ENGINEERING GEOLOGY Id Question on the Surface of Earth
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Graveyard Geology
GRAVEYARD GEOLOGY A Guide to Rocks in Graveyards and Cemeteries Wendy Kirk Department of Earth Sciences, David Cook University College London & Aldersbrook Geological Society London Geodiversity Partnership Introduction Walk around graveyards and cemeteries (in this case, those of London and the southeast of England) and it becomes apparent that, prior to the latter part of the twentieth century, many memorials were made out of just a few different rock types. These were chosen for reasons of appearance, cost, workability and ease of transport to the cemetery, as well as for resistance to weathering and dependence on local regulations. In the last few decades, a range of different, interesting and beautiful stones have appeared, many brought in from abroad, enhancing the diversity of materials used. The intention of this guide is to help a non-specialist identify the main rock types, to recognize some of the varieties and to know where some of these might have come from. Graveyards are a wonderful resource for those with an interest in geology at any level, wildlife, plants, history or sculpture. We hope you gain as much pleasure as we have done. First things first A useful place to start is to be able to distinguish between igneous, sedimentary and metamorphic rocks. Igneous rocks form from melted rock called magma. If this erupts at the surface, it is called lava. It cools and crystallizes quickly, so the grains are too small to see even with a hand lens (magnifying glass). If the lava erupt explosively to form a spray, the cooled fragments are known as volcanic ash. -
Upper Ordovician and Silurian Stratigraphy in Sequatchie Valley and Parts of the Adjacent Valley and Ridge, Tennessee
Upper Ordovician and Silurian Stratigraphy in Sequatchie Valley and Parts of the Adjacent Valley and Ridge, Tennessee GEOLOGICAL SURVEY PROFESSIONAL PAPER 996 Prepared in cooperation with the Tennessee Division of Geology Upper Ordovician and Silurian Stratigraphy in Sequatchie Valley and Parts of the Adjacent Valley and Ridge, Tennessee By ROBERT C. MILICI and HELMUTH WEDOW, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 996 Prepared in cooperation with the Tennessee Division of Geology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1977 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Milici, Robert C 1931- Upper Ordovician and Silurian stratigraphy in Sequatchie Valley and parts of the adjacent valley and ridge, Tennessee. (Geological Survey professional paper; 996) Bibliography: p. Supt. of Docs. no.: I 19.16:996 1. Geology, Stratigraphic--Ordovician. 2. Geology, Stratigraphic--Silurian. 3. Geology--Tennessee--Sequatchie Valley. 4. Geology--Tennessee--Chattanooga region. I. Wedow, Helmuth, 1917- joint author. II: Title. Upper Ordovician and Silurian stratigraphy in Sequatchie Valley .... III. Series: United States. Geological Survey. Professional paper; 996. QE660.M54 551.7'310976877 76-608170 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03002·1 CONTENTS Page Abstract 1 Introduction ----------------------------------------------------------------------------- -
STRATEGIC STONE STUDY a Building Stone Atlas of NORTH-EAST YORKSHIRE
STRATEGIC STONE STUDY A Building Stone Atlas of NORTH-EAST YORKSHIRE Published May 2012 Derived from BGS digital geological mapping at 1:625,000 scale, British Geological Survey © NE Yorkshire Bedrock Geology NERC. All rights reserved Click on this link to visit NE Yorkshire’s geology and their contribution to known building stones, stone structures and building stone quarries (Opens in new window http://maps.bgs.ac.uk/buildingstone?County=North-EastYorkshire ) NE Yorkshire Strategic Stone Study 1 Stratigraphical column of the Permian (in part),Triassic, Jurassic and Cretaceous rocks and Quaternary deposits in North-east Yorkshire showing the common buildings stones (bold) and alternative stone names. The oldest rocks are at the bottom of the table. Gp., Group; Fm., Formation; Mbr., Member. North East Yorkshire: Permian, Triassic, Jurassic, Cretaceous & Quaternary Building Stones PERIOD GROUP FORMATION MEMBER Common/alternative Stone Name Calcareous Tufa; Aquarium Stone Till (Boulder Clay) and Fluvio-glacial sand Quaternary and gravel; boulders Tertiary Cleveland Dyke Whinstone Flamborough Chalk Fm. Flamborough Chalk; White Chalk Burnham Chalk Fm. Burnham Chalk; White chalk Chalk Group Welton ChalkFm. Cretaceous Ferriby Chalk Fm. Grey chalk ungrouped Hunstanton Fm. Speeton Clay Kimmeridge Clay ungrouped Ampthill Clay North Grimston Upper Calcareous Grit Upper Calcareous Grit Cementstone North Grimston Cementstone Formation Coral Rag Member Coral Rag Malton Oolite Member Malton Oolite; Hildenley Limestone; Corallian Hildenley Stone Group Middle Calcareous Grit Middle Calcareous Grit Coralline Oolite Formation Member Birdsall Calcareous Grit Birdsall Calcareous Grit Member Hambleton Oolite Hambleton Oolite Member Yedmandale Member Passage Beds; Wallstone Lower Calcareous Grit Fm. Lower Calcareous Grit Oxford Clay Fm. -
Dicionarioct.Pdf
McGraw-Hill Dictionary of Earth Science Second Edition McGraw-Hill New York Chicago San Francisco Lisbon London Madrid Mexico City Milan New Delhi San Juan Seoul Singapore Sydney Toronto Copyright © 2003 by The McGraw-Hill Companies, Inc. All rights reserved. Manufactured in the United States of America. Except as permitted under the United States Copyright Act of 1976, no part of this publication may be repro- duced or distributed in any form or by any means, or stored in a database or retrieval system, without the prior written permission of the publisher. 0-07-141798-2 The material in this eBook also appears in the print version of this title: 0-07-141045-7 All trademarks are trademarks of their respective owners. Rather than put a trademark symbol after every occurrence of a trademarked name, we use names in an editorial fashion only, and to the benefit of the trademark owner, with no intention of infringement of the trademark. Where such designations appear in this book, they have been printed with initial caps. McGraw-Hill eBooks are available at special quantity discounts to use as premiums and sales promotions, or for use in corporate training programs. For more information, please contact George Hoare, Special Sales, at [email protected] or (212) 904-4069. TERMS OF USE This is a copyrighted work and The McGraw-Hill Companies, Inc. (“McGraw- Hill”) and its licensors reserve all rights in and to the work. Use of this work is subject to these terms. Except as permitted under the Copyright Act of 1976 and the right to store and retrieve one copy of the work, you may not decom- pile, disassemble, reverse engineer, reproduce, modify, create derivative works based upon, transmit, distribute, disseminate, sell, publish or sublicense the work or any part of it without McGraw-Hill’s prior consent. -
Geology of the Pegmatites and Associated Rocks of Maine
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR BULLETIN 445 GEOLOGY OF THE PEGMATITES AND ASSOCIATED ROCKS OF MAINE INCLUDING FELDSPAR, QUARTZ, MICA, AND GEM DEPOSITS BY EDSON S. BASTIN WASHINGTON GOVERNMENT PRINTING OFFICE 1911 CONTENTS. Introduction.............................................................. 9 Definition of pegmatite...................................................... 10 Geographic distribution.................................................... 10 Geology.................................................................. 10 Bordering rocks....................................................... 10 Pegmatites in foliated rocks........................................ 11 General statement............................................ 11 Sedimentary foliates........................................... 11 Igneous foliates.....".......................................... 12 Pegmatites in massive granites.................................... 13 'Age.................................................................. 15 General character..................................................... 15 Mineral and chemical composition................................. 15 Mineral constituents.......................................... 15 Relative proportions of minerals............................... 18 Quartzose phases. ..............................^............. 18 Fluidal cavities............................................... 19 Sodium and lithium phases................................... 20 Muscovite -
Mineralogy of the Peraluminous Spruce Pine Plutonic Suite
MINERALOGY OF THE PERALUMINOUS SPRUCE PINE PLUTONIC SUITE, MITCHELL, AVERY, AND YANCEY COUNTIES, NORTH CAROLINA by William Brian Veal (Under the Direction of Samuel E. Swanson) ABSTRACT The Spruce Pine plutonic suite consists of numerous Devonian (390-410 ma) peraluminous granitic plutons, dikes, sills, and associated pegmatites. The mineralogy of pegmatites and host granodiorites from seven locations was studied to determine the extent of fractionation of the pegmatites relative to the granodiorite. Garnets in the plutons are almandine- spessartine and some display epitaxial overgrowths of grossular garnet. Similar garnets are found in the pegmatites. Pegmatitic muscovite contains several percent iron and is compositionally similar to muscovite from the host granodiorite. Feldspars in the granodiorites and pegmatites are compositionally similar (plagioclase Ab69-98; k-feldspar Or95-98). The lack of compositional variation between minerals in pegmatites and host granodiorites indicates the pegmatites were not the result of extreme fractionation and indicates that pegmatite mineralogy can be used to characterize the mineralogy of an entire granodiorite body. INDEX WORDS: Spruce Pine, Pegmatites, Granodiorite, Garnet, Muscovite, Feldspar MINERALOGY OF THE PERALUMINOUS SPRUCE PINE PLUTONIC SUITE, MITCHELL, AVERY, AND YANCEY COUNTIES, NORTH CAROLINA by WILLIAM BRIAN VEAL B.S., Georgia Southwestern State University, 2002 A Thesis Submitted to the Graduate Faculty of The University of Georgia in Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE ATHENS, GEORGIA 2004 © 2004 William Brian Veal All Rights Reserved MINERALOGY OF THE PERALUMINOUS SPRUCE PINE PLUTONIC SUITE, MITCHELL, AVERY, AND YANCEY COUNTIES, NORTH CAROLINA by WILLIAM BRIAN VEAL Major Professor: Samual E. Swanson Committee: Michael F. -
Geological Alterations and Chemical Treatment of a Polluted Limestone Foundation
Missouri University of Science and Technology Scholars' Mine International Conference on Case Histories in (2008) - Sixth International Conference on Case Geotechnical Engineering Histories in Geotechnical Engineering 14 Aug 2008, 2:15pm - 4:00pm Geological Alterations and Chemical Treatment of a Polluted Limestone Foundation B. M. Al-Khailany Ministry of Higher Education and Scientific Research, Baghdad, Iraq R. R. Al-Omari Al-Nahrain University, Baghdad, Iraq W. F. Sagman Follow this and additional works at: https://scholarsmine.mst.edu/icchge Part of the Geotechnical Engineering Commons Recommended Citation Al-Khailany, B. M.; Al-Omari, R. R.; and Sagman, W. F., "Geological Alterations and Chemical Treatment of a Polluted Limestone Foundation" (2008). International Conference on Case Histories in Geotechnical Engineering. 23. https://scholarsmine.mst.edu/icchge/6icchge/session07/23 This Article - Conference proceedings is brought to you for free and open access by Scholars' Mine. It has been accepted for inclusion in International Conference on Case Histories in Geotechnical Engineering by an authorized administrator of Scholars' Mine. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. GEOLOGICAL ALTERATIONS AND CHEMICAL TREATMENT OF A POLLUTED LIMESTONE FOUNDATION Al-Khailany, B. M. Al-Omari, R. R. Sagman, W. F. Ministry of Higher Education and Al-Nahrain University Formerly Postgraduate Student Scientific Research Baghdad, Iraq Baghdad, Iraq ABSTRACT A large factory for the production of concentrated sulphuric acid is constructed in 1977 and located in the west of Iraq near Al-Kaim city. The footings carrying the installations rest on calcareous rocks which extend deep into the ground. -
Textures and Structures of Igneous Rocks
UNIT 2 TEXTURES AND STRUCTURES OF IGNEOUS ROCKS Structure______________________________________________ 2.1 Introduction 2.4 Forms of Igneous Rocks Expected Learning Outcomes Sill 2.2 Textures of Igneous Rocks Dyke Crystallinity Laccolith Granularity Bysmalith Shape of the Crystals Lopolith Mutual Relationship between Crystal and Phacolith Non-Crystalline Material Chonolith Intergrowth Textures Volcanic Neck Exsolution Textures Batholith Miscellaneous Textures Stock 2.3 Structures of Igneous Rocks Boss Vesicular and Amygdaloidal Structures 2.5 Summary Scoriaceous and Pumiceous Structures 2.6 Activity Lava Tunnels 2.7 Terminal Questions Blocky and Ropy Lava 2.8 References Platy and Sheet Structure 2.9 Further/Suggested Readings Pillow Lava 2.10 Answers Columnar/Prismatic Structure Lava Flow Structure Rift and Grain Perlitic Structure Rapakivi Structure Xenoliths ……………………………………………………………………………………………….…....Block 1 Igneous Petrology.......…-I 2.1 INTRODUCTION You have been introduced to the igneous rocks in the previous unit. You have also learnt that the slow cooling of magma takes place in the deeper parts of the Earth and large size crystals are formed. On the contrary, magma undergoing rapid cooling in shallower depth or on the surface of the Earth yielded fine grained crystals. The rapid cooling of lava/melt molten rock on the surface of the Earth produces fine grained minerals or glass. The igneous rocks vary in grain size from very coarse, medium to fine grained or even glassy in hand specimen and under the microscope. Thus, igneous rocks display variety of textures. Thus, the term texture refers to physical appearance of a rock. In this unit we will discuss textures and structures of igneous rocks. -
California State University, Northridge Depositional Environments of the Vaqueros Formation Along Upper Sespe Creek, Ventura
CALIFORNIA STATE UNIVERSITY, NORTHRIDGE DEPOSITIONAL ENVIRONMENTS OF THE VAQUEROS FORMATION ~ ALONG UPPER SESPE CREEK, VENTURA COUNTY, CALIFORNIA A thesis submitted in partial sa~isfaction of the requirements for the degree of Master of Science in Geology by Stephen Anthony Reid / January, 1979 approved: California State University, Northridge ii ~· ~· ~· Frontispiece. Air view of Piedra Blanca, looking northwest. Piedra Blanca consists of outcrops of the Vaqueros upper member exposed in the core of Tule Creek syncline. iv CONTENTS Page ABSTRACT X INTRODUCTION 1 PURPOSE 1 LOCATION AND GEOGRAPHY 1 GEOLOGIC SETTING AND PREVIOUS WORK 3 PROCEDURES 5 ACKNOWLEDGEMENTS 6 STRATIGRAPHY AND DEPOSITIONAL ENVIRONMENTS 8 INTRODUCTION 8 PRE-VAQUEROS ROCKS 9 SESPE FORMATION 9 STRATIGRAPHY AND LITHOLOGY 9 ENVIRONMENT OF DEPOSITION 10 VAQUEROS FORMATION 10 NOMENCLATURE 10 AGE 13 GENERAL STRATIGRAPHIC STATEMENT 14 DESCRIPTION OF LOWER MEMBER 16 GENERAL 16 LOWER SANDSTONE 19 Lithology 19 Fossils 26 LOWER LIMESTONE 28 v Page Lithology 28 Fossils 33 LOWER MUDSTONE 35 Lithology 35 Fossils 37 DEPOSITIONAL ENVIRONMENTS OF THE LOWER MEMBER 39 INTRODUCTION 39 FOSSILS 41 MUDDY BEACH 43 BAY MARGIN 44 OPEN BAY CENTER 45 SHALLOW GRASSY BAY 47 INLET INFLUENCED BAY 49 PALEOCURRENT ANALYSIS 50 SUMMARY 52 DESCRIPTION OF MIDDLE MEMBER 54 GENERAL 54 MIDDLE MUDSTONE AND SILTSTONE 56 Lithology 56 Fossils 61 ENVIRONMENT OF DEPOSITION 62 DESCRIPTION OF UPPER MEMBER 63 GENERAL 63 UPPER PLANE-BEDDED SANDSTONE 67 Lithology 67 vi Page Fossils 70 MASSIVE AND BIOTURBATED SANDSTONE -
Subsurface Geology of the Cochran Pegmatite, Cherokee-P…
SUBSURFACE GEOLOGY OF THE COCHRAN PEGMATITE, CHEROKEE-PICKENS DISTRICT, GEORGIA Alexander J. Gunow Gregory N. Bonn Bruce J. O'Connor Georgia Department of Natural Resources Environmental Protection Division Georgia Geologic Survey GEOLOGIC REPORT 5 Subsurface Geology of the Cochran Pegmatite, Cherokee-Pickens District, Georgia Alexander J. Gunow Gregory N. Bonn Bruce J. O'Connor Georgia Department of Natural Resources Joe D. Tanner, Commissioner Environmental Protection Division Harold F. Reheis, Director Georgia Geologic Survey William H. McLemore, State Geologist Atlanta 1992 Geologic Report 5 TABLE OF CONTENTS Page Abstract ..................................................................................................... 1 Introduction ............................................................................................. 2 General r>escription ................................................................................ 3 Results ....................................................................................................... 6 Discussion................................................................................................. 9 References ................................................................................................. 10 Appendices ........................................................................................... .... 11 A. Drill Hole Information and Mineralogy ......................... 11 B. Lithologic r>escription of Drill Core ............................... 17 LIST OF ILLUSTRATIONS -
Bedrock Geology and Geochemical Analysis of the Bowdoinham 7.5' Quadrangle, Southwestern Maine
Bedrock Geology and Geochemical Analysis of the Bowdoinham 7.5’ Quadrangle, southwestern Maine Joel Frank Cubley Submitted in Partial Fulfillment of the Requirements for the Degree of Bachelor of Arts Department of Geology Middlebury College Middlebury, Vermont April 2005 Bedrock Geology and Geochemical Analysis of the Bowdoinham 7.5’ Quadrangle, southwestern Maine Joel Cubley, Department of Geology Middlebury College, Middlebury, Vermont 05753 The Bowdoinham 7.5’ quadrangle, located in southwestern Maine, is situated along the boundary between the regionally extensive Liberty-Orrington and central Maine lithotectonic belts. Detailed 1:24,000 scale bedrock mapping in the northern half of the quadrangle has resulted in the delineation of the following lithologic units (described from west to east): (1) interlayered biotite granofels and calc-silicate gneisses of the Silurian-Devonian Vassalboro Formation (central Maine sequence), (2) a previously unrecognized, deformed and recrystallized Devonian metagranitoid pluton hereby named the Hornbeam Hill Intrusive Suite, (3) migmatitic biotite gneisses and other subordinate lithologies (e.g. amphibolites, rusty schists) associated with the Ordovician Falmouth-Brunswick sequence (Liberty-Orrington belt), and (4) several small but mappable granitic pegmatite bodies of both Devonian and Permian age. The Hornbeam Hill Intrusive Suite is significant because it stitches the contact between the Vassalboro Formation and Falmouth-Brunswick sequence rocks. Thin dikes and sills of Mesozoic diabase are found in the study area, but cannot be mapped at this scale. Stratified rocks in the quadrangle have been penetratively deformed, folded, and metamorphosed to upper amphibolite conditions during the Acadian orogeny. A pervasive east-dipping foliation (generally <45º) can be found in rocks of both lithotectonic belts, as well as the Hornbeam Hill Intrusive Suite, implying that the dominant episode of deformation in this region occurred after the emplacement of that pluton. -
A Building Stone Atlas of Oxfordshire
Strategic Stone Study A Building Stone Atlas of Oxfordshire First published by English Heritage March 2011 Rebranded by Historic England December 2017 Introduction The oldest rocks in Oxfordshire crop out in the north of the county and are of Lower Jurassic age, around 200 million years old. Younger Jurassic and Cretaceous formations progressively crop out towards the south. The harder limestone and chalk lithologies form escarpments, whilst clay underlies the intervening vales. The character of Oxfordshire’s stone buildings is very much determined by the nature of the local stone, which leads to a fascinating variation of styles across the county. With the exception of the Jurassic ooidal freestone quarried around Taynton, few building stones were of sufficient quality to be used much beyond their immediate source area. Now only a handful of building stone quarries are still active in the county, supplying Marlstone and the Chipping Norton Limestone. Unfortunately the other building stones described in the following pages are no longer available from working local quarries. The following summary of the principal local building stones is based largely on Arkell’s work, Oxford Stone and The Geology of Oxford, and Powell’s recent Geology of Oxfordshire. The oldest stones are described first, progressing towards the stratigraphically youngest to the south. XXX Strategic Stone Study 1 Oxfordshire Bedrock Geology Map Derived from BGS digital geological mapping at 1:625,000 scale, British Geological Survey ©NERC. All rights reserved Oxfordshire Strategic Stone Study 2 Lower Jurassic The distinctive warm-coloured Marlstone characterises the cottages in many villages such as Great Tew, Deddington, Lias Group Adderbury, Bloxham, Wroxton, Hook Norton and Hornton, as well as churches such as St.