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Minutes of Meeting at British Antarctic Survey Held on Wednesday 15Th November 2006 at 11.00 Am
APC(06)2nd Meeting ANTARCTIC PLACE-NAMES COMMITTEE MINUTES OF MEETING AT BRITISH ANTARCTIC SURVEY HELD ON WEDNESDAY 15TH NOVEMBER 2006 AT 11.00 AM. Present Mr P.J. Woodman Chairman Mrs C. Burgess Permanent Committee on Geographical Names Dr K. Crosbie Ad hoc member Prof J.A. Dowdeswell Director, Scott Polar Research Institute, University of Cambridge Mr A.J. Fox British Antarctic Survey Mr P. Geelan Ad hoc member: former Chairman, APC Lt Cdr J.E.J. Marshall Hydrographic Office Mr S. Ross Polar Regions Unit, Overseas Territories Department, Foreign and Commonwealth Office Ms J. Rumble Polar Regions Unit, Overseas Territories Department, Foreign and Commonwealth Office Dr J.R. Shears British Antarctic Survey Dr M.R.A. Thomson Ad hoc member Ms A. Martin Secretary 1. Apologies for absence and new members Apologies for absence were received from Dr Hattersley-Smith, Royal Geographical Society. The Chairman welcomed Dr Crosbie who had joined the committee as a result of the recruitment initiative following the last meeting. The Chairman also welcomed Mr Ross, the new BAT Desk Officer at the Polar Regions Unit, Foreign and Commonwealth Office. 2. Minutes of the last meeting, held on 10th May 2006 The minutes were approved by all present. It was pointed out that the letters of reappointment for Mr Geelan, Dr Thomson and Mr Woodman had not been received. The Secretary was asked to look into this and to ensure that the letters were sent. 3. Matters arising from the minutes of the last meeting Secretary’s review of development work being carried out on the BAT Gazetteer and APC website. -
2010-2011 Science Planning Summaries
Find information about current Link to project web sites and USAP projects using the find information about the principal investigator, event research and people involved. number station, and other indexes. Science Program Indexes: 2010-2011 Find information about current USAP projects using the Project Web Sites principal investigator, event number station, and other Principal Investigator Index indexes. USAP Program Indexes Aeronomy and Astrophysics Dr. Vladimir Papitashvili, program manager Organisms and Ecosystems Find more information about USAP projects by viewing Dr. Roberta Marinelli, program manager individual project web sites. Earth Sciences Dr. Alexandra Isern, program manager Glaciology 2010-2011 Field Season Dr. Julie Palais, program manager Other Information: Ocean and Atmospheric Sciences Dr. Peter Milne, program manager Home Page Artists and Writers Peter West, program manager Station Schedules International Polar Year (IPY) Education and Outreach Air Operations Renee D. Crain, program manager Valentine Kass, program manager Staffed Field Camps Sandra Welch, program manager Event Numbering System Integrated System Science Dr. Lisa Clough, program manager Institution Index USAP Station and Ship Indexes Amundsen-Scott South Pole Station McMurdo Station Palmer Station RVIB Nathaniel B. Palmer ARSV Laurence M. Gould Special Projects ODEN Icebreaker Event Number Index Technical Event Index Deploying Team Members Index Project Web Sites: 2010-2011 Find information about current USAP projects using the Principal Investigator Event No. Project Title principal investigator, event number station, and other indexes. Ainley, David B-031-M Adelie Penguin response to climate change at the individual, colony and metapopulation levels Amsler, Charles B-022-P Collaborative Research: The Find more information about chemical ecology of shallow- USAP projects by viewing individual project web sites. -
KEN MILLER Oklahoma State Treasurer It’S Your Money
A Message From KEN MILLER Oklahoma State Treasurer It’s your money. Please come get it! Please take a few minutes to see if your name is included on this list of all new names to see if you have treasure waiting to be claimed. Oklahoma businesses bring unclaimed cash, rebates, paychecks, royalties, stock and bonds to my office and it’s my job to return the money to the owners and heirs. Our service is always free and there is no time limit on claiming your property! These are just the most recent names we have received. Our online database contains thousands of names dating back to Search and file a claim online for your 1967. If your name is not on this list, check our website at: unclaimed property. Go to: www.treasurer.ok.gov www.treasurer.ok.gov If you find your name, start your claim online or use the form on the back. to get started. For all other questions Thank you, about unclaimed property, call us at 405-521-4273 Ken Miller, Oklahoma State Treasurer NOTICE OF NAMES OF PERSONS APPEARING TO BE OWNERS OF ABANDONED PROPERTY JULY 2011 – Newspaper Advertising Supplement 2 ADAIR COUNTY — BUNCH JULY 2011 • UNCLAIMED PROPERTY BEAVER COUNTY — BEAVER SOAP HAZEL MITCHELL NEILA NOELS OIL ADAIR RT BOX 165 COUNRTY VILL MOBILE PO BOX 387 SWIMMER CHERRIE L HOME PRK B OWEN GEORGIA BUNCH PO BOX 1097 MURRAY ASHLEY 704 W 13TH ST TABLE OF CONTENTS RODNEY KIMBLE TEEHEE CHARLOTTEA RT 1 BOX 556 PLEASANT PARALEE D PO BOX 2 RR 4 BOX 320 PRIETO KAMISHA RR 2 BOX 1170 ADAIR COUNTY PAGE 2 LOVE COUNTY PAGE 28 PROCTOR THIRSTY ASHLEY ANN 209 W CHINCAPIN PREFERRED PHCY RT1 BOX 1529 SAWNEY EDWARD L PROVIDERS OF SE OK ALFALFA COUNTY PAGE 2 MAJOR COUNTY PAGE 28 BAILEY WAYNE MR P.O. -
2003-2004 Science Planning Summary
2003-2004 USAP Field Season Table of Contents Project Indexes Project Websites Station Schedules Technical Events Environmental and Health & Safety Initiatives 2003-2004 USAP Field Season Table of Contents Project Indexes Project Websites Station Schedules Technical Events Environmental and Health & Safety Initiatives 2003-2004 USAP Field Season Project Indexes Project websites List of projects by principal investigator List of projects by USAP program List of projects by institution List of projects by station List of projects by event number digits List of deploying team members Teachers Experiencing Antarctica Scouting In Antarctica Technical Events Media Visitors 2003-2004 USAP Field Season USAP Station Schedules Click on the station name below to retrieve a list of projects supported by that station. Austral Summer Season Austral Estimated Population Openings Winter Season Station Operational Science Opening Summer Winter 20 August 01 September 890 (weekly 23 February 187 McMurdo 2003 2003 average) 2004 (winter total) (WinFly*) (mainbody) 2,900 (total) 232 (weekly South 24 October 30 October 15 February 72 average) Pole 2003 2003 2004 (winter total) 650 (total) 27- 34-44 (weekly 17 October 40 Palmer September- 8 April 2004 average) 2003 (winter total) 2003 75 (total) Year-round operations RV/IB NBP RV LMG Research 39 science & 32 science & staff Vessels Vessel schedules on the Internet: staff 25 crew http://www.polar.org/science/marine. 25 crew Field Camps Air Support * A limited number of science projects deploy at WinFly. 2003-2004 USAP Field Season Technical Events Every field season, the USAP sponsors a variety of technical events that are not scientific research projects but support one or more science projects. -
L MOUNTAINEER
]l MOUNTAINEER 1950 ,, The MOUNTAINEER 1950 MOUNT ROBSON •••from a forthcoming book by Bob and Ira Spring I• I9J O The MOUNTAINEER Volume 42 DECEMBER 15, 1950 Number 13 Organized 1906 Incorporated 1913 EditOt"ial Board 1950 HELEN McLELLAN, Editor HELEN A. FROBERG MILDRED HOFFMAN Typists and Proofreadet"S LILO BERLINER MARY HOSSACK ELENOR BUSWELL CLAIRE MOCK HILDE M. FROHLICH MRS. LOUIS NASH HAZEL GATES LEE SNIDER Photography Editing BOB AND IRA SPRING Mailing MRS. IRVING GAVETT Subscriprion Price, $2.00 a Year Published and Copyrighted 1950 by THE MOUNTAINEERS, INC. Published monrhly, January to November, inclusive, and semi-monthly during December by THE MOUNTAINEERS, INC., P. 0. Box 122, Seatrle 11, Washington Clubrooms at 523 Pike Street I Entered as Second Class Matter, April 18, 1922 ar Post Office at ) Seattle, Washingron, under rl1e Act of March 3, 1879 31 � THE MOUNTAINEERS, INC. OFFICERS-1951 President, T. Davis Castor Secrelt11')', Mary Anderson CAMERON BECKWITH Vice-President, Treamrer, Phyllis Cavander ELECTED TRUSTEES Terms Expiring October 31, 1951 Terms Expiring Octobe1 31, 1952 Mary Anderson T. Davis Castor Burge Bickford John Hossack Cameron Beckwith Leo Gallagher William Degenhardt Mrs. Irving Gavett Arthur Winder George MacGowan Seattle Committee Chairmen See Monthly Bulletin TACOMA BRANCH President, Keith Goodman Secrelary-Treamrer, Mary Fries Vice-President, Wally Miner Tmstee, John Carter TRUSTEES Norma Judd Walker Frederick Ann Jackson Clarence Garner CHAIRMEN OF COMMITTEES Climbing, Jack Gallagher Membership, Mildred Altes Conservation, Bill Kilmer Music, Irene Slade Dance, John Upham Photographic, Florence Richardson frish Cabin, Floyd Raver P11blicity, Carl Heacon IriJh Cabin Activity, Alice Bond Ski, Lester Fasig Local Walks, Marjorie Goodman Socict!, Stella Kellogg Specict! 011ti11gs, Gene Faure EVERETT UNIT President, Vivian Widmer Treas11rer, C. -
Downstream-Propagating Channel Responses to Decadal-Scale Climate Variability in a Glaciated River Basin
RESEARCH ARTICLE Downstream‐Propagating Channel Responses 10.1029/2018JF004734 to Decadal‐Scale Climate Variability Key Points: • Geomorphic analysis of stream gage in a Glaciated River Basin data in a glaciated river basin Scott W. Anderson1 and Chris P. Konrad1 indicates a downstream‐propagating vertical channel response to climate 1Washington Water Science Center, U.S. Geology Survey, Tacoma, WA, USA variability • The climate‐driven bed elevation response propagated downstream at 1 to 4 km per year; propagation rate Abstract Regional climate is an important control on the rate of coarse sediment mobilization and scaled closely with channel slope transport in alpine river systems. Changes in climate are then expected to cause a cascade of geomorphic • Comparisons with previously responses, including adjustments in downstream channel morphology. However, the mechanics and collected records suggest a regionally coherent relation sensitivity of channel response to short‐term climate variability remain poorly documented. In the Nooksack between climate variability and River, which drains a glaciated stratovolcano in Washington State, bed elevation changes were inferred from coarse sediment yield in shifting stage‐discharge relations at seven U.S Geological Survey stream gages. Decadal‐scale elevation sediment‐rich, glaciated basins trends can be explained as a downstream‐propagating channel response to regional climate variability, Supporting Information: where periods of persistent warm, dry (cool and wet) conditions corresponded to periods of aggradation • Supporting Information S1 (incision). The channel elevation response propagated downstream at a rate of 1 to 4 km per year; propagation rate scaled closely with channel slope. Historical trends in glacier extent and flood intensity both show some potential to explain climate‐sediment linkages, though assessing causation is complicated Correspondence to: by the shared climate signal in both records. -
Usgs Course Sediment Dynamics in the White River Watershed
Coarse Sediment Dynamics in the White River Watershed October 2019 Department of Natural Resources and Parks Water and Land Resources Division King Street Center, KSC-NR-0600 201 South Jackson Street, Suite 600 Seattle, WA 98104 www.kingcounty.gov i Coarse Sediment Dynamics in the White River Watershed Prepared for: King County Water and Land Resources Division Department of Natural Resources and Parks Submitted by: Scott Anderson and Kristin Jaeger U.S. Geological Survey Washington Water Science Center Funded in part by: King County Flood Control District ii iii Acknowledgements This study was partially funded by the King County Flood Control District and was completed with the technical support of King County employees Fred Lott, Judi Radloff, and Chris Brummer; Zac Corum (USACE Seattle); and Dan Johnson (USACE Mud Mountain Dam). Brian Collins improved this study immensely by providing copies of the 1907 Chittenden survey sheets. Thanks to Melissa Foster at Quantum Spatial for helping to acquire extended 2016 lidar coverage and for supplying ancillary data for previous acquisitions. Thanks to Taylor Kenyon and Scott Beason at Mount Rainier National Park for helping provide access and logistics for survey work in the National Park. We thank Brad Goldman of GoldAero for aiding in the collection of aerial imagery. iv Abstract Changes in upstream sediment delivery or downstream base level can cause propagating geomorphic responses in alluvial river systems. Understanding if or how these changing boundary conditions propagate through a watershed is central to understanding changes in channel morphology, flood conveyance and river habitat suitability. Here, we use a large set of high-resolution topographic surveys to assess coarse sediment delivery and routing in the 1,279 km2 glaciated White River, Washington State, USA. -
O AOTEAROA 1 August, 2007 Professor Allan C Ashworth, Ph.D
OurRef GES-NI 5-07-06/1s93 Your Ref: NGA PoU TAUNAHA O AOTEAROA 1 August,2007 ProfessorAllan C Ashworth,Ph.D. North DakotaState University Fargo,ND 58105-5517 UNITED STATES OF AMERICA Dear ProfessorAshworth, I am writing to formally adviseyou of an official name,Ashworth Glacier, assignedto a glacier with sharplydelineated sides flowing west south-westfrom SupportersRange, Transantarctic Mountains into Mill Glacier,north-east of PlunketPoint. This glacierfalls within the RossSea Region of Antarctica.The namingof this featurehonours your significantcontribution to science(palaeontology and stratigraphy)in Antarctica. Pleasenote that, under a CabinetDirective of 1956,the New ZealandGeographic Board Nga PouTaunaha o Aotearoa(the Board) has the responsibilityfor assigningplace names in the RossSea Region of Antarctica. This placename is thereforerecorded in the Board'sAntarctic place names database. It will alsobe recorded in SCAR'sComposite Gazetteer of Antarcticnames (http://www3.pnra.it/LU0GHl_ANTiSCAR_GAZE). It is my pleasureto provideyou with: . a copy of the GazetteNotice publishedon 3l May 2007page 1514, making Ashworth Glacier official - referhttp://www.linz.govt.nzlcore/placenames/placenamedecisions/20apr2007/index.htmland http://www.gazette.g0vt.nz/Pubforms.nsf/NZGZT/NZGazette5SMay0T.pdf/$file/NZGazette5SMay0T.pdf ; o a reportfrom the Board'sAntarctic Place Names database, listing Ashworth Glacier; . copiesof mapssliowing tlie locationof Ashworth Glacier; and o a coPYof a photoof Ashworth Glacier. Pleasealso note that the Board'sFrameworks document is availablevia the internetand is linkedfrom http://www.linz.govt.nz/rcs/linz/pub/web/root/core/Placenames/frameworks/index,jsp.This documentprovides comprehensiveinformation aboutthe Board arid its policiesand procedures, including a sectionon Antarctic naming,[f you haveany questions, particularly about the place naming process in theRoss Sea Region, pleasefeel freeto contactme. -
Major Middle Miocene Global Climate Change: Evidence from East Antarctica and the Transantarctic Mountains
Major middle Miocene global climate change: Evidence from East Antarctica and the Transantarctic Mountains A.R. Lewis† D.R. Marchant Department of Earth Sciences, Boston University, Boston, Massachusetts 02215, USA A.C. Ashworth Department of Geosciences, North Dakota State University, Fargo, North Dakota 58105, USA S.R. Hemming M.L. Machlus Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA ABSTRACT Keywords: alpine glaciers, geomorphology, understanding the full role of the Antarctic cryo- Dry Valleys, Miocene, till, volcanic ash, Antarc- sphere in this global climate event. Compari- We present a glacial record from the west- tica, Olympus Range, cold-based glaciers. son of this new glacial record to high-latitude ern Olympus Range, East Antarctica, that records elsewhere on the continent (e.g., Roc- documents a permanent shift in the thermal INTRODUCTION chi et al., 2006) and to offshore marine records regime of local glaciers, from wet- to cold- (e.g., Shevenell et al., 2004) will help establish based regimes, more than 13.94 m.y. ago. The Antarctic cryosphere prior to late Neo- the time-transgressive nature of the middle Mio- This glacial record provides the fi rst terres- gene time was substantially different from that cene climate transition and defi ne its role in trial evidence linking middle Miocene global of today. The volume of the East Antarctic Ice altering landscape development in mountainous climate cooling to a permanent reorganiza- Sheet varied signifi cantly over time scales as regions of Antarctica (e.g., Hicock et al., 2003; tion of the Antarctic cryosphere and to subse- short as 100 k.y. -
USGS Open-File Report 2007-1047 Extended Abstract
U.S. Geological Survey and The National Academies; USGS OF-2007-1047, Extended Abstract 135 Major middle Miocene climate change and the extinction of tundra communities: Evidence from the Transantarctic Mountains A. R. Lewis,1 D. R. Marchant,2 A. C. Ashworth,1 S. R. Hemming,3 and M. L. Machlus3 1Department of Geosciences, North Dakota State University, Fargo, ND 58105, U.S.A. ([email protected]; [email protected]) 2Department of Earth Sciences, Boston University, Boston, MA 02215, U.S.A. ([email protected]) 3Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, U.S.A. ([email protected]; [email protected]) Summary We present a glacial record from the western Olympus Range, East Antarctica, that documents a permanent shift in the thermal regime of local glaciers, from wet to cold based, between 14.11 and 13.94 million years ago (Ma). The record includes classic wet-based tills interbedded with fossil-rich glaciolacustrine deposits overlain by a series of cold-based drifts. Chronologic control comes from 40Ar/39Ar analyses of six in-situ volcanic ash deposits. The shift from wet- to cold-based glaciation reflects a drop in mean annual temperature of 20 to 30 ˚C and is shown to precede one or more major episodes of ice-sheet expansion across the region sometime between 13.62 and 12.44 Ma. Major implications are 1) that atmospheric cooling preceded, and thus may have triggered, maximum overriding of the polar East Antarctic Ice Sheet and 2) that complex terrestrial communities became extinct in this sector of the Transantarctic Mountains at ~14 Ma. -
The Holocene Glacial History of Dart Glacier, Southern Alps, New Zealand
The Holocene Glacial History of Dart Glacier, Southern Alps, New Zealand Lisa Holly Dowling A thesis submitted to Victoria University of Wellington in partial fulfilment of requirements for the degree of Master of Science in Physical Geography School of Geography, Environment and Earth Sciences Victoria University of Wellington 2019 Abstract ABSTRACT Mountain glaciers are sensitive climate indicators, as climate variability drives mass changes that are expressed in glacier length fluctuations. These length changes are preserved in the geological record, thus offering the potential to generate new palaeoclimate proxy data that can be used to extend instrumental climate records. This study presents geomorphological mapping and cosmogenic 10Be surface exposure dating of the Holocene moraines at Dart Glacier, New Zealand. These findings show that an early Holocene advance (~6 km longer than present-day) took place ~7817 ± 336 years ago. Moraine ages also show that a more restricted glacier readvance (~4 km longer than present-day) occurred ~321 ± 44 years ago. Through better constraining the timing and magnitude of Holocene glacier length changes, we extend the ~100-year history of observational records in the upper Dart valley. Net retreat of Dart Glacier during the Holocene is consistent with other moraine chronologies from New Zealand, which supports existing hypotheses that suggest summer insolation was the dominant driver of multi-millennial climate change at southern mid-latitudes during the current interglacial. Individual moraine forming events at Dart Glacier also coincide with moraine ages from several other catchments in the Southern Alps and likely reflect shorter-term (decadal-centennial-scale) climatic changes. The new geological record constraints of length changes at Dart Glacier offer the opportunity to test such hypotheses more formally using physics-based modelling. -
December 2019 : Quaternary Perspectives
T H E I N Q U A N E W S L E T T E R Quaternary Perspectives Contents December 2019 - Issue No 27 XXth INQUA XXI INQUA New INQUA New INQUA Quaternary EDITORS Congress Dublin Congress Rome Executive ECR Committee International 500 Dr Guido Stefano Mariani [email protected] Pages 1-3 Page 4 Committee Page 9 Pages 10-12 and the other INQUA ECR Committee members Pages 5-8 Coastal and Marine Humans and Palaeo-climate Stratigraphy and Terrestrial Processes, Quaternary Perspectives website Processes Biosphere Page 18 Chronology Deposits and History Pages 13-15 Pages 16-17 Page 19 Pages 20-23 Perspectives on the XXth INQUA Congress Dublin, Ireland INQUA Congress XX is in the books and my sense is that for all those who attended it was a great success. The meeting was organized by the Irish Quaternary Association (IQUA). A team headed up by Pete Coxon (Ireland), and consisting of Fraser Mitchell (Ireland), Keith Bennet (UK), Catherine Dalton (Ireland), Steve McCarron (Ireland) and others orchestrated a program of symposia, plenary lectures, field trips and social events that was first-rate. The management of events was in the very capable hands of Keynote PCO. The organization started almost immediately following the congress in Nagoya, Japan, and the hard work of the last four years paid off with a very well-organized scientific meeting. The congress got off to a great start with an INQUA presidents former and current attending the INQUA Congress: from left to right, Nat Rutter (1987-1991), John Clague (2003-2007), Allan Chivas (2007- 2011), Margaret Avery (2011-2015), Allan Ashworth (2015-2019), and Thijs van Kolfschoten (2019 - ).