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Strathnaver Province Archaeology Project: Langdale, Grumbeg, Achadh an Eas & & the Tulloch Data Structure Report 2007
STRATHNAVER PROVINCE ARCHAEOLOGY PROJECT: LANGDALE, GRUMBEG, ACHADH AN EAS & & THE TULLOCH DATA STRUCTURE REPORT 2007 PROJECT 2406 carried out on behalf of Historic Scotland Contents 1.0 Executive Summary 7 2.0 Introduction 7 3.0 Site Location and Topography 7 4.0 Archaeological Background 7 5.0 Aims and Objectives 9 6.0 Methodology 10 7.0 Results 11 7.1 Langdale 12 7.2 Achadh an Eas 13 7.3 Grumbeg 16 7.4 The Tulloch 18 8.0 Discussion 19 9.0 Recommendations 19 10.0 Acknowledgements 19 11.0 Bibliography 20 12.0 Gazetteer of Sites 21 12.1 Langdale 21 12.2 Achadh an Eas 24 12.3 Grumbeg 26 12.4 DES 28 List of Figures Figure 1: Site Location 6 Figure 2: Extract from the first edition OS map (1878) of Langdale 11 Figure 3: Extract from the first edition OS map (1878) of Achadh an Eas 15 Figure 4: Extract from the first edition OS map (1878) of Grumbeg 16 Figure 5: Survey Plan of The Tulloch with Contour Model 17 List of Plates Plate 1: Cluster B at Langdale, from the north-west; The Tulloch lies beyond the trees 13 by the farmstead in background to left Plate 2: Longhouse in cluster G at Achadh an Eas, from the south-east 15 Plate 3: Longhouse GB 1 at Grumbeg Project website: http://www.northsutherlandarchaeology.org.uk © Glasgow University 2007 This report is one of a series published by GUARD, Gregory Building, Lilybank Gardens, Glasgow, G12 8QQ STRATHNAVER PROVINCE ARCHAEOLOGY PROJECT: LANGDALE, GRUMBEG, ACHADH AN EAS & THE TULLOCH DATA STRUCTURE REPORT 2007 PROJECT 2406 by Olivia Lelong and Amy Gazin-Schwartz This document has been prepared in accordance with GUARD standard operating procedures. -
Sedimentology of the Early Neoproterozoic Morar Group in Northern Scotland: Implications for Basin Models and Tectonic Setting H
Sedimentology of the early Neoproterozoic Morar Group in northern Scotland: implications for basin models and tectonic setting H. C. Bonsor1*, R. A. Strachan2, A. R. Prave3 and M. Krabbendam1 1 British Geological Survey, Murchison House, West Mains Road, Edinburgh, EH9 3LA, UK * corresponding author: (H. C. Bonsor) email: [email protected] 2 School of Earth and Environmental Sciences, University of Portsmouth, Portsmouth, PO1 3QL, UK 3 Department of Earth Sciences, University of Andrews, St Andrews, KY16 9AL, UK Abstract The metasedimentary rocks of the Morar Group in northern Scotland form part of the early Neoproterozoic Moine Supergroup. The upper part of the Group is c. 2-3 km thick and contains two large km-scale facies successions: a coarsening-upwards marine-to-fluvial regression overlain by a fining-upwards fluvial-to-marine transgression. Fluvial facies make up less than a third of the total thickness; shallow-marine lithofacies comprise the remainder. Combining these new findings with previously published data indicates that the Morar Group represents, overall, a transgressive stratigraphic succession c. 6-9km thick, in which there is both an upward and eastward predominance of shallow-marine deposits, and a concomitant loss of fluvial facies. Smaller-scale (100s of m thick) transgressive-regressive cycles are superimposed on this transgressive trend. Collectively, the characteristics of the succession are consistent with deposition in a foreland basin located adjacent to the Grenville orogen, and possibly linked to the peri-Rodinian ocean. Subsidence and progressive deepening of the Morar basin may have, at least in part, been driven by loading of Grenville-orogeny- emplaced thrust sheets, and aided by sediment loading. -
Structural Geometry, Tectonic History And
STRUCTURALGEOMETRY, TECTONIC HISTORY AND DEFORMATIONMECHANISMS IN THE MOINETHRUST ZONENEAR ULLAPOOL N. W. SCOTLAND D.A. WINTER B. Sc. M.Sc. DIC Thesis submitted for the degree of Doctor of Philosophy at the University of Edinburgh 1984 The laboratory work for Chapter 6 was carried out at St. Andrews University by Dr. G. Oliver, the remainder of the thesis is all my own work. Signed. A-W CONTENTS PAGE ABSTRACT. 1 ACKNOWLEDGMENTS. 2 CHAPTER13 INTRODUCTION. 3 STRATIGRAPHY. 4 1.1.1. THE LEWISIAN GNEISS COMPLEX. 4 1.1.2. THE "TORRIDONIAN" SEDIMENTS. 5 1.1.3. THE CAMBRO-ORDOVICIANSEDIMENTS. 6 1.1.4. THE MOINE METASEDIMENTS. 7 1.2. THRUSTTECTONICS AND CURRENTRESEARCH IN THE 9 MOINE THRUSTZONE CHAPTERTWO THE STRUCTURALGEOMETRY OF THE MOINE THRUSTZONE BETWEEN LOCH BROOMAND THE ASSYNTCULMINATION 2.1. INTRODUCTION 11 2.1.1 NOMENCLATURE 12 2.2. STRUCTURALGEOMETRY: THE MOINE THRUST 13 2.2.1 LATE MOVEMENTON THE MOINE THRUST: THE EVIDENCEOF AN 15 EXTENSIONALMOINE THRUST 2.3. THE LOCH BROOMTHRUST SHEET 18 2.3.1 STRUCTURALGEOMETRY OF LOCH BROOMTHRUST SHEET 18 2.3.2 DISPLACEMENTON THE LOCH BROOMTHRUST 19 2.4. THE ULLAPOOLTHRUST SHEET 21 2.4.1 DISPLACEMENTON THE ULLAPOOLTHRUST 22 2.5. SHEETIV 22 2.5.1 STRUCTURALGEOMETRY OF SHEETIV 23 2.5.1.1 BEDDINGPLANE GEOMETRY AND ITS STRUCTURAL IMPORTANCEIN SHEETIV 23 2.5.1.2 FOLDINGIN SHEETIV 24 2.5.1.3 FAULTSAND TECTONIC VEINS 26 2.5.1.3a THE NE-SWSET OF EXTENSIONFAULTS 26 2.5.1.3b THE NW-SESET OF EXTENSIONFAULTS 27 2.5.1.3c THE STRIKE-SLIP FAULTS 28 2.5.1.4 TECTONICVEINS 29 2.5.1.5 CLASSIFICATIONOF THE EXTENSIONFAULTS 31 2.6. -
0X0a I Don't Know Gregor Weichbrodt FROHMANN
0x0a I Don’t Know Gregor Weichbrodt FROHMANN I Don’t Know Gregor Weichbrodt 0x0a Contents I Don’t Know .................................................................4 About This Book .......................................................353 Imprint ........................................................................354 I Don’t Know I’m not well-versed in Literature. Sensibility – what is that? What in God’s name is An Afterword? I haven’t the faintest idea. And concerning Book design, I am fully ignorant. What is ‘A Slipcase’ supposed to mean again, and what the heck is Boriswood? The Canons of page construction – I don’t know what that is. I haven’t got a clue. How am I supposed to make sense of Traditional Chinese bookbinding, and what the hell is an Initial? Containers are a mystery to me. And what about A Post box, and what on earth is The Hollow Nickel Case? An Ammunition box – dunno. Couldn’t tell you. I’m not well-versed in Postal systems. And I don’t know what Bulk mail is or what is supposed to be special about A Catcher pouch. I don’t know what people mean by ‘Bags’. What’s the deal with The Arhuaca mochila, and what is the mystery about A Bin bag? Am I supposed to be familiar with A Carpet bag? How should I know? Cradleboard? Come again? Never heard of it. I have no idea. A Changing bag – never heard of it. I’ve never heard of Carriages. A Dogcart – what does that mean? A Ralli car? Doesn’t ring a bell. I have absolutely no idea. And what the hell is Tandem, and what is the deal with the Mail coach? 4 I don’t know the first thing about Postal system of the United Kingdom. -
Structural, Petrological, and Tectonic Constraints on the Loch Borralan and Loch Ailsh Alkaline Intrusions, Moine Thrust Zone, GEOSPHERE, V
Research Paper GEOSPHERE Structural, petrological, and tectonic constraints on the Loch Borralan and Loch Ailsh alkaline intrusions, Moine thrust zone, GEOSPHERE, v. 17, no. 4 northwestern Scotland https://doi.org/10.1130/GES02330.1 Robert Fox and Michael P. Searle 24 figures Department of Earth Sciences, Oxford University, South Parks Road, Oxford OX1 3AN, UK CORRESPONDENCE: [email protected] ABSTRACT during ductile shearing. The minerals pseudomor- Grit Members of the An t-Sron Formation) and the phing leucites show signs of ductile deformation Ordovician Durness Group dolomites and lime- CITATION: Fox, R., and Searle, M.P., 2021, Structural, petrological, and tectonic constraints on the Loch Bor- During the Caledonian orogeny, the Moine indicating that high-temperature (~500 °C) defor- stones (Woodcock and Strachan, 2000; Strachan ralan and Loch Ailsh alkaline intrusions, Moine thrust thrust zone in northwestern Scotland (UK) mation acted upon pseudomorphed leucite crystals et al., 2010; British Geological Survey, 2007). zone, northwestern Scotland: Geosphere, v. 17, no. 4, emplaced Neoproterozoic Moine Supergroup rocks, that had previously undergone subsolidus break- The hinterland of the Caledonian orogenic p. 1126– 1150, https:// doi.org /10.1130 /GES02330.1. meta morphosed during the Ordovician (Grampian) down. New detailed field mapping and structural wedge comprises schists of the Moine Super- and Silurian (Scandian) orogenic periods, westward and petrological observations are used to constrain group with structural inliers of Lewisian basement Science Editor: Andrea Hampel Associate Editor: Robert S. Hildebrand over the Laurentian passive margin in the north- the geological evolution of both the Loch Ailsh gneisses and intrusive Caledonian granites (Geikie, ern highlands of Scotland. -
Geodiversity Audit and Action Plan 2013 - 2016
GEODIVERSITY AUDIT AND ACTION PLAN 2013 - 2016 THIS PROJECT IS BEING PART FINANCED BY THE SCOTTISH GOVERNMENT AND THE EUROPEAN COMMUNITY HIGHLAND LEADER 2007-2013 PROGRAMME. CONTENTS FOREWORD.................................................................................................................. 1 ROCKS FROM THE DAWN OF TIME……………………………………………………….2 INTRODUCTION............................................................................................................ 3 The North West Highlands Geopark........................................................................... 3 The Geology and Geological Structure of the NWHG................................................. 3 The Purpose of the Audit and Action Plan .................................................................. 5 Geodiversity................................................................................................................ 5 Part 1 – THE GEODIVERSITY AUDIT........................................................................... 7 North West Highland Geopark : Location Maps ............................................................. 9 NWHG REF. 001 - BEN HUTIG................................................................................ 13 NWHG REF. 002 - CLEIT AN T-SEABHAIG ............................................................ 15 NWHG REF. 003 - ERIBOLL.................................................................................... 17 NWHG REF. 004 - AN T-SRON .............................................................................. -
The Lewisian of Lochinver, Sutherland; the Type Area for the Inverian Metamorphism
The Lewisian of Lochinver, Sutherland; the type area for the Inverian metamorphism CALVIN R. EVANS & RICHARD ST J. LAMBERT CONTENTS t Petrology and chemistry of the Lewisian of Lochinver ~8 (A) Gneisses . i28 (B) The transition from granulite to amphibolite facies ~29 (c) Pegmatites x3o (D) Mafic and ultramafic dykes x33 2 Structural relationships x33 (A) Badcallian structures . ~34 (S) Inverian structures ~35 (c) Correlation of Inverian folding and metamorphism x38 (D) Intrusion of NW dykes ~38 (~) Laxfordian deformation ~38 3 Geochronology and isotope geology x38 (A) Age of formation of the potash pegmatites ~38 (B) Geochronology of the northern sector of the Lewisian I4I 4 Implications of the Inverian metamorphism and correlations with other shield areas I43 5 References x46 SUMMARY The Lochinver district contains gneisses, and structural features of each sector of the pegmatites and dykes generated in five main complex are described and new whole rock episodes: (I) pre-26oom.y, garnet pyroxene Rb-Sr ages given for the pegmatite suite, granulite facies gneisses with low angle dips, suggesting a maximum age of 254 o m.y. for the formed in their final state by the Badcallian suite (plus intrusion of a further suite at 23io metamorphism; (2) potash-rich pegmatites of m.y. or recrystallisation of the first suite at age range 254o to 23io m.y.; (3) 23 to-22oo 23io m.y.). Other pegmatite ages confirm the m.y. amphibolite facies gneisses occurring in presence ofpre-2ooo m.y. activity NE of Scourie vertical WNW zones, produced by a broadly and at Gruinard. Field and petrographic isochemical metamorphic event; (4) vertical evidence at Lochinver demonstrates the ~w-trending dykes emplaced at 22oo m.y. -
Morar Group Correlation
Correlation of Torridon and Morar groups 1 2 A fluvial origin for the Neoproterozoic Morar Group, NW Scotland; implications 3 for Torridon - Morar group correlation and the Grenville Orogen Foreland Basin 4 5 Maarten Krabbendam (1), Tony Prave (2), David Cheer (2, 3), 6 (1) British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 7 3 LA, UK. Email: [email protected] Corresponding author. 8 (2) School of Geography & Geoscience, Irvine Building, University of St Andrews, 9 St Andrews KY16 9AL, UK 10 (3) Present address: Scotland TranServ, Broxden Business Park, Perth, PH1 1RA 11 12 Running title: Correlation of Torridon and Morar groups 13 14 Abstract 15 Precambrian sedimentary successions are difficult to date and correlate. In the 16 Scottish Highlands, potential correlations between the thick, undeformed siliciclastic 17 ‘Torridonian’ successions in the foreland of the Caledonian Orogen and the highly 18 deformed and metamorphosed siliciclastic Moine succession within the Caledonian 19 Orogen have long intrigued geologists. New and detailed mapping of the 20 Neoproterozoic A ‘Mhoine Formation (Morar Group, lowest Moine Supergroup) in 21 Sutherland has discovered low strain zones exhibiting well-preserved sedimentary 22 features. The formation comprises 3-5 kilometres of coarse, thick-bedded psammite 23 with abundant nested trough and planar cross-bedding bedforms, defining metre-scale 24 channels. Palaeocurrent directions are broadly unimodal to the NNE-ENE. We 25 interpret the A ‘Mhoine Formation as high-energy, braided fluvial deposits. The A 26 ‘Mhoine Formation and the unmetamorphosed, Neoproterozoic Applecross-Aultbea 27 formations (Torridon Group), are similar in terms of lithology, stratigraphical 28 thickness, sedimentology, geochemistry, detrital zircon ages and stratigraphical 29 position on Archaean basement. -
Geological Notes and Location Descriptions for Field Excursions
Inverness: 30 April - 7 May Inverness: 30 Geological notes and location descriptions for field excursions Deformation mechanisms, Rheology and Tectonics 2017 Deformation mechanisms, Rheology and Tectonics 1 Geological notes* The crustal evolution and geology of NW Scotland can be considered with reference to the Palaeozoic Caledonian orogeny. This major episode of crustal reworking was associated with the formation of a North Atlantic Craton – suturing the Proterozoic and older crustal blocks of Laurentian and Baltica (together with Avalonia, further south). NW Scotland contains part of the western margin of this orogen (or at least its more intense parts), a tectonic feature termed the Moine Thrust Belt. The foreland to the thrust belt preserves much older geology, exhumed from up to 35-40km depth, that give insight to processes that form, rework and reassemble the continental crust. The Caledonian rocks allow us to follow a transect from exhumed middle crustal sections within the orogen out into the foreland. Collectively these outcrops provide arrays of analogues for crustal geology and deformation structures, and we can use these to promote discussion of their geophysical characteristics when targeted in situ. However, the Caledonian crust, together with its foreland, has seen later deformation associated with the formation of sedimentary basins, chiefly in the immediate offshore. We can also access basin faults and examine not only their individual characteristics but also debate how they may have been influenced by pre-existing structures. Pre-Caledonian geology The Lewisian. The Lewisian forms the oldest basement to the British Isles and has classic Laurentian geology. The key geological markers in the field used to build up a sequence of geological events are a suite of NW-SE-trending metabasic sheets – the Scourie dykes. -
Hiking Scotland's Western Isles
Hiking Scotland’s Western Isles July 11 - 21, 2015 (11 days) , with Carleton Professor Clint Cowan 83 © AAWH © AAWH © AAWH Dear Carleton College Alumni and Friends, Gearrannan Dun Carloway I invite you to join Carleton College geologist Clint Cowan ’83 on this ISLE OF LEWIS wonderful hiking adventure amid the wealth of geological and archaeologi- ISLE OF HARRIS cal sites in Scotland’s western Highlands and Islands. The rocks tell the whole stornoway story, going back 2.7 million years, as you travel from the Isle of Mull in the Cotland Tarbert Callanish south, along the western edge of highland Scotland, to the Isle of Lewis in the s Outer Hebrides, sometimes along the mainland coast, but more often across incomparably beautiful, fascinating islands. Rodel Uig To fully enjoy and visit all the sites on this itinerary, you must be reasonably ISLE OF SKYE fit and enjoy hiking. The daily hikes will be easy to moderate in difficulty, and their duration (and elevation gained) for each day is estimated within the itin- Talisker Distillery Western erary. You will not rush, but you will hike up to six miles per day, sometimes Loch Coruisk uphill and/or over uneven ground. Elgol Mallaig Two minibuses, each with an expert local driver/guide, will accompany the Glenfinnan group. Your guides will explain in advance the difficulty of each day’s walk(s) and, if you prefer, you can opt out of any walking excursion and be driven to Kilchoan Fingal’s Cave the next stop (but, bear in mind that some sites can only be visited if you walk to them). -
Thermobarometry of the Moine and Sgurr Beag Thrust Sheets, Northern Scotland
Smith ScholarWorks Geosciences: Faculty Publications Geosciences 8-1-2018 Thermobarometry of the Moine and Sgurr Beag Thrust Sheets, Northern Scotland Sarah E. Mazza Virginia Polytechnic Institute and State University, [email protected] Calvin Mako Virginia Polytechnic Institute and State University Richard D. Law Virginia Polytechnic Institute and State University Mark J. Caddick Virginia Polytechnic Institute and State University Maarten Krabbendam British Geological Survey See next page for additional authors Follow this and additional works at: https://scholarworks.smith.edu/geo_facpubs Part of the Geology Commons Recommended Citation Mazza, Sarah E.; Mako, Calvin; Law, Richard D.; Caddick, Mark J.; Krabbendam, Maarten; and Cottle, John, "Thermobarometry of the Moine and Sgurr Beag Thrust Sheets, Northern Scotland" (2018). Geosciences: Faculty Publications, Smith College, Northampton, MA. https://scholarworks.smith.edu/geo_facpubs/112 This Article has been accepted for inclusion in Geosciences: Faculty Publications by an authorized administrator of Smith ScholarWorks. For more information, please contact [email protected] Authors Sarah E. Mazza, Calvin Mako, Richard D. Law, Mark J. Caddick, Maarten Krabbendam, and John Cottle This article is available at Smith ScholarWorks: https://scholarworks.smith.edu/geo_facpubs/112 Thermobarometry of the Moine and Sgurr Beag thrust sheets, northern Scotland Sarah E. Mazza1*, Calvin Mako1, Richard D. Law1, Mark J. Caddick1, Maarten Krabbendam2, John Cottle3 1Department of Geosciences, Virginia -
A New Stratigraphic Framework for the Early Neoproterozoic Successions of Scotland
Accepted Manuscript Journal of the Geological Society A new stratigraphic framework for the early Neoproterozoic successions of Scotland Maarten Krabbendam, Rob Strachan & Tony Prave DOI: https://doi.org/10.1144/jgs2021-054 To access the most recent version of this article, please click the DOI URL in the line above. When citing this article please include the above DOI. Received 14 May 2021 Revised 19 August 2021 Accepted 23 August 2021 © 2021 UKRI. The British Geological Survey. Published by The Geological Society of London http://creativecommons.org/licenses/by/4.0/ This is an Open Access article distributed under the terms of the Creative Commons Attribution 4.0 License (http://creativecommons.org/licenses/by/4.0/) Manuscript version: Accepted Manuscript This is a PDF of an unedited manuscript that has been accepted for publication. The manuscript will undergo copyediting, typesetting and correction before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. Although reasonable efforts have been made to obtain all necessary permissions from third parties to include their copyrighted content within this article, their full citation and copyright line may not be present in this Accepted Manuscript version. Before using any content from this article, please refer to the Version of Record once published for full citation and copyright details, as permissions may be required. Downloaded from http://pubs.geoscienceworld.org/jgs/article-pdf/doi/10.1144/jgs2021-054/5396122/jgs2021-054.pdf by guest on 24 September 2021 A new stratigraphic framework for the early Neoproterozoic successions of Scotland Maarten Krabbendam1*, Rob Strachan2, Tony Prave3 1British Geological Survey, Lyell Centre, Research Avenue, Edinburgh EH14 4AP, Scotland, UK 2School of the Environment, Geography and Geosciences, University of Portsmouth, Portsmouth, PO1 3QL, UK.