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Vol 8, Issue 2, June 2009
mag30.qxd 05/05/2009 17:46 Page 1 MAGAZINE OF THE GEOLOGISTS’ ASSOCIATION Volume 8 No. 2 June 2009 Appeal for the Archives WSGS Study Tour of Guernsey Meetings July/October ROCKWATCH News Awards Proceedings of the GA Bernard Leake Retires Getting the most from the PGA Dates for your Diary Presidential Address/Lecture Reports GA Trip to Chafford Hundred Book Reviews CIRCULAR 979 mag30.qxd 05/05/2009 17:45 Page 2 Magazine of the Geologists’ Association From the President Volume 8 No.2, 2009 In writing the June presidential report, I am reminded of the vital role that the GA Published by the plays in upholding the importance of geology on a range of scales, from local Geologists’ Association. to international. For example, the GA can serve as a point of contact to provide Four issues per year. CONTENTS critical information on key geological ISSN 1476-7600 sequences that are under threat from 3. The Association insensitive development plans - in short, Production team: JOHN CROCKER, acting as an expert witness. This does Paula Carey, John Cosgrove, New GA Awards not necessarily entail opposing develop- Vanessa Harley, Bill French 4. GA Meetings July/October ment but rather looking for opportunities to enhance geological resources for 5. Awards Printed by City Print, Milton Keynes future study while ensuring that they are 6. Bernard Leake Retires appropriately protected. In addition, a major part of our national earth heritage The GEOLOGISTS’ ASSOCIATION 7. Dates for your Diary is preserved within our museums and in does not accept any responsibility for 8. -
85106 Magazine Vol 8
mag31.qxd 17/08/2009 20:08 Page 1 MAGAZINEMAGAZINE OFOF THETHE GEOLOGISTS’GEOLOGISTS’ ASSOCIAASSOCIATIONTION Volume 8 No. 3 September 2009 FESTIVAL OF GEOLOGY Festival Field Trips Future Lectures Report of Lectures Rockwatch Book Reviews Finds at Portishead Lyme Regis Festival CIRCULAR 980 Tell us about yourself Mole Valley Celebrations Curry Fund support for...... Suttona Antiquior London Quaternary Lectures Bob Stoneley - thanks Pliocene Forest mag31.qxd 12/08/2009 16:19 Page 2 Magazine of the Geologists’ Association From the President Volume 8 No. 3, 2009 Summer is generally a quiet time for Published by the news and therefore an excellent oppor- tunity to get out and about on fieldwork Geologists’ Association. CONTENTS at home or overseas. I have recently become interested in exploring more of Four issues per year. the famous fossil-rich Pleistocene caves ISSN 1476-7600 3. The Association in the south-west of England and have 4. FESTIVAL OF GEOLOGY Production team: JOHN CROCKER, just returned from a couple of weeks 5. Festival Field Trips excavating in a new cave in Somerset Paula Carey, John Cosgrove, 6. Future Lectures where we are finding abundant fossil Vanessa Harley, Bill French 7. Report March/April Lectures material, including wild horse, red deer, mountain hare and many thousands of 8. Rockwatch Printed by City Print, Milton Keynes rodent remains that date to the very 9. Book Review end of the last Ice Age, around 14,500 10. Finds at Portishead years ago. The vertebrate assemblage The GEOLOGISTS’ ASSOCIATION Lyme Regis Festival will provide an important means of does not accept any responsibility for 11. -
Summer 2021 Long Trail News
NEWS Quarterly of the Green Mountain Club SUMMER 2021 555 New End-to-Enders The Most Ever Recorded [FROM AGE 7 TO 80] CONTENTS Summer 2021, Volume 81, No. 2 The mission of the Green Mountain Club is to make the Vermont mountains play a larger part in the life of the people by protecting and maintaining the Long Trail System and fostering, through education, the stewardship of Vermont’s hiking trails and mountains. Quarterly of the Green Mountain Club Michael DeBonis, Executive Director Chloe Miller, Communications Manager & Long Trail News Editor Richard Andrews, Volunteer Copy Editor Sylvie Vidrine, Graphic Designer Green Mountain Club 4711 Waterbury-Stowe Road Waterbury Center, Vermont 05677 Phone: (802) 244-7037 Fax: (802) 244-5867 E-mail: [email protected] Website: greenmountainclub.org The Long Trail News is published by The Green Mountain Club, Inc., a nonprofit organization founded in 1910. In a 1971 Joint Resolution, the Vermont Legislature Julia LanzDuret-Hernandez on Mount Mansfield. designated the Green Mountain Club the “founder, sponsor, defender and protector of the Long Trail System...” FEATURES Contributions of manuscripts, photos, illustrations, and news are welcome from ❯ The Mountains That Made Me members and nonmembers. 5 by Julia LanzDuret-Hernandez The opinions expressed byLTN contributors are not necessarily those of GMC. 6 ❯ Congratulations to the 2020 End-to-Enders The Long Trail News (USPS 318-840) is published quarterly by The Green Mountain and Side-to-Siders Club, Inc., 4711 Waterbury-Stowe Road, ❯ Waterbury Center, VT 05677. Periodicals 8 A Day in the Life: Long Trail Thru-Hiker postage paid at Waterbury Center, VT, and additional offices. -
1992 October
VERMONT ARCHAEOLOGICAL SOCIETY NEWSLETTER Number 70 October 1992 the Ticonderoga Ferry operates from and secured VAS Annual Meeting there in the water. It remained there until the late on November 7 fall of 1991, when it was removed to Chimney Point by the DHP. At this time it still is at the Chimney The 1992 Annual Meeting of the VAS will be Point site, but there are plans to move it to Plymouth, held on Saturday, November 7, in Burlington, Vermont, and store it under cover there until such possibly at the Econolodge.Joe Popecki, Vie time as it is determined how to preserve it and Rolando, and Bob Sloma are working on the site exhibit it. selection and program. The final announcement plus the slate of candidates for the Board will be Meanwhile, Bruce Hedin, a Board member of the mailed in early October. Mount Independence Coalition, realized that he had seen another log of similar configuration the previous October in Catfish Bay. He brought this to the atten- Bridge Footings Slip tion of the President of MIC, Bernie Noble. Both of by Bernie Noble them went to Catfish Bay in September of 1991 to Mount Independence Coalition examine the second log more closely. On July 28, 1991 at the northern end of Mount In- Measurements were done on the log, detailed draw- dependence, a log was found floating near the shore. ings were made, and photographs were taken in order It was examined by members of the Division for to document the artifacts. The Catfish Bay log was Historic Preservation, officials from the Fort quite different from the one which floated ashore in Ticonderoga Association, various re-enactors and July. -
Žemynų Geografijos Pratybos
LIETUVOS EDUKOLOGIJOS UNIVERSITETAS GAMTOS MOKSLŲ FAKULTETAS BENDROSIOS GEOGRAFIJOS KATEDRA Virginijus Gerulaitis Žemynų geografijos pratybos Vilnius, 2013 - - Apsvarstyta ir rekomenduota spausdinti Lietuvos edukologi jos universiteto Gamtos mokslų fakulteto Bendrosios geogra fijos katedros posėdyje 2012 m. lapkričio 6 d. (protokolo Nr. 4) ir Lietuvos edukologijos universiteto Gamtos mokslų fakulteto tarybos posėdyje 2012 m. gruodžio 9 d. (protokolo Nr. 9). Recenzavo: doc. Mykolas Mikalajūnas (Lietuvos edukologijos universiteto Bendrosios geografijos katedra), dr. Regina Morkūnaitė (Geologijos ir geografijos institutas) © Virginijus Gerulaitis, 2013 © Leidykla „Edukologija“, 2013 ISSN 2335-240X ISBN 978-9955-20-816-7 Turinys Pratarmė 5 Europa 8 Azija 25 Šiaurės Amerika 49 Pietų Amerika 74 Afrika 99 Australija ir Okeanija 112 Antarktida 130 Literatūra 139 Žodynėlis 141 Priedai 154 Žemynų GEOGRAFIJOS PRATYBOS 3 Pratarmė - Žemynų geografija yra regioninės geografijos mokslo šaka, visapusiai tyrinėjanti žemynų gamtinius teritorinius komplek sus, jų kilmę, evoliuciją ir paplitimo dėsningumus. Jos teorinį pagrindą sudaro geografinės sferos teritorinė diferenciacija. - Žemynų gamtos sąlygų apžvalga pagrįsta geografinės sferos - komponentų tarpusavio sąveikos analize. Geografijos mokyto - jų rengimo programoje numatytam „Žemynų geografijos“ kur sui skiriami 7 kreditai, arba 280 valandų. Jis dėstomas ketvir - tame ir penktame semestruose. Nuolatinių studijų programos trečiame semestre 64 valandos skiriamos paskaitoms, 32 va landos – praktiniams darbams ir 64 valandos – savarankiškam darbui. Ištęstinių studijų programos paskaitoms skiriamos 24 valandos, praktiniams darbams – 16 valandų, o 120 valandų numatoma savarankiškam darbui. Ketvirtame semestre šios disciplinos studijoms skiriami trys kreditai: nuolatinių studijų programos 48 valandos skiriamos paskaitoms, 24 valandos – praktiniams darbams ir 48 valandos – savarankiškam darbui. Ištęstinių studijų programos paskaitoms skiriama 18 valandų, praktiniams darbams – 12 valandų ir 90 valandų numatoma savarankiškam darbui. -
THE C OOLIDGE R ANGE SUMMER RECREATION TR AILS Legend Giff
VERMONT THE COOLIDGE RANGE Long Trail North 100 Tucker Johnson 2000 Thundering North SUMMER RECREATION TRAILS Brook Rd Willard Gap Giord Woods Kent Pond Coolidge State Forest State Park Giord Woods State Park 3 Coolidge State Park Deer Leap Mtn Plymsbury Wildlife Management Area 2782’ Rd River Green Mountain National Forest Deer Leap Old Maine Jct. Appalachain Trail Corridor Overlook Rutland City Forest 2000 k West Hill Rd o o Forest Legacy Public Access Easments r B t n e 4 K 4 Killington Rd Pico Pond VERMONT 3000 100 3 Wheelerville Rd 4 3800 Churchill Scott Pico Camp/ spring Pico Peak 3957’ Little Pico Gre o k 3110’ at R oaring Bro Ottauquechee River Rams Head Mtn 3618’ East Roaring Brook Rd Brewers Corners Shagback Mtn Brewers Brook 7 Snowdon Peak 2688’ 3592’ 1800 Skye Peak 2000 3816’ 1600 2200 Cooper Lodge Ed dy 2400 Bro ok 2600 4 Killington Peak ok 2800 s ro 4235’ Fall B 3000 3 Bear Mtn Wheelerville Rd Ottauquechee 3262’ River Notch Rd Mendon Peak 3800 3840’ 3600 Little Killington Peak 3939’ 3200 Ma 3000 dden Brook Reservoir Brook Giord Woods State Park Trails VERMONT North VERMONT Shrewsbury Peak 100 100 3710’ Smith Peak ok Robinson Hill ro 3205’ B t n 2747’ e Shrewsbury Peak rg a S 6 Kent Pond 3200 9 Gov. Clement 3000 1 2800 5 2600 Woodard Jockey Hill Reservoir 2400 2640’ Russell Stone Hut Hill CCC Road 1800 Ingalls Hill Russell Hill 1600 2654’ 2545’ 2000 Tinker Brook 8 Black Pond ko Thundering T ro Brook Rd i n B 2200 k e r 1000 500 0 1000 2000 4 feet Tin Shanty Rd Shanty Tin Black River North Coolidge State Park Trails Upper Cold River Rd Burnt Mtn 2803’ VERMONT 1200 100A 2000 Cold River Rd 2 Northam Rd Round Top Mtn Rd 1400 VERMONT North Shrewsbury Old Plymouth Rd 100 k to Coolidge State Park oo Br ing via Rt 100A 3 mi. -
110 Woodhaven Place Oberlin, Ohio 44074 28 July 1989 End-To-End
110 Woodhaven Place Oberlin, Ohio 44074 28 July 1989 End-to-End Committee Green Mountain Club 43 State Street, P.O. Box 889 Montpelier, Vermont 05602 Hello: I am surprised, as I review my memories of twenty-one years of backpacking, to find that I have taken only five hikes in Vermont. Somehow of all the states and all the trails and all the terrains I have hiked, it is the Green Mountains which are, to me, the most varied, the most lovely, the most precious. Other backpacking trips are visits away; on the Long Trail I am at home. This explains, I am sure, why in those five trips (indeed, in only three of them) I have completely covered the Long Trail. With this letter I am applying for end-to-end certification. I have attached a brief report detailing my daily activities. Sincerely, Dan Styer 1 End-to-End Report Dan Styer 1982: Sherburne Pass to Camel's Hump June 21 Bus to Rutland, hitchhike to Sherburne Pass. Walk in about a quarter mile and camp. June 22 My first sighting of Braun's Holly Fern. At David Logan Shelter, a hummingbird flies among the Cow-Parsnip. Sleep alone there. Torrential downpour at night, during which porkie enters shelter. June 23 Rain on-and-off all day. My first sightings of Twisted Stalk, of White Bog Orchis (Habenaria dilatata), and of Three-toothed Cinquefoil. Impress a family at Sunrise Shelter by building a fire in the soaking wet woods. Slip and fall on wet puncheon, hurting knee. Sleep at Sucker Brook Shelter, which is full. -
Cretaceous Intrusions and Rift Features in the Champlain Valley of Vermont
University of New Hampshire University of New Hampshire Scholars' Repository New England Intercollegiate Geological NEIGC Trips Excursion Collection 1-1-1987 Cretaceous Intrusions and Rift Features in the Champlain Valley of Vermont McHone, J. Gregory Follow this and additional works at: https://scholars.unh.edu/neigc_trips Recommended Citation McHone, J. Gregory, "Cretaceous Intrusions and Rift Features in the Champlain Valley of Vermont" (1987). NEIGC Trips. 418. https://scholars.unh.edu/neigc_trips/418 This Text is brought to you for free and open access by the New England Intercollegiate Geological Excursion Collection at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in NEIGC Trips by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. B - 5 CRETACEOUS INTRUSIONS AND RIFT FEATURES IN THE CHAMPLAIN VALLEY OF VERMONT J. Gregory Mcflone Department of Geological Sciences University of Kentucky Lexington, KY 40506-0059 INTRODUCTION On this field trip we will examine sites near Burlington, Vermont where alkalic dikes and fractures are exposed that could be related to Cretaceous rifting. The setting of these and many similar features is the structural (as opposed to sedimentary) basin of the Lake Champlain Valley, which invites comparison with younger and better-studied continental rifts, such as the Rio Grande Rift of eastern New Mexico or the Gregory Rift of eastern Africa. The validity of such an interpretation depends upon careful study of the tectonic history of the Valley, especially the timing of faulting and its relation to magmatism. The Lake Champlain Valley between Vermont and New York is from 20 to 50 km wide and 140 km long between the northern Taconic Mountains and the Canadian border. -
APPALACHIAN WORKSHOP Lkmf
G-o9Q eA-w- JQA—vii: Gioj"- kj tzb 4s• IØ So APPALACHIAN WORKSHOP lKMF JNtSTY OF Vth1Oft1T LTOft VT I2;LoXPiItti ir QUEBEC VEROT APPALACHIAN WORKS+OP Apr11 14 - 16, 1989 Kalkin Hall, University of Vermont Burlington, Vermont Co-Sponsored by: The Department of Geology Visiting Lecture Series The Canadian Studies Program The Graduate College, University of Vermont EDITORS Maurice Coipron and Barr,' Doolan Department of Geology • University of Vermont Burlington, Vermont Cover: Perspective block diagram of the Québec- Vermont Orogen (from Dóolan, 1989; see Doolan, this volume). Additional copies are available upon request from: Vermont Geological Society, Inc. P.O. Box 304 twfontpelier, Vermont 05602 PROGRAM AND CONTENTS SATURDA V. APRIL 15, 1989 8:00 - INTRODUCTORY REMARKS I. EVOLUTION OF THE ANCIENT NORTH AMERICAN MARGIN IN THE QUEBEC REENTRANT ............................................................................. 1 Chairperson: Charles A. Ratté 8:15 - Stephen Kumarapeli* and Hillar Pintson: Geochronologic constraints on the timing of rifting and continental breakup at the Sutton Mountains triple junction...........3 8:40 - William M. Dowling: Paleogeographic analysis of the preshelf facies in the Oak Hill and Camels Hump Groups: constraints on syn-rift and post-break-up subsidence in theQuébecreentrant ...........................................................................................................5 9:05 - Charlotte Mehrtens: The Cambrian platform and platform margin in northwestern Vermont..............................................................................................................................8 -
Deer Leap Recreation Opportunity Guide
Green Mountain National Forest Caring for the Land and Serving People Trail Facts: Length: 3.1 mile loop Feature: Views, Appalachian Trail Access Max. Elevation Change: 600 feet USGS maps: Pico Peak Quad Amount of use: Heavy Hiking level: Difficult Average trip time: 1 ½ – 2 hours loop Trail Description: From the parking lot at Sherburne Pass, the hike begins just east of The Inn at Long Trail on the north side of US Route 4. If you park on the south side, use extreme caution crossing US Route 4: it is a busy highway. Please stay on the marked trails. Short-cutting to the Deer Leap overlook is very dangerous. In addition to hiker safety considerations, we ask people to stay out of this lower area to give the eroded, denuded surfaces a chance to "heal" and to protect some areas special to Abenaki people. Follow the Sherburne Pass Trail north to the Junction with the Appalachian Trail at 0.5 miles. The Appalachian Trail North continues to the right in an easterly direction to Gifford Woods State Park (1.0 mile), on its way to New Hampshire and Maine. To continue the Loop, take the Appalachian Trail South, which travels northerly for a short stretch, and you will almost immediately reach the junction with Deer Leap Trail, marked with blue blazes. The Appalachian Trail South continues northerly to its junction with the Long Trail at 0.9 miles. Take the Deer Leap Trail as it climbs quickly to a small ridge and through an open birch forest to another junction at 0.9 miles. -
Cotutelle De Thèse Évolution Tectonique Et
Université du Québec TINŒtS-CJéoressources et Université de Nice-Sophia Antipolis Faculté des Sciences - UMR Géosciences Azur COTUTELLE DE THÈSE ÉVOLUTION TECTONIQUE ET GÉOCHRONOLOGIE 4°ArP9 Ar DE LA ZONE . DE HUMBER INTERNE, APPALACHES DU SUD DU QUÉBEC *** TECTONIC EVOLUTION AND 4°ArP9 Ar GEOCHRONOLOGY OF THE INTERNAL HUMBER ZONE, SOUTHERN QUEBEC APPALACHIANS Par SÉBASTIEN CASTONGUAY, M.Sc. Thèse présentée pour l'obtention du grade conjoint de Philosophiae doctor (ph.D.) en sciences de la terre et Docteur en Sciences (sciences de la terre) Jury d'évaluation Examinateur externe Jacques Malavieille Laboratoire de Géophysique et Tectonique, Université Montpellier II 34095 Cedex 05 Montpellier France Examinateur externe L. Peter Gromet Dept. Geological Sciences, Brown University, Providence, Rhode Island 02912 U.S.A. Président du jury et Michel Malo Examinateur interne Centre Géoscientifique de Québec, INRS Géoressources, Sainte-Foy, QC. GlV 4C7 Canada Directeur de recherche Alain Tremblay Centre Géoscientifique de Québec, INRS Géoressources, Sainte-Foy, QC. GIV 4C7 Canada Directeur de recherche Gilbert Féraud UMR Géosciences Azur, CNRS-Université de Nice Sophia Antipolis 06108 Cedex 02 Nice France Thèse soutenue le 10 décembre 1999 à Sainte-Foy, Québec, Canada. © droits réservés de Sébastien Castonguay, 2000 iii Résumé L'évolution tectonique de la partie interne et métamorphique de la marge laurentienne (zone de Humber) des Appalaches du sud du Québec résulte de la superposition de plusieurs épisodes de déformation et de métamorphisme qui s'étendent de l'Ordovicien moyen jusqu'au Dévonien moyen. Les orogénies taconienne (Ordovicien moyen à tardif) et acadienne (Dévonien moyen à tardif) sont séparées par une activité tectonique silurienne qui était jusqu'à maintenant inconnue. -
OROGRAPHY 9 and Covered with a Coating of Clay Which Smoothed Over Its Inequalities and Concealed Most of the Underlying Rocks
OROGRAPHY 9 and covered with a coating of clay which smoothed over its inequalities and concealed most of the underlying rocks. Since its emergence the surface has been but slightly altered by drainage channels cut across it. Orographical maps of Eastern and Western Canada, showing elevations above sea-level, will be found on pages 8 and 10 of this1 volume. Canadian Shield.—The portion of the Precambrian continent whose exposed surface still forms a large part of Canada has an area of about two and a half million square miles. Its northern border crosses the Arctic archipelago and the eastern lies beyond Baffin island and Labrador and reaches the depressed area occupied by the St. Lawrence river, a short spur or point crossing this valley at the outlet of lake Ontario to join the Adirondack mountains in New York. The southern boundary runs from the spur west to Georgian bay, skirts the north shore of lake Huron and sweeps almost around the ancient depressed area occupied by lake Superior. The western edge, from the lake of the Woods and lake Winnipeg, bears northwest to the western end of lake Athabaska, and passes through the basins occupied by Great Slave and Great Bear lakes, reaching the Arctic ocean east of the Mackenzie River delta. In detail, the surface features of the Canadian Shield are irregular; but, viewed broadly, it has the conforma tion of a great plain, depressed toward the centre and in the north, and slightly elevated along the eastern and southern borders, where it presents a rather steep outward slope.