Lithostratigraphy Adopted for Local Geological Sites
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A Building Stone Atlas of Warwickshire
Strategic Stone Study A Building Stone Atlas of Warwickshire First published by English Heritage May 2011 Rebranded by Historic England December 2017 Introduction The landscape in the county is clearly dictated by the Cob was suitable for small houses but when more space was underlying geology which has also had a major influence on needed it became necessary to build a wooden frame and use the choice of building stones available for use in the past. The wattle fencing daubed with mud as the infilling or ‘nogging’ to geological map shows that much of this generally low-lying make the walls. In nearly all surviving examples the wooden county is underlain by the red mudstones of the Triassic Mercia frame was built on a low plinth wall of whatever stone was Mudstone Group. This surface cover is however, broken in the available locally. In many cases this is the only indication we Nuneaton-Coventry-Warwick area by a narrow strip of ancient have of the early use of local stones. Adding the stone wall rocks forming the Nuneaton inlier (Precambrian to early served to protect the wooden structure from rising damp. The Devonian) and the wider exposure of the unconformably infilling material has often been replaced later with more overlying beds of the Warwickshire Coalfield (Upper durable brickwork or stone. Sometimes, as fashion or necessity Carboniferous to early Permian). In the south and east of the dictated, the original timber framed walls were encased in county a series of low-lying ridges are developed marking the stone or brick cladding, especially at the front of the building outcrops of the Lower and Middle Jurassic limestone/ where it was presumably a feature to be admired. -
Folk Song in Cumbria: a Distinctive Regional
FOLK SONG IN CUMBRIA: A DISTINCTIVE REGIONAL REPERTOIRE? A dissertation submitted in partial fulfilment of the degree of Doctor of Philosophy by Susan Margaret Allan, MA (Lancaster), BEd (London) University of Lancaster, November 2016 ABSTRACT One of the lacunae of traditional music scholarship in England has been the lack of systematic study of folk song and its performance in discrete geographical areas. This thesis endeavours to address this gap in knowledge for one region through a study of Cumbrian folk song and its performance over the past two hundred years. Although primarily a social history of popular culture, with some elements of ethnography and a little musicology, it is also a participant-observer study from the personal perspective of one who has performed and collected Cumbrian folk songs for some forty years. The principal task has been to research and present the folk songs known to have been published or performed in Cumbria since circa 1900, designated as the Cumbrian Folk Song Corpus: a body of 515 songs from 1010 different sources, including manuscripts, print, recordings and broadcasts. The thesis begins with the history of the best-known Cumbrian folk song, ‘D’Ye Ken John Peel’ from its date of composition around 1830 through to the late twentieth century. From this narrative the main themes of the thesis are drawn out: the problem of defining ‘folk song’, given its eclectic nature; the role of the various collectors, mediators and performers of folk songs over the years, including myself; the range of different contexts in which the songs have been performed, and by whom; the vexed questions of ‘authenticity’ and ‘invented tradition’, and the extent to which this repertoire is a distinctive regional one. -
Aust Cliff and Manor Farm
This excursion guide is a draft chapter, subject to revision, to be published in a field guide book whose reference is: Lavis, S. (Ed.) 2021. Geology of the Bristol District, Geologists’ Association Guide No. 75. It is not to be circulated or duplicated beyond the instructor and their class. Please send any corrections to Michael Benton at [email protected] Aust Cliff and Manor Farm Michael J. Benton Maps OS Landranger 172 1:50 000 Bristol & Bath Explorer 167 1:25 000 Thornbury, Dursley & Yate BGS Sheet 250 1:50 000 Chepstow Main references Swift & Martill (1999); Allard et al. (2015); Cross et al. (2018). Objectives The purpose of the excursion is to examine a classic section that documents the major environmental shift from terrestrial to marine rocks caused by the Rhaetian transgression, as well as the Triassic-Jurassic boundary, and to sample the rich fossil faunas, and espe- cially the Rhaetian bone beds. Risk analysis Low tides are essential for the excursion to Aust Cliff. Tides rise very rapidly along this section of coast (with a tidal range of about 12 m) and strong currents sweep past the bridge abutment. Visitors should begin the excursion on a falling tide. If caught on the east side of the bridge abutment when the tide rises, visitors should continue east along the coast to the end of the cliff where a path leads back to the motorway service area. In addition, the entire section is a high cliff, and rock falls are frequent, so hard hats must be worn. The Manor Farm section lies inland and is lower, so hard hats are less necessary. -
New Additions to CASCAT from Carlisle Archives
Cumbria Archive Service CATALOGUE: new additions August 2021 Carlisle Archive Centre The list below comprises additions to CASCAT from Carlisle Archives from 1 January - 31 July 2021. Ref_No Title Description Date BRA British Records Association Nicholas Whitfield of Alston Moor, yeoman to Ranald Whitfield the son and heir of John Conveyance of messuage and Whitfield of Standerholm, Alston BRA/1/2/1 tenement at Clargill, Alston 7 Feb 1579 Moor, gent. Consideration £21 for Moor a messuage and tenement at Clargill currently in the holding of Thomas Archer Thomas Archer of Alston Moor, yeoman to Nicholas Whitfield of Clargill, Alston Moor, consideration £36 13s 4d for a 20 June BRA/1/2/2 Conveyance of a lease messuage and tenement at 1580 Clargill, rent 10s, which Thomas Archer lately had of the grant of Cuthbert Baynbrigg by a deed dated 22 May 1556 Ranold Whitfield son and heir of John Whitfield of Ranaldholme, Cumberland to William Moore of Heshewell, Northumberland, yeoman. Recites obligation Conveyance of messuage and between John Whitfield and one 16 June BRA/1/2/3 tenement at Clargill, customary William Whitfield of the City of 1587 rent 10s Durham, draper unto the said William Moore dated 13 Feb 1579 for his messuage and tenement, yearly rent 10s at Clargill late in the occupation of Nicholas Whitfield Thomas Moore of Clargill, Alston Moor, yeoman to Thomas Stevenson and John Stevenson of Corby Gates, yeoman. Recites Feb 1578 Nicholas Whitfield of Alston Conveyance of messuage and BRA/1/2/4 Moor, yeoman bargained and sold 1 Jun 1616 tenement at Clargill to Raynold Whitfield son of John Whitfield of Randelholme, gent. -
Back Matter (PDF)
PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY 309 INDEX TO VOLUME 55 General index unusual crinoid-coral association 301^ Lake District Boreholes Craven inliers, Yorkshire 241-61 Caradoc volcanoes 73-105 Chronostratigraphy Cretoxyrhinidae 111, 117 stratigraphical revision, Windermere Lithostratigraphy crinoid stems, N Devon 161-73 Supergroup 263-85 Localities crinoid-coral association 301-4 Lake District Batholith 16,73,99 Minerals crinoids, Derbiocrinus diversus Wright 205-7 Lake District Boundary Fault 16,100 New Taxa Cristatisporitis matthewsii 140-42 Lancashire Crummock Fault 15 faunal bands in Lower Coal Measures 26, Curvirimula spp. 28-9 GENERAL 27 Dale Barn Syncline 250 unusual crinoid-coral association 3Q1-A Acanthotriletes sp. 140 Dent Fault 257,263,268,279 Legburthwaite graben 91-2 acritarchs 243,305-6 Derbiocrinus diversus Wright 205-7 Leiosphaeridia spp. 157 algae Derbyshire, limestones 62 limestones late Triassic, near York 305-6 Diplichnites 102 foraminifera, algae and corals 287-300 in limestones 43-65,287-300 Diplopodichnus 102 micropalaeontology 43-65 origins of non-haptotypic palynomorphs Dumfries Basin 1,4,15,17 unusual crinoid-coral association 301-4 145,149,155-7 Dumfries Fault 16,17 Lingula 22,24 Alston Block 43-65 Dunbar-Oldhamstock Basin 131,133,139, magmatism, Lake District 73-105 Amphoracrinus gilbertsoni (Phillips 1836) 145,149 Manchester Museum, supplement to 301^1 dykes, Lake District 99 catalogue of fossils in Geology Dept. Anacoracidae 111-12 East Irish Sea Basin 1,4-7,8,10,12,13,14,15, 173-82 apatite -
Stratigraphy, Basins, Ireland, Triassic, Jurassic, Penarth Group, Lias Group
[Type text] Raine et al. Uppermost Triassic and Lower Jurassic sediments, NI and ROI [Type text] 1 Uppermost Triassic to Lower Jurassic sediments of the island of Ireland and its surrounding basins. 2 3 RoBert Raine1, Philip Copestake2, Michael J. Simms3 and Ian Boomer4 4 5 1Geological Survey of Northern Ireland, Dundonald House, Upper Newtownards Road, Belfast, BT4 3SB, 6 Northern Ireland 7 2Merlin Energy Resources Ltd., Newberry House, New St, Herefordshire, HR8 2EJ, England, 8 3Ulster Museum, Belfast, BT9 5AB, Northern Ireland 9 4Geosciences Research Group, GEES, University of Birmingham, B15 2TT, England 10 11 Abstract 12 The uppermost Triassic to Lower Jurassic interval has not been extensively studied across the island 13 of Ireland. This paper seeks to redress that situation and presents a synthesis of records of the 14 uppermost Triassic and Lower Jurassic from both onshore and offshore basins as well as descriBing 15 the sedimentological characteristics of the main lithostratigraphical units encountered. Existing data 16 have been supplemented with a re-examination and logging of some outcrops and the integration of 17 data from recent hydrocarbon exploration wells and boreholes. The Late Triassic Penarth Group and 18 Early Jurassic Lias Group can Be recognised across the RepuBlic of Ireland and Northern Ireland. In 19 some onshore basins, almost 600 m of strata are recorded, however in offshore Basins thicknesses in 20 excess of two kilometres for the Lower Jurassic have now been recognised, although little detailed 21 information is currently availaBle. The transition from the Triassic to the Jurassic was a period of 22 marked gloBal sea-level rise and climatic change (warming) and this is reflected in the 23 lithostratigraphical record of these sediments in the basins of Northern Ireland and offshore Basins 24 of the Republic of Ireland. -
Complete 230 Fellranger Tick List A
THE LAKE DISTRICT FELLS – PAGE 1 A-F CICERONE Fell name Height Volume Date completed Fell name Height Volume Date completed Allen Crags 784m/2572ft Borrowdale Brock Crags 561m/1841ft Mardale and the Far East Angletarn Pikes 567m/1860ft Mardale and the Far East Broom Fell 511m/1676ft Keswick and the North Ard Crags 581m/1906ft Buttermere Buckbarrow (Corney Fell) 549m/1801ft Coniston Armboth Fell 479m/1572ft Borrowdale Buckbarrow (Wast Water) 430m/1411ft Wasdale Arnison Crag 434m/1424ft Patterdale Calf Crag 537m/1762ft Langdale Arthur’s Pike 533m/1749ft Mardale and the Far East Carl Side 746m/2448ft Keswick and the North Bakestall 673m/2208ft Keswick and the North Carrock Fell 662m/2172ft Keswick and the North Bannerdale Crags 683m/2241ft Keswick and the North Castle Crag 290m/951ft Borrowdale Barf 468m/1535ft Keswick and the North Catbells 451m/1480ft Borrowdale Barrow 456m/1496ft Buttermere Catstycam 890m/2920ft Patterdale Base Brown 646m/2119ft Borrowdale Caudale Moor 764m/2507ft Mardale and the Far East Beda Fell 509m/1670ft Mardale and the Far East Causey Pike 637m/2090ft Buttermere Bell Crags 558m/1831ft Borrowdale Caw 529m/1736ft Coniston Binsey 447m/1467ft Keswick and the North Caw Fell 697m/2287ft Wasdale Birkhouse Moor 718m/2356ft Patterdale Clough Head 726m/2386ft Patterdale Birks 622m/2241ft Patterdale Cold Pike 701m/2300ft Langdale Black Combe 600m/1969ft Coniston Coniston Old Man 803m/2635ft Coniston Black Fell 323m/1060ft Coniston Crag Fell 523m/1716ft Wasdale Blake Fell 573m/1880ft Buttermere Crag Hill 839m/2753ft Buttermere -
Landform Studies in Mosedale, Northeastern Lake District: Opportunities for Field Investigations
Field Studies, 10, (2002) 177 - 206 LANDFORM STUDIES IN MOSEDALE, NORTHEASTERN LAKE DISTRICT: OPPORTUNITIES FOR FIELD INVESTIGATIONS RICHARD CLARK Parcey House, Hartsop, Penrith, Cumbria CA11 0NZ AND PETER WILSON School of Environmental Studies, University of Ulster at Coleraine, Cromore Road, Coleraine, Co. Londonderry BT52 1SA, Northern Ireland (e-mail: [email protected]) ABSTRACT Mosedale is part of the valley of the River Caldew in the Skiddaw upland of the northeastern Lake District. It possesses a diverse, interesting and problematic assemblage of landforms and is convenient to Blencathra Field Centre. The landforms result from glacial, periglacial, fluvial and hillslopes processes and, although some of them have been described previously, others have not. Landforms of one time and environment occur adjacent to those of another. The area is a valuable locality for the field teaching and evaluation of upland geomorphology. In this paper, something of the variety of landforms, materials and processes is outlined for each district in turn. That is followed by suggestions for further enquiry about landform development in time and place. Some questions are posed. These should not be thought of as being the only relevant ones that might be asked about the area: they are intended to help set enquiry off. Mosedale offers a challenge to students at all levels and its landforms demonstrate a complexity that is rarely presented in the textbooks. INTRODUCTION Upland areas attract research and teaching in both earth and life sciences. In part, that is for the pleasure in being there and, substantially, for relative freedom of access to such features as landforms, outcrops and habitats, especially in comparison with intensively occupied lowland areas. -
Supplementary Information
Heritage Team 4th Floor 100 Parliament Street London SW1A 2BQ T: 020 7211 2018 [email protected] www.gov.uk/dcms 11 November 2016 Dear Ms Bourdin, Thank you for your letter of 17 October requesting further information regarding the nomination of the English Lake District for World Heritage inscription. You have asked for further details concerning proposals for development in the English Lake District and we feel that it would be helpful to preface our response with some explanation of the planning functions and powers of the Lake District National Park Authority, which is the planning authority for the whole of the candidate English Lake District World Heritage site. The English Lake District is an outstanding cultural landscape that has evolved over a long period of time and needs to continue evolving to sustain its future. We have a vibrant community of some 42,000 residents and an economy that is sustained by the key activities of upland hill farming and tourism. These activities inevitably need to develop in order to sustain the local economy and along with other requirements of the Lake District community, they generate planning applications which are determined by the Lake District National Park Authority. UK National Parks have the highest level of planning protection in the UK and the framework for our decision-making is outlined below. BACKGROUND TO THE PLANNING FUNCTION OF UK NATIONAL PARKS UK National Parks were established under the National Parks and Access to the Countryside Act 1949, and amended by the Environment Act 1995, to: conserve and enhance the natural beauty, wildlife and cultural heritage (of the National Parks); and promote opportunities for the understanding and enjoyment of the special qualities (of the National Parks) by the public. -
PANORAMA from Gowbarrow Fell (GR407218) 481M
PANORAMA from Gowbarrow Fell (GR407218) 481m PAN ORAMA 1 2 3 Little Mell Fell 4 5 7 8 9 12 6 The 10 11 Hause Ullswater Lowthwaite Great Hagg Meldrum Wood 1 Greystoke Forest 2 CARLISLE 3 Cold Fell 4 Melmerby Fell 5 PENRITH 6 Little Meldrum N 7 Cross Fell 8 Little Dun Fell 9 Great Dun Fell 10 POOLEY BRIDGE 11 Heughscar Hill 12 Mickle Fell E Loadpot Hill Arthur’s Pike Wether Hill 8 9 10 12 Bonscale 11 13 3 Pike Ullswater 4 6 14 5 7 Green Gowbarrow Hallin Fell 15 16 Hill 1 2 Bay Ullswater 1 Swinburn’s Park 2 Ullswater Outward Bound School 3 Swarthbeck Gill 4 Steel Knotts 5 SANDWICK 6 Martindale 7 Winter Crag 8 High Raise 9 Rampsgill Head 10 High Street 11 Thornthwaite Crag E 12 Gray Crag 13 Caudale Moor 14 Beda Head 15 The Nab 16 Rest Dodd S 17 9 10 11 12 13 14 15 16 18 1 3 4 5 6 8 2 7 Place 25 Fell 23 24 Swineside Common 20 21 Knott Fell 19 Dowthwaitehead Grisedale Glenridding Dodd 22 1 Red Screes (summit not in view) 2 Little Hart Crag 3 Dove Crag 4 Hart Crag 5 St Sunday Crag 6 Fairfield 7 Seat Sandal 8 Dollywaggon Pike 9 High Spying How 10 Helvellyn 11 Helvellyn Lower Man 12 White Side 13 Raise 14 Stybarrow Dodd 15 Hart Side 16 Birkett Fell 17 Great Dodd 18 Randerside 19 Arnison Crag 20 Hartsop Above How 21 Birks 22 Birkhouse Moor S 23 Heron Pike 24 Catstycam 25 Sheffield Pike W 8 9 10 11 12 1 6 7 2 3 4 Great Mell Souther Fell 13 Fell Wolf 5 Crags Matterdale Forest 1 Clough Head 2 Lord’s Seat 3 Barf 4 Dodd 5 Lonscale Fell 6 Skiddaw Little Man 7 Skiddaw 8 Blencathra 9 Sharp Edge 10 Bannerdale Crags 11 Bowscale Fell W 12 Carrock Fell 13 MUNGRISDALE N This graphic is an extract from The Near Eastern Fells, volume two in the Lakeland Fellranger series published in April 2008 by Cicerone Press (c) Mark Richards 2008. -
A Tectonic History of Northwest England
A tectonic history of northwest England FRANK MOSELEY CONTENTS Introduction 56x Caledonian earth movements 562 (A) Skiddaw Slate structures . 562 (B) Borrowdale Volcanic structures . 570 (C) Deformation of the Coniston Limestone and Silurian rocks 574 (D) Comment on Ingleton-Austwick inlier 580 Variscan earth movements. 580 (A) General . 580 (B) Folds 584 (C) Fractures. 587 4 Post Triassic (Alpine) earth movements 589 5 References 59 ° SUMMARY Northwest England has been affected by the generally northerly and could be posthumous Caledonian, Variscan and Alpine orogenies upon a pre,Cambrian basement. The end- no one of which is entirely unrelated to the Silurian structures include early N--S and later others. Each successive phase is partially NE to ~NE folding. dependent on earlier ones, whilst structures The Variscan structures are in part deter- in older rocks became modified by succeeding mined by locations of the older massifs and in events. There is thus an evolutionary structural part they are likely to be posthumous upon sequence, probably originating in a pre- older structures with important N-S and N~. Cambrian basement and extending to the elements. Caledonian wrench faults were present. reactivated, largely with dip slip movement. The Caledonian episodes are subdivided into The more gentle Alpine structures also pre-Borrowdale Volcanic, pre-Caradoc and follow the older trends with a N-s axis of warp end-Silurian phases. The recent suggestions of or tilt and substantial block faulting. The latter a severe pre-Borrowdale volcanic orogeny are was a reactivation of older fault lines and rejected but there is a recognizable angular resulted in uplift of the old north Pennine unconformity at the base of the volcanic rocks. -
Dent to Aye Gill Pike This Rewarding Walk Has Spectacular Views of the Howgill Fells (Below), the Three Peaks of Yorkshire, and Dentdale
Dent to Aye Gill Pike This rewarding walk has spectacular views of the Howgill Fells (below), the Three Peaks of Yorkshire, and Dentdale. Start: Dent car park (GPS: SD 703 871) Distance: 10.5km (6.5 miles) Highest point: 556m (Aye Gill Pike summit) Time: Allow 3 to 4 hours Grade: Difficult Notes: This route has sections with no obvious path, so a map and navigational skills are required. There are short sections on quiet roads where care should be taken, and the route can be boggy in places. There are toilets, a village shop, café and pubs in Dent. Other options: For a more challenging experience, follow this route in the opposite direction, beginning with the very steep climb up to Aye Gill Pike. 1. (GPS: SD 704 870) Turn left out of the car park and walk through the cobbled village centre. Leave the village on this road and pick up the riverside path for the Dales Way on your left, just before the river Dee. Follow this path until you reach the tarmac road. 2. (GPS: SD 700 873) Turn right along the road and pick up the Dales Way again on your right, continuing along the river to the road at Barth Bridge. 3. (GPS: SD 694 878) At the road turn right. Walk along here for a short distance (approx 150m) and turn up the small tarmac lane on your right. Continue along this quiet lane for approximately 1km, until reaching Lunds Farm. 4. (GPS: SD 694 887) At the entrance to Lunds Farm turn left and continue through the cobbled yard.