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Road Biking Guide
SUGGESTED ITINERARIES QUICK TIP: Ride your bike before 10 a.m. and after 5 p.m. to avoid traffic congestion. ARK JASPER NATIONAL P SHORT RIDES HALF DAY PYRAMID LAKE (MAP A) - Take the beautiful ride THE FALLS LOOP (MAP A) - Head south on the ROAD BIKING to Pyramid Lake with stunning views of Pyramid famous Icefields Parkway. Take a right onto the Mountain at the top. Distance: 14 km return. 93A and head for Athabasca Falls. Loop back north GUIDE Elevation gain: 100 m. onto Highway 93 and enjoy the views back home. Distance: 63 km return. Elevation gain: 210 m. WHISTLERS ROAD (MAP A) - Work up a sweat with a short but swift 8 km climb up to the base MARMOT ROAD (MAP A) - Head south on the of the Jasper Skytram. Go for a ride up the tram famous Icefields Parkway, take a right onto 93A and or just turn back and go for a quick rip down to head uphill until you reach the Marmot Road. Take a town. Distance: 16.5 km return. right up this road to the base of the ski hill then turn Elevation gain: 210 m. back and enjoy the cruise home. Distance: 38 km. Elevation gain: 603 m. FULL DAY MALIGNE ROAD (MAP A) - From town, head east on Highway 16 for the Moberly Bridge, then follow the signs for Maligne Lake Road. Gear down and get ready to roll 32 km to spectacular Maligne Lake. Once at the top, take in the view and prepare to turn back and rip home. -
Arctic West Summer 2007 USCGC HEALY (WAGB-20) 03 Apr – 30 Sept 2007 Cruise Report
Arctic West Summer 2007 USCGC HEALY (WAGB-20) 03 Apr – 30 Sept 2007 Cruise Report Front Cover: HEALY conducts flight operations off the coast of Kodiak, Alaska, as seen by the aircrew of an HH-60J medium-range helicopter. '1519 CommandingOfficer AlaskanWay South usccc HEALY(WAGB-2o) Seattle,WA 98134 H;';3,3lXtTl**@ Phone:(206) 217-6300 8lr'#o'"'ll8*l/ Fax (206)217-6309 16155 17Mar 2008 HEALY (WAGB-2O) To: CG PACAREA Subj: ARCTICWEST SUMMER 2OO7 CRUISE REPORT Ref: (a) PolarIcebreaker Cruise Reports, COMDTINST 16155.28 1. This reportis submittedin accordancewith reference(a) andcovers the periodfrom 03 April 2007to 30 September2007. 2. HEALY completedthree missions to supportArctic researchduring the Arctic West Summer 2007(AWS-07) deployment. The first mission,HLY 07-01,was conducted in supportof the BeringEcosystern Study, or B-E-S-T. Scientificresearch objectives for the missionincluded charactenzationof ice; hydrographicand nutrient analysis of ice-edgeand ice-free regions; planktonidentification; and tracking of nutrientlevels. HEALY operatedfor 32 daysin the centralBering Seaand the areabounded by the InternationalDate Line, St. LawrenceIsland, Nunivak Islandand the Pribilof Islands,visiting a total of 216stations. The embarkedcivilian helicopterprovided ice reconnaissance,assisted scientists in conductingmarine mammal surveys,and enabled numerous passenger transfers to-and-from nearby island communities. HEALY's secondmission, HLY 07-02,continued a long-term(1950-present) assessment of deep seabenthos in the BeringSea. Scientistsperformed numerous over-the-side evolutions, includingVan Veengrabs, bottom trawls, HAPS cores, CTD casts,and plankton net tows. The third andfinal missionof the 2007deployment, HLY 07-03,comprised a detailedgeophysical surveyof the seafloornorth of Barrow,AK. To facilitatemapping of specificbenthic features, scientistsprovided tracklines for the Officerof the Deck (OOD)on the Bridgeto follow, or positionedthe cursoron HEALY's SeaBeamdisplay and asked the OOD to proceedtoward the cursor. -
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air Canada (Alberta – VE6/VA6) Association Reference Manual (ARM) Document Reference S87.1 Issue number 2.2 Date of issue 1st August 2016 Participation start date 1st October 2012 Authorised Association Manager Walker McBryde VA6MCB Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged Page 1 of 63 Document S87.1 v2.2 Summits on the Air – ARM for Canada (Alberta – VE6) 1 Change Control ............................................................................................................................. 4 2 Association Reference Data ..................................................................................................... 7 2.1 Programme derivation ..................................................................................................................... 8 2.2 General information .......................................................................................................................... 8 2.3 Rights of way and access issues ..................................................................................................... 9 2.4 Maps and navigation .......................................................................................................................... 9 2.5 Safety considerations .................................................................................................................. -
Table of Contents. Letter of Transmittal. Officers 1910
TWELFTH REPORT OFFICERS 1910-1911. OF President, F. G. NOVY, Ann Arbor. THE MICHIGAN ACADEMY OF SCIENCE Secretary-Treasurer, GEO. D. SHAFER, East Lansing. Librarian, A. G. RUTHVEN, Ann Arbor. CONTAINING AN ACCOUNT OF THE ANNUAL MEETING VICE-PRESIDENTS. HELD AT Agriculture, CHARLES E. MARSHALL, East Lansing. Geography and Geology, W. H. SHERZER, Ypsilanti. ANN ARBOR, MARCH 31, APRIL 1 AND 2, 1910. Zoology, A. S. PEARSE, Ann Arbor. Botany, C. H. KAUFFMAN, Ann Arbor. PREPARED UNDER THE DIRECTION OF THE Sanitary and Medical Science, GUY KIEFER, Detroit. COUNCIL Economics, H. S. SMALLEY, Ann Arbor. BY PAST-PRESIDENTS. GEO. D. SHAFER DR. W. J. BEAL, East Lansing. Professor W. H. SHERZER, Ypsilanti. BRYANT WALKER, ESQ. Detroit. BY AUTHORITY Professor V. M. SPALDING, Tucson, Arizona. LANSING, MICHIGAN DR. HENRY B. BAKER, Holland. WYNKOOP HALLENBECK CRAWFORD CO., STATE PRINTERS Professor JACOB REIGHARD, Ann Arbor. 1910 Professor CHARLES E. BARR, Albion. Professor V. C. VAUGHAN, Ann Arbor. Professor F. C. NEWCOMBE, Ann Arbor. TABLE OF CONTENTS. DR. A. C. LANE, Tuft's College, Mass. Professor W. B. BARROWS, East Lansing. DR. J. B. POLLOCK, Ann Arbor. Letter of Transmittal .......................................................... 1 Professor M. H. W. JEFFERSON, Ypsilanti. DR. CHARLES E. MARSHALL, East Lansing. Officers for 1910-1911. ..................................................... 1 Professor FRANK LEVERETT, Ann Arbor. Life of William Smith Sayer. .............................................. 1 COUNCIL. Life of Charles Fay Wheeler.............................................. 2 The Council is composed of the above named officers Papers published in this report: and all Resident Past-Presidents. President's Address—Outline of the History of the Great Lakes, Frank Leverett.......................................... 3 On the Glacial Origin of the Huronian Rocks of WILLIAM SMITH SAYER. -
Washington Division of Geology and Earth Resources Open File Report 86-2, 34 P
COAL MATURATION AND THE NATURAL GAS POTENTIAL OF WESTERN AND CENTRAL WASHINGTON By TIMOTHY J. WALSH and WILLIAMS. LINGLEY, JR. WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 91-2 MARCH 1991 This report has not been edited or reviewed for conformity with Division of Geology and Earth Resources standards and nomenclature. ''llailal WASHINGTONNatural STATE Resources DEPARTMENT OF Brian Boyle ~ Comm1SSioner ol Public Lands Art Stearns Supervisor Division of Geology and Earth Resources Raymond Lasmanis. State Geologist CONTENTS Page Abstract ...................................................... 1 Introduction 1 Tertiary stratigraphy .............................................. 3 Structure as determined from mine maps ................................. 8 Thermal maturation as determined from coal data . 8 Timing of thermal maturation . 16 Mechanisms of heat flow . 17 Exploration significance ............................................ 17 Conclusions 19 References cited . 20 ILLUSTRATIONS Figure 1: Map showing distribution of Ulatisian and Narizian fluvial and deltaic rocks in western and central Washington . 2 Figure 2: Plot of porosity versus depth, selected wells, Puget and Columbia Basins 4 Figure 3: Correlation chart of Tertiary rocks and sediments of western and central Washington . 5 Figure 4: Isopach of Ulatisian and Narizian surface-accumulated rocks in western and central Washington . 7 Figure 5: Isorank contours plotted on structure contours, Wingate seam, Wilkeson-Carbonado coalfield, Pierce County . 9 Figure -
Intoduction to SNOW PASS - GMC 2003
Intoduction to SNOW PASS - GMC 2003 Welcome to Snow Pass. This is the first GMC to be held at this location, and as far as we can ascertain, you are only the second group to have ever camped amongst this group of lakes. Many GMC’s are situated in valleys; however, this site is unusual as you are on the Continental Divide at an E-W “pass” between the Sullivan and Athabasca rivers, this is the arbitrary division between the Columbia Icefield to the south and the Chaba/Clemenceau Icefields to the north. But, you are also at a N-S pass between the Wales and “Watershed” glaciers, so you are at a “four way intersection” and from Base Camp you can access seven (7) different glacier systems. An intriguing local feature is the snout of the “Watershed” glacier, which actually divides so that it flows both west to join the Wales Glacier and thus drains to the Pacific and also turns east and feeds to the Arctic, which is why it is called the “Watershed” Glacier. In 2003, it may not be too obvious why in 1919 the Alberta/British Columbia Interprovincial Survey called this location “Snow Pass” but in the 1930’s (and even ? the early 1950’s) your Base Camp was still completely ice covered! There was permanent ice/snow from the “Aqueduct” to the “Watershed” to the “Toronto” Glaciers, an area of snow 5 km E-W and 10km N-S. Thus, in 1919, it really was a “snow pass”. See the appended “deglaciation” map. There is a wonderful photograph taken from the summit of Sundial peak in 1919 in the A/BC Volume, p. -
Volcanism and Igneous Intrusion
PNL-2882 UC-70 3 3679 00053 2145 .. ' Assessment of Effectiveness of Geologic Isolation Systems DISRUPTIVE EVENT ANALYSIS: VOLCANISM AND IGNEOUS INTRUSION B. M. Crowe Los Alamos Scientific. Laboratory August 1980 Prepared for the Office of Nuclear Waste Isolation under its Contract with the U.S. Department of Energy Pacific Northwest Laboratory Richland, Washington 99352 PREFACE Associated with commercial nuclear power production in the United States is the generation of potentially hazardous radioactive waste products. The Department of Energy (DOE), through the National Waste Terminal Storage (NWTS) Program and the Office of Nuclear Waste Isolation (ONWI), is seeking to develop nuclear waste isolation systems in geologic formations. These underground waste isolation systems will preclude contact with the biosphere of waste radionuclides in concentrations which are sufficient to cause deleterious impact on humans or their environments. Comprehensive analyses'of specific isolation systems are needed to assess the post-closure expectations of the systems. The Assessment of Effectiveness of Geologic Isolation Systems (AEGIS) .' Program has been established for developing the capability of making those analys;s! Among the analysis'required for the system evaluation is the detailed assessment of the post-closure performance of nuclear waste repositories in geologic formations. This assessment is concerned with aspects of the nuclear program which previously have not been addressed. The nature of the isolation systems (e.g., involving breach scenarios and transport through the geosphere) and the great length of time for which the wastes must be controlled dictate the development, demonstration, and application of novel assessment capabili ties. The assessment methodology must be thorough, flexible, objective, and scientifically defensible. -
OCR Document
AN INTRODUCTORY PROSPECTING MANUAL K N A O S I A T B N A O S N I I T K A F R Prepared by: J. R. Parker (Staff Geologist, Red Lake Resident Geologist Office, Ministry of Northern Development and Mines) Revised in 2004 and 2007 by: D. P. Parker and B. V. D'Silva (D'Silva Parker Associates) Discover Prospecting July 2007 Original Acknowledgments The author would like to thank K.G. Fenwick, Manager, Field Services Section (Northwest) and M.J. Lavigne, Resident Geologist, Thunder Bay, for initiating this prospecting manual project. Thanks also to the members of the Prospecting Manual Advisory Committee: P. Sangster, Staff Geologist, Timmins; M. Smyk, Staff Geologist, Schreiber-Hemlo; M. Garland, Regional Minerals Specialist, Thunder Bay; P. Hinz, Industrial Minerals Geologist, Thunder Bay; E. Freeman, Communications Project Officer, Toronto; R. Spooner, Mining Recorder, Red Lake; R. Keevil, Acting Staff Geologist, Dorset; and T. Saunders, President, N.W. Ontario Prospector's Association, Thunder Bay for their comments, input and advice. The author also thanks R. Spooner, Mining Recorder, Red Lake, for writing the text on the Mining Act in the "Acquiring Mining Lands" section of this manual. Thanks to B. Thompson, Regional Information Officer, Information and Media Section, Thunder Bay, for assistance in the preparation of slides and his advice on the presentation of the manual. Thanks also to B.T. Atkinson, Resident Geologist, Red Lake; H. Brown, Acting Staff Geologist, Red Lake; M. Garland, Regional Minerals Specialist, Thunder Bay; and M. Smyk, Staff Geologist, Schreiber-Hemlo for editing the manuscript of the manual. -
Dinosaur Provincial Park and Area Tourism Development Plan Study
Final Report Dinosaur Provincial Park and Area Tourism Development Plan Study Submitted to: Canadian Badlands Ltd. Alberta Tourism, Parks and Recreation by IBI Group July 2010 Government of Alberta and Canadian Badlands Ltd. DINOSAUR PROVINCIAL PARK AND AREA TOURISM DEVELOPMENT PLAN STUDY REPORT FINAL REPORT JULY 2010 IBI GROUP FINAL REPORT TABLE OF CONTENTS EXECUTIVE SUMMARY .................................................................................................................... 1 1. INTRODUCTION ...................................................................................................................... 7 1.1 Purpose and Scope of the Study ......................................................................................................... 8 1.2 Study Limitations .................................................................................................................................. 9 1.3 Outline of Report ................................................................................................................................... 9 2. CHARACTERIZATION OF THE STUDY AREA .................................................................... 10 2.1 County of Newell ................................................................................................................................. 13 2.2 City of Brooks ...................................................................................................................................... 16 2.3 Special Area No. 2 .............................................................................................................................. -
Open Kosei.Pdf
The Pennsylvania State University The Graduate School Department of Geosciences GEOCHEMISTRY OF ARCHEAN–PALEOPROTEROZOIC BLACK SHALES: THE EARLY EVOLUTION OF THE ATMOSPHERE, OCEANS, AND BIOSPHERE A Thesis in Geosciences by Kosei Yamaguchi Copyright 2002 Kosei Yamaguchi Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy May 2002 We approve the thesis of Kosei Yamaguchi Date of Signature ____________________________________ _______________________ Hiroshi Ohmoto Professor of Geochemistry Thesis Advisor Chair of Committee ____________________________________ _______________________ Michael A. Arthur Professor of Geosciences ____________________________________ _______________________ Lee R. Kump Professor of Geosciences ____________________________________ _______________________ Raymond G. Najjar Associate Professor of Meteorology ____________________________________ _______________________ Peter Deines Professor of Geochemistry Associate Head for Graduate Program and Research in Geosciences iii ABSTRACT When did the Earth's surface environment become oxic? The timing and mechanism of the rise of atmospheric pO2 level in the early Precambrian have been long debated but no consensus has been reached. The oxygenation of the atmosphere and oceans has significant impacts on the evolution of the biosphere and the geochemical cycles of redox-sensitive elements. In order to constrain the evolution of the atmosphere, oceans, biosphere, and geochemical cycles of elements, a systematic and multidisciplinary -
Chemical Weathering in Highsedimentyielding Watersheds
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110, F01008, doi:10.1029/2003JF000088, 2005 Chemical weathering in high-sediment-yielding watersheds, New Zealand W. Berry Lyons and Anne E. Carey Department of Geological Sciences and Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA D. Murray Hicks NIWA Research, Christchurch, New Zealand Carmen A. Nezat1 Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA Received 3 September 2003; revised 14 September 2004; accepted 30 November 2004; published 15 February 2005. [1] We have determined the chemical erosion yields for fifteen watersheds in New Zealand, ranging in size from 12.2 to 2928 km2. These rates, coupled with previously measured physical erosion yields, allow us to compare these two modes of landscape denudation. The physical erosion yields are some of the highest measured in the world. Although in most instances the chemical erosion yields are only a small fraction of the total erosion yields, the absolute values are very high. Our data strongly support the notion that chemical erosion rates are greatly influenced by the yield of physical erosion and that the rapid production of fresh surfaces as a result of high physical erosion rates and subsequent denudation is critical to the high chemical erosion yields observed. Citation: Lyons, W. B., A. E. Carey, D. M. Hicks, and C. A. Nezat (2005), Chemical weathering in high-sediment-yielding watersheds, New Zealand, J. Geophys. Res., 110, F01008, doi:10.1029/2003JF000088. 1. Introduction Vance et al., 2003]. In general, the net, large-scale erosional potential of a landscape is thought to increase with precip- [2] Over the past decade, a debate has occurred regard- itation, drainage area and slope [Montgomery et al., 2001]. -
Bulletin 39: the Metal Resources of New Mexico and Their Economic
BULLETIN 3 9 The Metal Resources of New Mexico and Their Economic Features Through 1954 A revision of Bulletin 7, by Lasky and Wootton, with detailed information for the years 1932-1954 BY EUGENE CARTER ANDERSON 1957 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS EX OFFICIO THE HONORABLE EDWIN L. MECHEM………...Governor of New Mexico MRS. GEORGIA L. LUSK ......................Superintendent of Public Instruction APPOINTED MEMBERS ROBERT W. BOTTS ....................................................................Albuquerque HOLM O. BURSUM, JR. .....................................................................Socorro THOMAS M. CRAMER .................................................................... Carlsbad JOHN N. MATHEWS, JR. ...................................................................Socorro RICHARD A. MATUSZESKI ......................................................Albuquerque Contents Page INTRODUCTION .......................................................................................................... 1 Purpose and Scope of Bulletin ..................................................................................... 1 Other Reports Dealing With the Geology and Mineral Resources of New Mexico ......................................................................................................