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Quaternary of Scotland the GEOLOGICAL CONSERVATION REVIEW SERIES
Quaternary of Scotland THE GEOLOGICAL CONSERVATION REVIEW SERIES The comparatively small land area of Great Britain contains an unrivalled sequence of rocks, mineral and fossil deposits, and a variety of landforms that span much of the earth's long history. Well-documented ancient volcanic episodes, famous fossil sites, and sedimentary rock sections used internationally as comparative standards, have given these islands an importance out of all proportion to their size. These long sequences of strata and their organic and inorganic contents, have been studied by generations of leading geologists thus giving Britain a unique status in the development of the science. Many of the divisions of geological time used throughout the world are named after British sites or areas, for instance the Cambrian, Ordovician and Devonian systems, the Ludlow Series and the Kimmeridgian and Portlandian stages. The Geological Conservation Review (GCR) was initiated by the Nature Conservancy Council in 1977 to assess, document, and ultimately publish accounts of the most important parts of this rich heritage. The GCR reviews the current state of knowledge of the key earth-science sites in Great Britain and provides a firm basis on which site conservation can be founded in years to come. Each GCR volume describes and assesses networks of sites of national or international importance in the context of a portion of the geological column, or a geological, palaeontological, or mineralogical topic. The full series of approximately 50 volumes will be published by the year 2000. Within each individual volume, every GCR locality is described in detail in a self- contained account, consisting of highlights (a precis of the special interest of the site), an introduction (with a concise history of previous work), a description, an interpretation (assessing the fundamentals of the site's scientific interest and importance), and a conclusion (written in simpler terms for the non-specialist). -
Scottish Highlands Hillwalking
SHHG-3 back cover-Q8__- 15/12/16 9:08 AM Page 1 TRAILBLAZER Scottish Highlands Hillwalking 60 DAY-WALKS – INCLUDES 90 DETAILED TRAIL MAPS – INCLUDES 90 DETAILED 60 DAY-WALKS 3 ScottishScottish HighlandsHighlands EDN ‘...the Trailblazer series stands head, shoulders, waist and ankles above the rest. They are particularly strong on mapping...’ HillwalkingHillwalking THE SUNDAY TIMES Scotland’s Highlands and Islands contain some of the GUIDEGUIDE finest mountain scenery in Europe and by far the best way to experience it is on foot 60 day-walks – includes 90 detailed trail maps o John PLANNING – PLACES TO STAY – PLACES TO EAT 60 day-walks – for all abilities. Graded Stornoway Durness O’Groats for difficulty, terrain and strenuousness. Selected from every corner of the region Kinlochewe JIMJIM MANTHORPEMANTHORPE and ranging from well-known peaks such Portree Inverness Grimsay as Ben Nevis and Cairn Gorm to lesser- Aberdeen Fort known hills such as Suilven and Clisham. William Braemar PitlochryPitlochry o 2-day and 3-day treks – some of the Glencoe Bridge Dundee walks have been linked to form multi-day 0 40km of Orchy 0 25 miles treks such as the Great Traverse. GlasgowGla sgow EDINBURGH o 90 walking maps with unique map- Ayr ping features – walking times, directions, tricky junctions, places to stay, places to 60 day-walks eat, points of interest. These are not gen- for all abilities. eral-purpose maps but fully edited maps Graded for difficulty, drawn by walkers for walkers. terrain and o Detailed public transport information strenuousness o 62 gateway towns and villages 90 walking maps Much more than just a walking guide, this book includes guides to 62 gateway towns 62 guides and villages: what to see, where to eat, to gateway towns where to stay; pubs, hotels, B&Bs, camp- sites, bunkhouses, bothies, hostels. -
Wakefield, West Riding: the Economy of a Yorkshire Manor
WAKEFIELD, WEST RIDING: THE ECONOMY OF A YORKSHIRE MANOR By BRUCE A. PAVEY Bachelor of Arts Oklahoma State University Stillwater, Oklahoma 1991 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of MASTER OF ARTS May, 1993 OKLAHOMA STATE UNIVERSITY WAKEFIELD, WEST RIDING: THE ECONOMY OF A YORKSHIRE MANOR Thesis Approved: ~ ThesiSAd er £~ A J?t~ -Dean of the Graduate College ACKNOWLEDGEMENTS I am deeply indebted to to the faculty and staff of the Department of History, and especially the members of my advisory committee for the generous sharing of their time and knowledge during my stay at O.S.U. I must thank Dr. Alain Saint-Saens for his generous encouragement and advice concerning not only graduate work but the historian's profession in general; also Dr. Joseph Byrnes for so kindly serving on my committee at such short notice. To Dr. Ron Petrin I extend my heartfelt appreciation for his unflagging concern for my academic progress; our relationship has been especially rewarding on both an academic and personal level. In particular I would like to thank my friend and mentor, Dr. Paul Bischoff who has guided my explorations of the medieval world and its denizens. His dogged--and occasionally successful--efforts to develop my skills are directly responsible for whatever small progress I may have made as an historian. To my friends and fellow teaching assistants I extend warmest thanks for making the past two years so enjoyable. For the many hours of comradeship and mutual sympathy over the trials and tribulations of life as a teaching assistant I thank Wendy Gunderson, Sandy Unruh, Deidre Myers, Russ Overton, Peter Kraemer, and Kelly McDaniels. -
Run-Of-River Hydro-Electric Schemes in the Highlands a Photostudy of Their Impact on Wild Land and Our Enjoyment of the Mountains March 2019
Run-of-River hydro-electric schemes in the Highlands a photostudy of their impact on wild land and our enjoyment of the mountains March 2019 this is Glen Quoich, one of the most intrusive schemes, formerly wild and secluded, yet conspicuous from the South Cluanie Ridge and the Quoich Munros, in off the Kinloch Hourn road David Jarman - mountain landform research - Ross-shire [email protected] Run-of-River hydro-electric schemes in the Highlands ULLAPOOL slides 11 3 - 11 Glen Quoich 1 12 12 - 17 Gleann Cia-aig, Kinlocharkaig 2 10 18 - 20 Kingairloch 3 13 9 INVERNESS 21 - 24 Auch, Bridge of Orchy 4 8 7 KYLE 25 - 29 Ceannacroc, Glen Moriston 5 6 30 - 34 Gleann nam Fiadh, Affric 6 5 35 - 39 Liatrie pinewood, Glen Cannich 7 1 40 - 43 Carn nan Gobhar, Mullardoch 8 2 44 - 49 Monar Lodge, Strathfarrar 9 FORT WILLIAM 50 - 51 Moruisg, Achnasheen 10 11 52 Fannich Lodge 3 53 - 58 Grudie Bridge, Loch Maree 12 59 - 64 Coulags, Strath Carron 13 4 65 a summing up these schemes just happen to be ones we have come across while going about the Highlands in the last few years - there are many more, and this is not a ‘sample survey’. most of them we consider very or disastrously intrusive, but a few show what can be done, if we have to sacrifice any more of our wild Highlands. weir Gleann nam Fiadh, Affric Gleouraich 1034m 1 Glen Quoich Loch Quoich (c) J Michael Loughridge this is Gleouraich, a popular Munro above Loch Quoich and tucked in behind is Glen Quoich, seen in these old photos from the South Cluanie Ridge, and (inset) from the summit. -
Henges in Yorkshire
Looking south across the Thornborough Henges. SE2879/116 NMR17991/01 20/5/04. ©English Heritage. NMR Prehistoric Monuments in the A1 Corridor Information and activities for teachers, group leaders and young archaeologists about the henges, cursus, barrows and other monuments in this area Between Ferrybridge and Catterick the modern A1 carries more than 50,000 vehicles a day through West and North Yorkshire. It passes close to a number of significant but often overlooked monuments that are up to 6,000 years old. The earliest of these are the long, narrow enclosures known as cursus. These were followed by massive ditched and banked enclosures called henges and then smaller monuments, including round barrows. The A1 also passes by Iron Age settlements and Roman towns, forts and villas. This map shows the route of the A1 in Yorkshire and North of Boroughbridge the A1 the major prehistoric monuments that lie close by. follows Dere Street Roman road. Please be aware that the monuments featured in this booklet may lie on privately-owned land. 1 The Landscape Setting of the A1 Road Neolithic and Bronze Age Monuments Between Boroughbridge and Cursus monuments are very long larger fields A1 Road quarries Catterick the A1 heads north with rectangular enclosures, typically more the Pennines to the west and than 1km long. They are thought to the low lying vales of York and date from the middle to late Neolithic Mowbray to the east. This area period and were probably used for has a rural feel with a few larger ceremonies and rituals. settlements (like the cathedral city of Ripon and the market town of The western end of the Thornborough pockets of woodland cursus is rounded but some are square. -
WESTER ROSS Wester Ross Ross Wester 212 © Lonelyplanet Walk Tooneofscotland’Sfinestcorries, Coire Mhicfhearchair
© Lonely Planet 212 Wester Ross Wester Ross is heaven for hillwalkers: a remote and starkly beautiful part of the High- lands with lonely glens and lochs, an intricate coastline of rocky headlands and white-sand beaches, and some of the finest mountains in Scotland. If you are lucky with the weather, the clear air will provide rich colours and great views from the ridges and summits. In poor conditions the remoteness of the area makes walking a much more serious proposition. Whatever the weather, the walking can be difficult, so this is no place to begin learning mountain techniques. But if you are fit and well equipped, Wester Ross will be immensely rewarding – and addictive. The walks described here offer a tantalising taste of the area’s delights and challenges. An Teallach’s pinnacle-encrusted ridge is one of Scotland’s finest ridge walks, spiced with some scrambling. Proving that there’s much more to walking in Scotland than merely jumping out of the car (or bus) and charging up the nearest mountain, Beinn Dearg Mhór, in the heart of the Great Wilderness, makes an ideal weekend outing. This Great Wilderness – great by Scottish standards at least – is big enough to guarantee peace, even solitude, during a superb two-day traverse through glens cradling beautiful lochs. Slioch, a magnificent peak overlooking Loch Maree, offers a comparatively straightforward, immensely scenic ascent. In the renowned Torridon area, Beinn Alligin provides an exciting introduction to its consider- WESTER ROSS able challenges, epitomised in the awesome traverse of Liathach, a match for An Teallach in every way. -
Beinn Eighe and Liathach for Grandeur: a Visit to Its Lochan Is a Must
H of Wester Ross 1 Gairloch District: from Little Loch Broom to Loch Torridon 1 The central part of Wester Ross, from Little Loch Broom to Loch Torridon, is privileged to have an unmatched collection of mountains – or rather hills, as they are traditionally known in Scotland. The main service centre of this area is Gairloch, from which they can all be reached. The aim of this booklet is to introduce these hills to both active and armchair hill- walkers. It is not a complete guide; for that you need something like the SMC North West Highlands guide, plus a good map. But it contains hints from local knowledge, relevant geological information, and a lot of pictures. Fine weather is assumed (yes, there are fine days here!): if possible, don’t climb these hills without it, unless you enjoy the mere exercise or the navigational challenge, or you are simply bagging summits (p20)! And remember that in snowy winter conditions hill-walking is transformed into a different and more technical sport – mountaineering. Our hills are not high by continental standards, but while the greater ranges are still rising or being worn down (which may take only 50 million years), ours have been carved by ice out of truly ancient rocks: gneiss (p11), amphibolite (p19), sandstone (p23), and quartzite (p27), each with its own distinct character as you walk on it. This geology, everywhere visible, explains why the landscape here is so much rockier, rougher and more varied than the land further east, which was overrun by the softer rock of the mountain-building Moine Thrust (p35). -
The Munro Bagger
The Munro Bagger Fancy testing your walking skills on a hike up Scotland’s towering Munros? At 914 metres (3000ft) the views are immense, so bagging one of these impressive Scottish mountains is something every walker should include on their bucket list. Over the course of a week, your personal mountain guide will assist you in the ascent of 6 of Scotland’s most iconic Munros in the beautiful North West Highlands, whilst staying in luxury lodge or hotel accommodation, with private transfers. Days One to Three The Torridons are an incomparable group of 8 hills between Loch Maree and Loch Torridon, with the big three being Liathach, Beinn Eighe and Beinn Alligin. The Torridons are uniquely photogenic thanks to the isolation of each hill. Day Four Rest day. Day Five and Six Suilven and Ben More Assynt/Conival. Suilven may only be 731 metres high but its remarkable outline makes it one of Scotland’s best known and easily identified mountains. Ben More Assynt and Conival are the only Munros in Assynt and are connected by a fine ridge. Together they give amazing views characteristic of all Assynt Peaks. Ossian Adventures @ossianadventures +(44) 01738 451600 From £3,000 to £5,000 per person. [email protected] Based on a minimum of 4 guests in the party, 7 night stay. ossianadventures.com Please note, a good level of fitness is required. The following is a flavour of what we a can offer. Access to the most private, obtainable castles, palaces, mansions and lodges in Scotland. • Photographic Safari • Private Transfers • North Coast 500 in -
Letters to the Editors Fossil Rock Ghciers Have Not Been Described As
Downloaded from http://sjg.lyellcollection.org/ by guest on September 25, 2021 Letters to the Editors A FOSSIL ROCK GLACIER IN WESTER ROSS SIRS, Fossil rock ghciers have not been described as occurring in Scotland (the present climate does not permit active ones). It is believed that an example exists near Loch Torridon in Wester Ross. The feature begins at the foot of Beinn Alligin in a corrie-like valley head whose rock walls rise very steeply and, finally, precipitously for 500 m or more to culminate at 985 m (Fig. 1). It is composed of pieces of Torridon Sandstone (the bedrock of the area), few of those that can be seen being below boulder size: much of the visible debris is massive blocks up to 5 m or more long. Between the boulders cavities many metres deep penetrate into the interior of the feature and make it extremely difficult to traverse. The debris forms a continuous mass that rises to a maximal height of 12-15 m, is i-2 km long, 400 m wide near its source and tapers gradually to about 200 m near its terminus. It rests on a fairly gentle slope that falls from about 400 m altitude to about 260 m. The edge of the tongue-like mass of material is sharply defined. The surface relief (other than that provided by the blocks themselves) consists of ridges and depres sions, some of the latter being closed. In the NW. half of the feature there are short ill-defined transverse ridges and clearer longitudinal ones. -
Thornborough Final Review
The Prehistoric Society Book Reviews CULT, RELIGION AND PILGRIMAGE ARCHAEOLOGICAL INVESTIGATIONS AT THE NEOLITHIC AND BRONZE AGE MONUMENT COMPLEX OF THORNBOROUGH, NORTH YORKSHIRE BY J HARDING CBA Research Report 174, 2013. 236 pp, 155 figs with 29 col plates (59 figs in digital appendices), 11 tables (32 tables in digital appendices), ISBN 978-1-902771-97-7, pb, £25 This impressive Research Report took me, enthralled, down memory lane. I had been one of a happy band of undergraduates at Oxford University who dug at Dorchester-on-Thames (Oxfordshire) under the inspired leadership of Richard Atkinson in the late 1940s. I maintained my links with Dorchester and Atkinson by sharing directorship of an excavation of the major henge monument there, Big Rings, Site XIII, with an underlying ring-ditch containing a possible timber building, Site XIV (Whittle et al 1992). The Big Rings, its bank between two ditches and opposed entrances, class IIA in Atkinson’s classification, had no obvious analogy in southern England. Arminghall (Norfolk; Clark 1936) is double-ditched, to be sure; but with single entrance and a timber structure within, it was obviously different. Condicote (Gloucestershire), a double-ditched possible henge monument, was almost unknown at that time and its full character has yet to be established (Saville 1983). But we knew of the existence of three close-spaced henge monuments to the north of Ripon in north-east Yorkshire, the Thornborough Circles, which appeared to be identical if a little larger. The Yorkshire sites invited our attention. The Big Rings (with a spectacular Beaker burial positioned outside its northern entrance, Site XII) had also produced Beaker sherds in a primary position in one butt-end of the inner ditch at its southern entrance and it seemed reasonable therefore to attempt a restricted examination of one of the Thornborough Circles to see if all these henges were similar in period and culture. -
Subsidence Hazards Caused by the Dissolution of Permian Gypsum in England: Geology, Investigation and Remediation
SUBSIDENCE HAZARDS CAUSED BY THE DISSOLUTION OF PERMIAN GYPSUM IN ENGLAND: GEOLOGY, INVESTIGATION AND REMEDIATION A H Cooper, British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG. This is a recompiled version of the final draft of the published paper, it is presented with coloured versions of the figures and may differ slighly from the published edited version. Please respect copyright of BGS/NERC and refer to the final published version if you wish to quote the work. Published as: Cooper, AH. 1998. Subsidence hazards caused by the dissolution of Permian gypsum in England: geology, investigation and remediation. 265–275 in: Geohazards in engineering geology, Maund, JG, Eddleston, M (eds.). Geological Society of London. Special Publications in Engineering Geology, 15. ABSTRACT About every three years natural catastrophic subsidence, caused by gypsum dissolution, occurs in the vicinity of Ripon, North Yorkshire, England. Holes up to 35 m across and 20 m deep have appeared without warning. In the past 150 years, 30 major collapses have occurred, and in the last ten years the resulting damage to property is estimated at about £1,000,000. Subsidence, associated with the collapse of caves resulting from gypsum dissolution in the Permian rocks of eastern England, occurs in a belt about 3 km wide and over 100 km long. Gypsum (CaSO4.2H2O) dissolves rapidly in flowing water and the cave systems responsible for the subsidence are constantly enlarging, causing a continuing subsidence problem. Difficult ground conditions are associated with caves, subsidence breccia pipes (collapsed areas of brecciated and foundered material), crown holes and post-subsidence fill deposits. -
Loch Maree Fault (NW-SE)
Walk Wester Ross 50+ walks Loch Torridon to Little Loch Broom 1 This guide describes most of the worthwhile low-level walks in the central part of Wester Ross, from Torridon to Dundonnell. Most visitors and settlers in Wester Ross are attracted by the outdoors – sea, moor, wood, loch, hill, river – and walking is the best way to experience it. (For the mountains, see the guide “Hills of Wester Ross”.) First, a gentle warning... This is a rough wild land with a lot of weather, and the walks reflect this: few are really easy. Most of the walks are on paths or tracks, but don’t expect all these to be as flat and well-surfaced as in the lowlands. Hazards may include bracken, heather, mud, bog or slippery rocks. A few pathless walks are included where careful micro-navigation is needed at certain points: these points are highlighted with a red line at the side. But don’t be put off! The weather is often good, and this is a great area for walking. Go slowly with your eyes open to see all that nature has to offer: wildflowers and plants of all kinds from trees to mosses and lichens, birds and other animals, insects, lochs (lakes) and burns (streams), ancient rocks, beautiful and spectacular scenery. And in many places there are ruins, traces of the human past from prehistoric round-houses to former crofting townships and evidence of old agriculture. The walks are arranged in 13 groups as on the map opposite. In addition to the 50 main walks, more difficult or longer extensions are often described.