORTH" LAND 1, 1 1 °Vostok ussr MARIE BYRD L LAND WILKES LAND ouiiiv_. , ROSS|NZJ Y/lnda^Z / SEA I#V/VICTORIA .TERRE , **•»./ LAND \ /"AOELIE-V Leningradskaya .V USSR,-'' \ --- — -"'BALLENYIj ANTARCTIC PENINSULA 1 Tenitnte Matianzo arg 2 Esptrarua arg 3 Almirarrta Brown arc 4PttrtlAHG 5 Otcipcion arg 6 Vtcecomodoro Marambio arg * ANTARCTICA 7 Arturo Prat chile 8 Bernardo O'Higgins chile 1000 Miles 9 Prasid«fTtB Frei chile s 1000 Kilometres 10 Stonington I. -
Species Status Assessment Emperor Penguin (Aptenodytes Fosteri)
SPECIES STATUS ASSESSMENT EMPEROR PENGUIN (APTENODYTES FOSTERI) Emperor penguin chicks being socialized by male parents at Auster Rookery, 2008. Photo Credit: Gary Miller, Australian Antarctic Program. Version 1.0 December 2020 U.S. Fish and Wildlife Service, Ecological Services Program Branch of Delisting and Foreign Species Falls Church, Virginia Acknowledgements: EXECUTIVE SUMMARY Penguins are flightless birds that are highly adapted for the marine environment. The emperor penguin (Aptenodytes forsteri) is the tallest and heaviest of all living penguin species. Emperors are near the top of the Southern Ocean’s food chain and primarily consume Antarctic silverfish, Antarctic krill, and squid. They are excellent swimmers and can dive to great depths. The average life span of emperor penguin in the wild is 15 to 20 years. Emperor penguins currently breed at 61 colonies located around Antarctica, with the largest colonies in the Ross Sea and Weddell Sea. The total population size is estimated at approximately 270,000–280,000 breeding pairs or 625,000–650,000 total birds. Emperor penguin depends upon stable fast ice throughout their 8–9 month breeding season to complete the rearing of its single chick. They are the only warm-blooded Antarctic species that breeds during the austral winter and therefore uniquely adapted to its environment. Breeding colonies mainly occur on fast ice, close to the coast or closely offshore, and amongst closely packed grounded icebergs that prevent ice breaking out during the breeding season and provide shelter from the wind. Sea ice extent in the Southern Ocean has undergone considerable inter-annual variability over the last 40 years, although with much greater inter-annual variability in the five sectors than for the Southern Ocean as a whole. -
Novitatesamerican MUSEUM PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET NEW YORK, N.Y
NovitatesAMERICAN MUSEUM PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET NEW YORK, N.Y. 10024 U.S.A. NUMBER 2552 OCTOBER 15, 1974 EDWIN H. COLBERT AND JOHN W COSGRIFF Labyrinthodont Amphibians from Antarctica Labyrinthodont Amphibians from Antarctica EDWIN H. COLBERT Curator Emeritus, The Amer'wan Museum of Natural History Professor Emeritus, Columbia University Curator of Vertebrate Paleontology The Museum of Northern Arizona, Flagstaff JOHN W COSGRIFF Associate Professor of Biology Wayne State University, Michigan AMERICAN MUSEUM NOVITATES NUMBER 2552, pp. 1-30, figs. 1-20, table 1 ISSN 0003-0082 Issued October 15, 1974 Price $1.95 Copyright © The American Museum of Natural History 1974 ABSTRACT ian which, following further comparative studies, Labyrinthodont amphibians from the Lower is identified in the present paper as a brachyopid. Triassic Fremouw Formation of Antarctica are The discovery of this specimen-an accidental described. These consist of a fragment of a lower event tangential to Barrett's study of the geology jaw collected at Graphite Peak in the Transant- of the Transantarctic Mountains in the general arctic Mountains in December, 1967, and various region of the Beardmore Glacier-was the stimu- fossils from Coalsack Bluff (west of the lus for a program of vertebrate paleontological Beardmore Glacier and some 140 km., or about collecting in Antarctica. An expedition under the 88 miles, northwest of Graphite Peak) during the auspices of the Institute of Polar Studies of The austral summer of 1969-1970 and from near the Ohio State University and the National Science junction of the McGregor and Shackleton Gla- Foundation went to the Beardmore Glacier area ciers (about 100 km., or 60 miles, more or less, during the austral summer of 1969-1970 for the to the east and a little south of Graphite Peak) during the austral summer of 1970-1971. -
The Antarctic Sun, December 28, 2003
Published during the austral summer at McMurdo Station, Antarctica, for the United States Antarctic Program December 28, 2003 Photo by Kristan Hutchison / The Antarctic Sun A helicopter lands behind the kitchen and communications tents at Beardmore Camp in mid-December. Back to Beardmore: By Kristan Hutchison Researchers explore the past from temporary camp Sun staff ike the mythical town of Brigadoon, a village of tents appears on a glacial arm 50 miles L from Beardmore Glacier about once a decade, then disappears. It, too, is a place lost in time. For most people, a visit to Beardmore Camp is a trip back in history, whether to the original camp structure from 19 years ago, now buried under snow, or to the sites of ancient forests and bones, now buried under rock. Ever since Robert Scott collected fos- sils on his way back down the Beardmore Glacier in February 1912, geologists and paleontologists have had an interest in the rocky outcrops lining the broad river of ice. This year’s Beardmore Camp was the third at the location on the Lennox-King Glacier and the researchers left, saying there Photo by Andy Sajor / Special to The Antarctic Sun Researchers cut dinosaur bones out of the exposed stone on Mt. Kirkpatrick in December. See Camp on page 7 Some of the bones are expected to be from a previously unknown type. INSIDE Quote of the Week Dinosaur hunters Fishing for fossils “The penguins are happier than Page 9 Page 11 Trackers clams.” Plant gatherers - Adelie penguin researcher summing Page 10 Page 12 up the attitude of a colony www.polar.org/antsun 2 • The Antarctic Sun December 28, 2003 Ross Island Chronicles By Chico That’s the way it is with time son. -
The Neogene Biota of the Transantarctic Mountains
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Related Publications from ANDRILL Affiliates Antarctic Drilling Program 2007 The Neogene biota of the Transantarctic Mountains A. C. Ashworth North Dakota State University, [email protected] A. R. Lewis North Dakota State University, [email protected] D. R. Marchant Boston University, [email protected] R. A. Askin [email protected] D. J. Cantrill Royal Botanic Gardens, [email protected] See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/andrillaffiliates Part of the Environmental Indicators and Impact Assessment Commons Ashworth, A. C.; Lewis, A. R.; Marchant, D. R.; Askin, R. A.; Cantrill, D. J.; Francis, J. E.; Leng, M. J.; Newton, A. E.; Raine, J. I.; Williams, M.; and Wolfe, A. P., "The Neogene biota of the Transantarctic Mountains" (2007). Related Publications from ANDRILL Affiliates. 5. https://digitalcommons.unl.edu/andrillaffiliates/5 This Article is brought to you for free and open access by the Antarctic Drilling Program at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Related Publications from ANDRILL Affiliates by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors A. C. Ashworth, A. R. Lewis, D. R. Marchant, R. A. Askin, D. J. Cantrill, J. E. Francis, M. J. Leng, A. E. Newton, J. I. Raine, M. Williams, and A. P. Wolfe This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/ andrillaffiliates/5 U.S. Geological Survey and The National Academies; USGS OF-2007-1047, Extended Abstract.071 The Neogene biota of the Transantarctic Mountains A. -
Borehole Temperatures Reveal Peninsula Warming
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | The Cryosphere Discuss., 5, 3053–3084, 2011 www.the-cryosphere-discuss.net/5/3053/2011/ The Cryosphere doi:10.5194/tcd-5-3053-2011 Discussions TCD © Author(s) 2011. CC Attribution 3.0 License. 5, 3053–3084, 2011 This discussion paper is/has been under review for the journal The Cryosphere (TC). Borehole Please refer to the corresponding final paper in TC if available. temperatures reveal Peninsula warming Borehole temperatures reveal details of V. Zagorodnov et al. 20th century warming at Bruce Plateau, Antarctic Peninsula Title Page Abstract Introduction V. Zagorodnov1, O. Nagornov2, T. A. Scambos3, A. Muto3,*, E. Mosley-Thompson1, E. C. Pettit4, and S. Tyuflin2 Conclusions References 1Byrd Polar Research Center, The Ohio State University, Columbus OH 43210, USA Tables Figures 2Moscow Engineering Physics Institute, Kashirskoe Shosse 31, Moscow 115409, Russia 3 National Snow and Ice Data Center, CIRES, University of Colorado at Boulder, J I Boulder CO 80309, USA 4Department of Geology and Geophysics, University of Alaska Fairbanks, Fairbanks, J I AK 99775, USA Back Close *now at: Dept. of Geosciences, Pennsylvania State University, State College, PA 16802, USA Received: 15 September 2011 – Accepted: 17 October 2011 – Published: 2 November 2011 Full Screen / Esc Correspondence to: V. Zagorodnov ([email protected]) Printer-friendly Version Published by Copernicus Publications on behalf of the European Geosciences Union. Interactive Discussion 3053 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract TCD Two ice core boreholes of 143.74 m and 447.65 m (bedrock) were drilled during the 2009–2010 austral summer on the Bruce Plateau at a location named LARISSA Site 5, 3053–3084, 2011 Beta (66◦020 S, 64◦040 W, 1975.5 m a.s.l.). -
Download Factsheet
Antarctic Factsheet Geographical Statistics May 2005 AREA % of total Antarctica - including ice shelves and islands 13,829,430km2 100.00% (Around 58 times the size of the UK, or 1.4 times the size of the USA) Antarctica - excluding ice shelves and islands 12,272,800km2 88.74% Area ice free 44,890km2 0.32% Ross Ice Shelf 510,680km2 3.69% Ronne-Filchner Ice Shelf 439,920km2 3.18% LENGTH Antarctic Peninsula 1,339km Transantarctic Mountains 3,300km Coastline* TOTAL 45,317km 100.00% * Note: coastlines are fractal in nature, so any Ice shelves 18,877km 42.00% measurement of them is dependant upon the scale at which the data is collected. Coastline Rock 5,468km 12.00% lengths here are calculated from the most Ice coastline 20,972km 46.00% detailed information available. HEIGHT Mean height of Antarctica - including ice shelves 1,958m Mean height of Antarctica - excluding ice shelves 2,194m Modal height excluding ice shelves 3,090m Highest Mountains 1. Mt Vinson (Ellsworth Mts.) 4,892m 2. Mt Tyree (Ellsworth Mts.) 4,852m 3. Mt Shinn (Ellsworth Mts.) 4,661m 4. Mt Craddock (Ellsworth Mts.) 4,650m 5. Mt Gardner (Ellsworth Mts.) 4,587m 6. Mt Kirkpatrick (Queen Alexandra Range) 4,528m 7. Mt Elizabeth (Queen Alexandra Range) 4,480m 8. Mt Epperly (Ellsworth Mts) 4,359m 9. Mt Markham (Queen Elizabeth Range) 4,350m 10. Mt Bell (Queen Alexandra Range) 4,303m (In many case these heights are based on survey of variable accuracy) Nunatak on the Antarctic Peninsula 1/4 www.antarctica.ac.uk Antarctic Factsheet Geographical Statistics May 2005 Other Notable Mountains 1. -
Glaciological Studies at Siple Station (Antarctica): Potential Ice-Core Paleoclimatic Record
Journal of Glaciology, Vol. 37, No. 125, 1991 Glaciological studies at Siple Station (Antarctica): potential ice-core paleoclimatic record E. MOSLEY-THOMPSON, J. DAI, L. G. THOMPSON, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio 43210-1308, U.S.A. P. M . GROOTES, Q_uat~rnary Isotope Laboratory, University of Washington, Seattle, Washington 98195, U.S.A. JAMES K. ARBOGAST AND j. F. PASKIEVITCH Byrd Polar Research Center, The Ohio State University, Columbus, Ohio 43210-1308, U.S.A. ABSTRACT. The quality and utility of the records of oxygen-isotopic abundances, dust concentrations and anionic concentrations preserved in the ice at Siple Station (75°55' S, 84°15' W) are assessed from four shallow (20m) cores. The combination of high accumu lation (0.56 m a- 1 w.e. ) and low mean annual temperature (-24°C) preserves the prominent seasonal variations in 818 0 which are very spatially coherent. Sulfate concentrations vary seasonall y and, in conjunction with 818 0, will allow accurate dating of deeper cores from Siple Station. The concentrations of insoluble dust are the lowest measured in Antarctica, making Siple Station an excellent location to examine large increases in atmospheric tubidity. The seasonal variations and annual fluxes of the anions are examined for the last two decades (AD 1966-85) with regard to probable sources. An unusually high sulfate flux in 1976 may reflect the February 1975 eruption of Mount Ngauruhoe, New Zealand. No annual signal in nitrate concentration is confirmed and no unusually high nitrate fluxes support the suggestion of nitrate production by large solar flares. -
VLF Wave Injection Into the Magnetosphere from Siple Station
VOL. 79, NO. 16 JOURNAL OF GEOPHYSICAL RESEARCH JUNE I, 1974 VLF Wave Injection Into the MagnetosphereFrom Siple Station, Antarctica R. A. HELLIWELL AND J.P. KATSUFRAKIS RadioscienceLaboratory, Stanford University,Stanford, California 94305 Radio signalsin the 1.5- to 16-kHz range transmittedfrom Siple Station, Antarctica (L = 4), are used to control wave-particleinteractions in the magnetosphere.Observations at the conjugatepoint show signalgrowth and triggeredemissions including risers, failers, and hooks. Growth ratesof the order of 100 dB/s and total gainsup to 30 dB are observed.Triggered emissions may be cut off or havetheir fre- quencyrate of changealtered by Siplepulses. Similar effectsoccur in associationwith harmonicsfrom the Canadianpower system. The observedtemporal growth is predictedby a recentlyproposed feedback model of cyclotroninteraction. Plasma instability theories predicting only spatialgrowth are not in ac- cord with these observations.Possible applications include study of nonlinear plasma instability phenomena,diagnostic measurements of energeticparticles trapped in the magnetosphere,modification of the ionosphere through control of precipitation, and VLF communication through the magnetosphere. This is a report of the first resultsof a new experimentto plasma instability. To obtain further experimental data, a control wave-particleinteractions in the magnetosphere,us- transmitter was neededthat could operate at lower frequen- ing VLF waves.Coherent whistlermode signalswere injected cies and whose power, pulse length, and frequency could into the magnetospherein the 1.5- to 16.0-kHz range from a easily be varied. 100-kW transmitter located at Siple Station, Antarctica. The The next step was constructionof a 33.6-km-long horizon- output signalswere observedat the Sipleconjugate point near tal dipole at Byrd Station (L = 7.25) in 1965 [Guy, 1966]. -
Hnjtflrcilild
HNjTflRCililD A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) Drillers on the Ross Ice Shelf last season used a new hot water system to penetrate fc. 416m of ice and gain access to the waters of the Ross Sea. Here the rig is at work on an access hole for a Norwegian science rproject. ' U . S . N a v y p h o t o Registered ol Post Office Headquarters, Vol. 8, No. 9. Wellington. New Zealand, as a magazine. SOUTH GEORGIA. •.. SOUTH SANDWICH Is' ,,r circle / SOUTH ORKNEY Is' \ $&?-""" "~~~^ / "^x AFAtKtANOis /^SiJS?UK*"0.V" ^Tl~ N^olazarevskayauss« SOUTH AMERICA / /\ ,f Borg°a ~7^1£^ ^.T, \60'E, /? cnirru „ / \ if sa / anT^^^Mo odezhnaya V/ x> SOUTH 9 .» /WEDDELL \ .'/ ' 0,X vr\uss.aT/>\ & SHETtAND-iSfV, / / Halley Bay*! DRONNING MAUD LAND ^im ^ >^ \ - / l s * S Y 2 < 'SEA/ S Euk A J COATSu k V ' tdC O A T S t d / L A N D ! > / \ Dfu^naya^^eneral Belgrano^RG y\ \ Mawson ANTARCTIC SrV MAC ROBERTSON LAND\ \ aust /PENINSULA'^ (see map below) Sobral arg / t Davis aust K- Siple ■■ [ U S A Amundsen-Scott / queen MARY LAND <JMirny AJELLSWORTH Vets') LAND °Vostok ussr MARIE BYRDNs? vice ShelA^ WIIKES tAND , ? O S S ^ . X V a n d a N z / SEA I JpY/VICTORIA .TERRE ,? ^ P o V t A N D V ^ / A D H J E j / V G E O R G E V L d , , _ / £ ^ . / ,^5s=:»iv-'s«,,y\ ^--Dumont d Urville france Leningradskaya \' / USSB_,^'' \ / -""*BALLENYIs\ / ANTARCTIC PENINSULA 1 Teniente Matienzo arg 2 Esperanza arg 3 Almirante Brown arg 4 Petrel arg 5 Decepcion arg. -
Age of the Falla Formation (Triassic), Queen Alexandra Range
West Antarctica, has been computed with the use of a Bentley, C. R., and J . W. Clough. 1972. Seismic refraction finite difference technique. Results agree well with ob- shooting in Ellsworth and Dronning Maud Lands. In: Ant- served data. Comparison with calculations based on arctic Geology and Geophysics (R. J . Adie, ed.). Oslo, Uni- versitetsforlaget. 169-172. approximations commonly made in surface wave analyses Clough, J . W. 1973. Radio-echo sounding: brine percolation 4 (Poissons ratio = 1/ ; density = constant) surprisingly layer. Journal of Glaciology, 12(64): 141-143. shows that the group velocities are relatively more sensi- Kohnen, H. 1971. The relation between seismic urn structure, tive to incorrect densities than to incorrect shear wave temperature, and accumulation. Zeitschrift für Gletscherkunde velocities. und Glazialgeologie, VII( I-2): 141-151. Kohnen, H. 1972. Uber die beziehung zwischen seismischen 7. Final strain-rate calculations for a grid network geschwindigkeiten und der dichte in firn and eis. Zeitschrift across Roosevelt Island show a strongly asymmetrical für Geophysik, 38: 925-935. profile, with the longitudinal extensional strains twice as Kohnen, H., and C. R. Bentley. 1973. Seismic refraction and re- great on the northeast as on the southwest flank of the flection measurements at Byrd Station, Antarctica. Journal of Glaciology, 12(64): 101-111. island. Since accumulation rates on the two flanks are Kososki, B. A. 1972. A gravity study of West Antarctica. M. S. about the same the difference in strain rates is probably Thesis, University of Wisconsin. attributable to the effect of the Ross Ice Shelf. Robertson, J. D. 1972. A seismic study of the structure and metamorphism of 6rn in West Antarctica.