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Moroccan Climbing: Rock, Sun and Snow
PAUL KNOTT Moroccan Climbing: Rock, Sun and Snow OroCCO fascinates me. It has a rich complexity, retaining an alluring M mystique despite being well travelled and documented. During 1998 and 1999 I was lucky enough to get a real insight into the country and its climbing through a post at the delightful Al Akhawayn University in the Middle Atlas Mountains. Here I give a flavour of the rock climbing, skiing and mountain walking, all of them spiced with the cultural interest inherent in Morocco's mountain country. After three days' driving from the UK, I sped through dry limestone plateaux to Ifrane with its promise of sunshine and snow. I found myself sharing an office with Michael Peyron - Alpine Club member, Atlas guidebook author and Berber expert. Along with other companions, we escaped at weekends to explore the wealth of lesser-known mountains a short drive from the fairy-tale campus. We sought and found crags and mountains with European-style ease of access. For big, unexplored rock climbs one of my favourite places was the Dades Gorge. This was visited by Trevor Jones and Les Brown in 1990, but otherwise seems to have seen little or no climbing. Above Boumalne-de Dades the valley becomes strikingly beautiful, with its kasbahs and its unusual rock features (doigts de singes or monkey fingers) set amongst emerald green jardins. On my first visit we got no further than this; the downpour sent raging torrents across the road and stranded us at Ait-Arbi. We found the doigts disappointing for climbing. I returned some weeks later, to the gorge itself. -
Japan Geoscience Union Meeting 2009 Presentation List
Japan Geoscience Union Meeting 2009 Presentation List A002: (Advances in Earth & Planetary Science) oral 201A 5/17, 9:45–10:20, *A002-001, Science of small bodies opened by Hayabusa Akira Fujiwara 5/17, 10:20–10:55, *A002-002, What has the lunar explorer ''Kaguya'' seen ? Junichi Haruyama 5/17, 10:55–11:30, *A002-003, Planetary Explorations of Japan: Past, current, and future Takehiko Satoh A003: (Geoscience Education and Outreach) oral 301A 5/17, 9:00–9:02, Introductory talk -outreach activity for primary school students 5/17, 9:02–9:14, A003-001, Learning of geological formation for pupils by Geological Museum: Part (3) Explanation of geological formation Shiro Tamanyu, Rie Morijiri, Yuki Sawada 5/17, 9:14-9:26, A003-002 YUREO: an analog experiment equipment for earthquake induced landslide Youhei Suzuki, Shintaro Hayashi, Shuichi Sasaki 5/17, 9:26-9:38, A003-003 Learning of 'geological formation' for elementary schoolchildren by the Geological Museum, AIST: Overview and Drawing worksheets Rie Morijiri, Yuki Sawada, Shiro Tamanyu 5/17, 9:38-9:50, A003-004 Collaborative educational activities with schools in the Geological Museum and Geological Survey of Japan Yuki Sawada, Rie Morijiri, Shiro Tamanyu, other 5/17, 9:50-10:02, A003-005 What did the Schoolchildren's Summer Course in Seismology and Volcanology left 400 participants something? Kazuyuki Nakagawa 5/17, 10:02-10:14, A003-006 The seacret of Kyoto : The 9th Schoolchildren's Summer Course inSeismology and Volcanology Akiko Sato, Akira Sangawa, Kazuyuki Nakagawa Working group for -
Quaternary Glaciations of the Atlas Mountains, North Africa
The University of Manchester Research Quaternary Glaciations of the Atlas Mountains, North Africa DOI: 10.1016/B978-0-444-53447-7.00076-3 Link to publication record in Manchester Research Explorer Citation for published version (APA): Hughes, P. D., Fenton, C. R., & Gibbard, P. L. (2011). Quaternary Glaciations of the Atlas Mountains, North Africa. In Developments in Quaternary Science|Dev. Quat. Sci. (Vol. 15, pp. 1065-1074). Elsevier BV. https://doi.org/10.1016/B978-0-444-53447-7.00076-3 Published in: Developments in Quaternary Science|Dev. Quat. Sci. Citing this paper Please note that where the full-text provided on Manchester Research Explorer is the Author Accepted Manuscript or Proof version this may differ from the final Published version. If citing, it is advised that you check and use the publisher's definitive version. General rights Copyright and moral rights for the publications made accessible in the Research Explorer are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. Takedown policy If you believe that this document breaches copyright please refer to the University of Manchester’s Takedown Procedures [http://man.ac.uk/04Y6Bo] or contact [email protected] providing relevant details, so we can investigate your claim. Download date:03. Oct. 2021 Provided for non-commercial research and educational use only. Not for reproduction, distribution or commercial use. This chapter was originally published in the book Developments in Quaternary Science, Vol.15, published by Elsevier, and the attached copy is provided by Elsevier for the author's benefit and for the benefit of the author's institution, for non- commercial research and educational use including without limitation use in instruction at your institution, sending it to specific colleagues who know you, and providing a copy to your institution’s administrator. -
Quaternary Deposits and Landscape Evolution of the Central Blue Ridge of Virginia
Geomorphology 56 (2003) 139–154 www.elsevier.com/locate/geomorph Quaternary deposits and landscape evolution of the central Blue Ridge of Virginia L. Scott Eatona,*, Benjamin A. Morganb, R. Craig Kochelc, Alan D. Howardd a Department of Geology and Environmental Science, James Madison University, Harrisonburg, VA 22807, USA b U.S. Geological Survey, Reston, VA 20192, USA c Department of Geology, Bucknell University, Lewisburg, PA 17837, USA d Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, USA Received 30 August 2002; received in revised form 15 December 2002; accepted 15 January 2003 Abstract A catastrophic storm that struck the central Virginia Blue Ridge Mountains in June 1995 delivered over 775 mm (30.5 in) of rain in 16 h. The deluge triggered more than 1000 slope failures; and stream channels and debris fans were deeply incised, exposing the stratigraphy of earlier mass movement and fluvial deposits. The synthesis of data obtained from detailed pollen studies and 39 radiometrically dated surficial deposits in the Rapidan basin gives new insights into Quaternary climatic change and landscape evolution of the central Blue Ridge Mountains. The oldest depositional landforms in the study area are fluvial terraces. Their deposits have weathering characteristics similar to both early Pleistocene and late Tertiary terrace surfaces located near the Fall Zone of Virginia. Terraces of similar ages are also present in nearby basins and suggest regional incision of streams in the area since early Pleistocene–late Tertiary time. The oldest debris-flow deposits in the study area are much older than Wisconsinan glaciation as indicated by 2.5YR colors, thick argillic horizons, and fully disintegrated granitic cobbles. -
The Effects of Ice on Stream Flow
LIBRARY COPY DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTI8 SMITH, DIKECTOK WATER-SUPPLY PAPER 337 THE EFFECTS OF ICE ON STREAM FLOW BY WILLIAM GLENN HOYT WASHINGTON GOVERNMENT PRINTING OFFICE 1913 CONTENTS. Page. Introduction____________________________________ 7 Factors that modify winter run-off_______________________ 9 Classification_________________________________ 9 Climatic factors_______________________________ 9 Precipitation and temperature____________________ 9 Barometric pressure__________________________ 17 Chinook winds________________________________ 18 Geologic factors________________________________ 19 Topographic factors______________________________ 20 Natural storage_____________________________ 20 Location, size, and trend of drainage basins____________ 22 Character of streams_________________________ 22 Vegetational factors_____________________________. 23 Artificial control _________________________________ 23 Formation of ice______________________________^____ 24 General conditions ________________________________ 24 Surface ice __ __ __ ___________________ 24 Method of formation____________________________. 24 Length and severity of cold period__________________ 25 Temperature of affluents________________________'__ 26 Velocity of water and. character of bed_______________ 27 Fluctuations in stage__________________________ 27 Frazil______________________________________ 28 Anchor ice_____________________ __________ 29 Effect of ice on relation of stage to discharge_________ ______ 30 The -
Climbing in the Atlas Mountains a Survey
HAMISH BROWN Climbing in the Atlas Mountains A Survey (Plates 24-27) magine a country with eighty per cent sunshine throughout the year, I grand mountain scenery, its rock climbing potential barely touched, all within easy reach, with no political hassles orcostly fees, and a lovely people. It may sound too good to be true but it all exists in Europe's nearest truly exotic foreign country: Morocco. The Atlas Mountains, which sweep across from north-east to south-west, separating 'the desert and the sown', offer a climber's paradise. Quite why the Atlas has suffered neglect by climbers from Britain is hard to understand. Perhaps the names are too difficult - there's no kudos in reporting unpronounceable climbs - or the information is hidden away in French publications. 1 Time the cat escaped from out of the bag. I spent a winter in the Atlas in 1965 and repeated this delight in 1966. Having gone there specifically to climb (Notes in AJ 1966) I ended simply hooked on the whole Atlas ambience and began to wander rather than be restricted to one area. The natural outcome of this was an end-to-end trek 2 in 1995 : 96 days, 900 miles and about 30 peaks bagged. Farfrom rounding off my knowledge, the trip introduced me to a score of new worthy areas to visit and I've had five Atlas months every year since. 3 The scope for climbing is vast. The country must have 50 limestone gorges, miles long and up to 2000 feet deep, each ofwhich would fill volumes ofclimbs if located in Europe, while on the mountains there are crests to be traversed and notable granite faces still virgin. -
Determination of Stream Flow During the Frozen Season
Water-Supply and Irrigation Paper No. 187 Series M, General Hydrographic Investigations, 19 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR DETERMINATION OF STREAM FLOW DURING THE FROZEN SEASON BY H. K. BARROWS AND ROBERT E. HORTON WASHINGTON GOVERNMENT PRINTING OFFICE 190T CONTENTS. Importance of winter records of stream flow.................................. 5 Methods of gaging streams during the open season............................. 6 General statement............'......................................... 6 Weir method ......................................................... 6 Velocity method ...................................................... 6 Slope method......................................................... 7 Conditions during the winter season.......................................... 7 Factors affecting ice formation .......................................... 7 Classification of winter conditions........................................ 8 Duration of ice season ................................................. 9 Change in thickness of ice.............................................. 10 Surface, anchor, and needle ice.......................................... 10 Range of winter gage heights ............................................ 13 Flow of streams under ice cover............................................. 14 General considerations................................................. 14 Friction due to air and ice.............................................. 14 Relative importance -
The Periglaciation of Great Britain Colin K
Cambridge University Press 978-0-521-31016-1 - The Periglaciation of Great Britain Colin K. Ballantyne and Charles Harris Index More information Index Abbot's Salford, Worcestershire, 53 aufeis, see also icings, 70 bimodal flows, see ground-ice slumps Aberayron, Dyfed, Wales, 104 Australia, 179, 261 Binbrook, Lincolnshire, 157 Aberystwyth, Dyfed, Wales, 128, 206, 207 Austrian Alps, 225 Bingham flow, 231 Acheulian hand axes, see hand axes avalanche activity, 219-22; 226-30, 236, 244, Birling Gap, Sussex, 102, 108 Achnasheen, NW Scotland, 233 295, 297 Black Mountain, Dyfed, 231, 234 active layer, see also seasonal thawing, 5, 27, avalanche boulder tongues, 220, 226, 295 Black Rock, Brighton, Sussex, 125, 126 35,41,42,114-18, 140,175 avalanche cones, 220, 226 Black Top Creek, EUesmere Island, Canada, 144 detachment slides, 115, 118, 276 avalanche impact pits, 226 Black Tors, Dartmoor, 178 glides, 118 avalanche landforms, 7, 8 blockfields, 8, 164-9, 171, 173-6, 180, 183, processes, 85-102 avalanche tongues, 227, 228 185,187,188,193,194 thickness, 107-9,281-2 avalanche-modified talus, 226-30 allochthonous, 173 Adwick-Le-Street, Yorkshire, 45, 53 Avon, 132, 134, 138, 139 autochthonous, 174, 182 aeolian, processes, see also wind action, 141, Avon Valley, 138 blockslopes, 173-6, 187, 190 155-60,161,255-67,296 Axe Valley, Devon, 103, 147 blockstreams, 173 aeolian sediments, see also loess and Bodmin Moor, Cornwall, 124, 168 coversands, 55, 96, 146-7, 150, 168, Badwell Ash, Essex, 101 Bohemian Highlands, 181 169, 257-60 Baffin Island, 103, 143,219 -
Glacial Action & Periglacial Landforms
These Slides Accompany the YouTube Video Tutorial: https://www.youtube.com/watch?v=a9V92qwyT2A Glacial Action & Periglacial Landforms www.examrace.com www.doorsteptutor.comwww.examrace.com These Slides Accompany the YouTube Video Tutorial: https://www.youtube.com/watch?v=a9V92qwyT2A Types of Glaciers • Based on Morphology • Based on Thermal • Alpine or Valley Characteristics • Ice Cap • Temperate • Outlet Glaciers • Polar • Ice Sheet • Subpolar • Continental Glacier • IceShelves • Ice Streams • Tidewater Glaciers www.examrace.com www.doorsteptutor.comwww.examrace.com These Slides Accompany the YouTube Video Tutorial: https://www.youtube.com/watch?v=a9V92qwyT2A Calving Serac www.examrace.com www.doorsteptutor.comwww.examrace.com These Slides Accompany the YouTube Video Tutorial: https://www.youtube.com/watch?v=a9V92qwyT2A Iceberg www.examrace.com www.doorsteptutor.comwww.examrace.com These Slides Accompany the YouTube Video Tutorial: https://www.youtube.com/watch?v=a9V92qwyT2A Permafrost •Continuous •Discontinuous •Alpine •Sporadic •Subsea www.examrace.com www.doorsteptutor.comwww.examrace.com These Slides Accompany the YouTube Video Tutorial: https://www.youtube.com/watch?v=a9V92qwyT2A Ground Ice •Pore Ice •Needle Ice •Wedged Ice •Segregated Ice •Intrusive Ice Patterned Ground www.examrace.com www.doorsteptutor.comwww.examrace.com These Slides Accompany the YouTube Video Tutorial: https://www.youtube.com/watch?v=a9V92qwyT2A Palsas Pingos www.examrace.com www.doorsteptutor.comwww.examrace.com These Slides Accompany the YouTube Video Tutorial: https://www.youtube.com/watch?v=a9V92qwyT2A Solifluction Lobes Blockfields or Felsenmeer www.examrace.com www.doorsteptutor.comwww.examrace.com These Slides Accompany the YouTube Video Tutorial: https://www.youtube.com/watch?v=a9V92qwyT2A Rock Glaciers Thermokarst www.examrace.com www.doorsteptutor.comwww.examrace.com. -
Nota Lepidopterologica
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Nota lepidopterologica Jahr/Year: 2012 Band/Volume: 35 Autor(en)/Author(s): Bartsch Daniel Artikel/Article: Revision of types of several species of Bembecia Hübner, 1819 from northern Africa and southwestern Europe (Sesiidae) 125-133 ©Societas Europaea Lepidopterologica; download unter http://www.biodiversitylibrary.org/ und www.zobodat.at Notalepid. 35 (2): 125-133 125 Revision of types of several species of Bembecia Hübner, 1819 from northern Africa and southwestern Europe (Sesiidae) Daniel Bartsch Staatliches Museum fur Naturkunde Stuttgart, Rosenstein 1, 70191 Stuttgart, Germany; [email protected] Received 14 March 2012; reviews returned 18 April 2012; accepted 18 August 2012. Subject Editor: Jadranka Rota. Abstract. The type specimens of Sesia sirphiformis Lucas, 1 849 from Lac Tonga in Algeria and Dipso- sphecia megillaeformis v. tunetana Le Cerf, 1 920 syn. n. from the vicinity of Tunis were examined and found to be conspecific. Bembecia sirphiformis belongs to the B. ichneumoniformis (Denis & Schiffer- müller, 1775) species group and is currently known only from northern Africa. Records from Sicily, Sar- dinia, Corsica, southern Italy, and Morocco (as B. tunetana) are here considered doubtful and may belong to other species. B. astragali (Joannis, 1909) stat. rev., which was described from northern Spain and southern France and was previously considered conspecific with B. sirphiformis, actually appears not to be so closely related to B. sirphiformis and seems to belong to the B. megillaeformis (Hübner, 1813) spe- cies group. B. igueri Bettag & Bläsius, 1998 syn. n. from Morocco is now considered to be a synonym of B. -
Icrar2009.Pdf
ICR ANNUAL REPORT 2009 (Volume 16) - ISSN 1342-0321 - This Annual Report covers from 1 January to 31 December 2009 Editors: Professor: ONO, Teruo Professor: HIRATAKE, Jun Professor: MAMITSUKA, Hiroshi Associate Professor: MATSUDA, Kazunari Assistant Professor: YOSHIDA, Hiroyuki Editorial Staff: Public Relations Section: TANIMURA, Michiko KOTANI, Masayo NAKANO, Yukako TAKEHIRA, Tokiyo Published and Distributed by: Institute for Chemical Research (ICR), Kyoto University Copyright 2010 Institute for Chemical Research, Kyoto University Enquiries about copyright and reproduction should be addressed to: ICR Annual Report Committee, Institute for Chemical Research, Kyoto University Note: ICR Annual Report available from the ICR Office, Institute for Chemical Research, Kyoto University, Gokasho, Uji, Kyoto 611-0011, Japan Tel: +81-(0)774-38-3344 Fax: +81-(0)774-38-3014 E-mail [email protected] URL http://www.kuicr.kyoto-u.ac.jp/index.html Uji Library, Kyoto University Tel: +81-(0)774-38-3010 Fax: +81-(0)774-38-4370 E-mail [email protected] URL http://lib.kuicr.kyoto-u.ac.jp/homepage/japanese/index.htm Printed by: Nakanishi Printing Co., Ltd. Ogawa Higashi-iru, Shimodachiuri, Kamigyo-ku, Kyoto 602-8048, Japan TEL: +81-(0)75-441-3155 FAX: +81-(0)75-417-2050 ICR ANNUAL REPORT 2009 ICR ANNUAL REPORT 2009 (Volume 16) - ISSN 1342-0321 - This Annual Report covers from 1 January to 31 December 2009 Editors: Professor: ONO, Teruo Professor: HIRATAKE, Jun Professor: MAMITSUKA, Hiroshi Associate Professor: MATSUDA, Kazunari Assistant Professor: -
The Nature of Last Glacial Periglaciation in the Channel Islands
Note of a paper read at the Annual Conference of the Ussher Society, January 1998 THE NATURE OF LAST GLACIAL PERIGLACIATION IN THE CHANNEL ISLANDS S. D. GURNEY, H. C. L. JAMES AND P. WORSLEY Gurney, S. D., James, H. C. L. and Worsley, P. The nature of last glacial periglaciation in the Channel Islands. Geoscience in south-west England, 9, 241-249. S.D. Gurney, Department of Geography, H.C.L. James, Department of Science and Technology Education, P. Worsley, Postgraduate Research Institute for Sedimentology, The University of Reading, P.O. Box 227, Reading, RG6 6AB. INTRODUCTION If permafrost extent is a good indicator of the intensity of cold climates, then the ice wedge casts and sand and gravel wedges found in Following the recognition of periglacially induced macro-scale northern France, particularly in Brittany, demonstrate former sedimentary structures and fabrics of deposits of Last Glacial age on Pleistocene cold environmental conditions having extended into that Alderney, a search for analogous features on Guernsey and Jersey has region (van Vliet-Lanë, 1996; van Vliet-Lanoë et al ., 1997). The been undertaken. It has long been known that cold climate related chronology for such periglacial conditions in Brittany, however, mass wasting deposits (head) and aeolian deposits (loess) are common suggests a rather earlier date than for southwest England and the throughout the Channel Islands. Structures specifically related to Channel Islands. For example, Loyer et al . (1995) indicate that during frozen ground, however, either seasonal or perennial, have not Marine Oxygen Isotope Stage (OIS) 6, permafrost extension was rather previously been documented outside Alderney.