Bed Rock Geology of the East Barre Area, Vermont

Total Page:16

File Type:pdf, Size:1020Kb

Bed Rock Geology of the East Barre Area, Vermont BED ROCK GEOLOGY OF THE EAST BARRE AREA, VERMONT By VARANASI RAMA MURTHY VERMONT GEOLOGICAL SURVEY CHARLES G. DOLL, State Geologist Published by VERMONT DEVELOPMENT COMMISSION MONTPELIER, VERMONT BULLETIN NO. 10 1957 dm I '- S ' - S '5 i . Rock of Ages Ouariv seen from its southwestern end. Prominent joint surfaces and a dark dike cutting the Barre granite are seen in the left side of the photograph. Grout piles in the background. CONTENTS PAGE ABSTRACT 11 INTRODUCTION ....................... 12 Location and Area .................... 12 Regional Geologic Setting . . . . . . . . . . . . . . . 12 Previous Work ..................... 14 Present Study ..................... 15 Method of Work . . . . . . . . . . . . . . . . . . . 16 Acknowledgments ................... 16 Topography and Drainage ................ 17 Climate and Water Supply ................ 18 Industries and Access to the Area ............. 19 STRATIGRAPRY . . . . . . . . . . . . . . . . . . . . . . 19 General Statement ................... 19 Stratigraphic Units . . . . . . . . . . . . . . . . . . 20 Stratigraphic Relations .................. 21 Definitions of Formations ................ 22 Westmore Formation . . . . . . . . . . . . . . . . 22 Barton River Formation ................ 22 Waits River Formation ................ 24 Barton River Formation ................. 24 Distribution . . . . . . . . . . . . . . . . . . . . 24 Lithology ...................... 24 Thickness . . . . . . . . . . . . . . . . . . . . . 25 Correlation ...................... 25 Age ......................... 26 Westmore Formation . . . . . . . . . . . . . . . . . 27 Distribution . . . . . . . . . . . . . . . . . . . . 27 Lithology ...................... 28 Thickness........................ 31 Correlation ...................... 31 Age......................... 32 Waits River Formation ................. 35 General Statement .................. 35 History of the Name .................. 35 Lithology ...................... 36 Thickness . . . . . . . . . . . . . . . . . . . . . 37 PAGE Correlation ...................... 38 Age ......................... 38 Standing Pond Member of the Waits River Formation . . 39 General Statement .................. 39 Lithology ...................... 40 Thickness . . . . . . . . . . . . . . . . . . . . . . 41 Gile Mountain Formation . . . . . . . . . . . . . . . . 41 History of the Name .................. 41 Distribution . . . . . . . . . . . . . . . . . . . . . 42 Lithology ...................... 42 Thickness . . . . . . . . . . . . . . . . . . . . . . 44 Correlation ...................... 44 Age ......................... 44 Relationship between the Westmore and the Gile Mountain formation ...................... 44 STRUCTURE ........................ 46 General Statement ................... 46 Terminology ...................... 47 Bedding ....................... 47 Schistosity ...................... 47 Cleavage ....................... 47 Syncline and Anticline ................. 47 Trend of Bedding ................... 47 Dextral and Sinistral Patterns of Folds .......... 48 Structural Features ................... 48 Early Structures ....................SO Early Schistosity .................. 50 Early Folds ......................SI Later Structures ....................S6 General Statement ..................S6 Field Data ..................... 57 Origin of the Structures . . . . . . . . . . . . . . . . . 59 Structure of the Westmore Formation ........... 66 Structural Synthesis ................... 68 PLUTONIC ROCKS ..................... 69 General Statement ................... 69 Early Work ...................... 70 The Bane granite .................... 70 PAGE Petrography . . . . . . . . . . . . . . . . . . . . 71 Modal Analysis of the Bane Granite ........... 73 Relationship between Muscovite and Biotite ....... 76 Relationship between Muscovite and Plagioclase . . . . 76 The Knox Mountain Granite ............... 79 Petrography ..................... 79 Qualitative Spectrographic Analysis of the Granites ..... 81 Relation of the Granites with the host rocks . . . . . . . 82 Internal Structural Features of the Granites . . . . . . . 86 Flow Structures .................... 86 Joints ........................ 86 Longitudinal Joints ................. 87 Cross Joints..................... 87 Flat-lying Joints .................. 88 Origin of the Bane Granite ................ 88 Petrologic Evidence .................. 89 Structural Evidence .................. 92 Mode of Emplacement .................. 93 Age of the Bane Granite ................. 95 Dike Rocks ....................... 95 Granitic Dikes . . . . . . . . . . . . . . . . . . . 95 Structural Trends .................. 96 Mineralogy of the Pegmatites ............. 97 Basic Dikes ...................... 97 Mineralogy ..................... 97 METAMORPHISM ...................... 98 General Statement ................... 98 Argillaceous Rocks .................. 99 Green-Schist Facies ................. 99 Albite-Epidote-Amphibolite Facies .......... 100 Amphibolite Facies . . . . . . . . . . . . . . . . 101 Calcareous and Impure Calcareous Rocks ........ 101 Green-Schist Facies ................. 101 Albite-Epidote-Amphibolite Facies .......... 102 Amphibolite Facies . . . . . . . . . . . . . . . . 102 Metavolcanics .................... 103 Contact Metamorphism ................ 104 Amphibolite Facies . . . . . . . . . . . . . . . . 104 PAGE Distribution and Mode of Occurrence of Important Minerals . 105 Chlorite ...................... 105 Calcite ....................... 105 Biotite ....................... 108 Garnet ....................... 108 Actinolite ..................... 108 Hornblende ..................... 110 Diopside ...................... 110 Sillimanite ..................... 110 Cordierite...................... 110 Plagioclase Feldspar ................. 110 Relation between Deformation and Metamorphism...... 111 Cause of Metamorphism ................. 112 ECONOMIC GEOLOGY .................... 113 Granite ......................... 113 Factors Affecting the Value of Granite .......... 113 Economic Classification of Granite ........... 114 Copper Deposits .................... 114 History of the Mines ................. 114 Geology of the Mines Region .............. 115 Mineralogy of the Ore ................. 115 Origin of the Ore ................... 116 Gravel Deposits ..................... 117 BIBLIOGRAPHY ...................... 118 Illustrations PLATES PAGE Frontis piece. Rock of Ages Quarry, seen from its southwestern 2 end. Prominent joint surface and a dark dike cutting the Barre granite are seen in the left side of the photograph. Grout piles in the background. PLATE 1. Geological Map of the East Bane quadrangle. Scale 1:62,500 . (in pocket) 2. Structural Map of the East Bane quadrangle . Scale 1:62,500 . (in pocket) 3. Regional geologic map and probable structure sections ...................(in pocket) PLATES PAGE 4. Bedding in the Westmore formation. Outcrop about lz miles N25°E of Cobble Hill School. Alternation of argil- laceous and arenaceous Iithology. Thicker beds are more quartzose. Schistosity parallel to bedding . . . . . . . 29 5. Sinistral folds shown by deformed quartz veins in the West- more formation on top of Mt. Pleasant ........ 52 6. Sinistral minor folds in the bedding, on the eastern flank of Mt. Pleasant, 150 yds. NE of the summit. Outcrops of the Westmore formation ...............S2 7. Early stage sinistral folds in calcareous schist of the Waits River formation. Size of the minor folds varies from a few inches to a few feet. Outcrop I Y2 miles south of Pike Hill School ...................... 55 8. Slip cleavage parallel to axial planes of small chevron folds in the Standing Pond amphibolite. Outcrop IY4 miles N70°E of Eaton School .................. 55 9. Completely recumbent acute fold in a limestone bed of the Waits River formation. Outcrop 1Y2 miles S20°E of South Washington village ................ 58 10. Acute recumbent fold in limestone beds of the Waits River formation. Picture taken obliquely to include the cross- section and the longitudinal section. Axial plane dips 20° due north. Outcrop 1V2 miles south of South Washington village ...................... 58 11. Sinistral recumbent folds in limestone beds of the Waits River formation. Outcrop back of a farm house IY6, miles S10°E of South Washington village .......... 59 12. Plastic deformation in calcareous beds of the Waits River formation. Folds plunge west, and the axial planes of folds dip 35° due NW. Outcrop 1Y2 miles N45°W of South Washington village ................. 60 13. Rotated sinistral folds of the early stage, on the crestal part of the cleavage arch. Outcrop of calcareous schist of the Waits River formation IY2 miles southeast of South Washington village ................. 60 14. Sinistral folds of the early stage deformation in the Waits River formation. Outcrop I mile SE of Waits River village 61 15. Sinistral folds in limestone bed of the Waits River formation. PLATES PAGE Outcrop in road-cut on Rte. 302, mile NW of Fuller Hill ........................ 61 16. Sharp contact between 'dark' and 'light' granite. Faint banding observable
Recommended publications
  • Poster Final
    Evidence for polyphase deformation in the mylonitic zones bounding the Chester and Athens Domes, in southeastern Vermont, from 40Ar/39Ar geochronology Schnalzer, K., Webb, L., McCarthy, K., University of Vermont Department of Geology, Burlington Vermont, USA CLM 40 39 Sample Mineral Assemblage Metamorphic Facies Abstract Microstructure and Ar/ Ar Geochronology 18CD08A Quartz, Muscovite, Biotite, Feldspar, Epidote Upper Greenschist to Lower Amphibolite The Chester and Athens Domes are a composite mantled gneiss QC Twelve samples were collected during the fall of 2018 from the shear zones bounding the Chester and Athens Domes for 18CD08B Quartz, Biotite, Feldspar, Amphibole Amphibolite Facies 18CD08C Quartz, Muscovite, Biotite, Feldspar, Epidote Upper Greenschist to Lower Amphibolite dome in southeast Vermont. While debate persists regarding Me 40 39 microstructural analysis and Ar/ Ar age dating. These samples were divided between two transects, one in the northeastern 18CD08D Quartz, Muscovite, Biotite, Feldspar, Garnet Upper Greenschist to Lower Amphibolite the mechanisms of dome formation, most workers consider the VT NH section of the Chester dome and the second in the southern section of the Athens dome. These samples were analyzed by X-ray 18CD08E Quartz, Muscovite Greenschist Facies domes to have formed during the Acadian Orogeny. This study diraction in the fall of 2018. Oriented, orthogonal thin sections were also prepared for each of the twelve samples. The thin sec- 18CD09A Quartz, Amphibole Amphib olite Facies 40 CVGT integrates the results of Ar/Ar step-heating of single mineral NY tions named with an “X” were cut parallel to the stretching lineation (X) and normal to the foliation (Z) whereas the thin sections 18CD09B Quartz, Biotite, Feldspar, Amphibole, Muscovite Amphibolite Facies grains, or small multigrain aliquots, with data from microstruc- 18CD09C Quartz, Amphibole, Feldspar Amphibolite Facies named with a “Y” have been cut perpendicular to the ‘X-Z’ thin section.
    [Show full text]
  • Mineral Industries and Geology of Certain Areas
    REPORT -->/ OF TFIE STATE GEOLOGIST ON THE S 7 (9 Mineral Industries and Geology 12 of Certain Areas OF -o VERMONT. 'I 6 '4 4 7 THIRD OF THIS SERIES, 1901-1902. 4 0 4 S GEORGE H. PERKINS, Ph. D., 2 5 State Geologist and Professor of Geology, University of Vermont 7 8 9 0 2 4 9 1 T. B. LYON C0MI'ANV, I'RINTERS, ALILiNY, New VORK. 1902. CONTENTS. PG K 1NTRODFCTION 5 SKETCH OF THE LIFE OF ZADOCK THOMPSON, G. H. Perkins ----------------- 7 LIST OF OFFICIAL REPORTS ON VERMONT GEOLOGY ----------------- -- -- ----- 14 LIST OF OTHER PUBLICATIONS ON VERMONT GEOLOGY ------- - ---------- ----- 19 SKETCH OF THE LIFE OF AUGUSTUS WING, H. M. Seely -------------------- -- 22 REPORT ON MINERAL INDUSTRIES, G. H. Perkins ............................ 35 Metallic Products ------------------------------------------------------ 32 U seful Minerals ------------------------------------------------------- 35 Building and Ornamental Stone ----------------------------------------- 40 THE GRANITE AREA OF BAItRE, G. I. Finlay------------------------------ --- 46 Topography and Surface Geology ------------------------------------ - -- 46 General Geology, Petrography of the Schists -------------------------- - -- 48 Description and Petrography of Granite Areas ----------------------------51 THE TERRANES OF ORANGE COUNTY, VERMONT, C. H. Richardson ------------ 6i Topography---------------------------- -............................. 6z Chemistry ------------------------------------------------------------66 Geology --------------------------------------------------------------
    [Show full text]
  • Mechanical Stratigraphic Controls on Natural Fracture Spacing and Penetration
    Journal of Structural Geology 95 (2017) 160e170 Contents lists available at ScienceDirect Journal of Structural Geology journal homepage: www.elsevier.com/locate/jsg Mechanical stratigraphic controls on natural fracture spacing and penetration * Ronald N. McGinnis a, , David A. Ferrill a, Alan P. Morris a, Kevin J. Smart a, Daniel Lehrmann b a Department of Earth, Material, and Planetary Sciences, Southwest Research Institute, 6220 Culebra Road, San Antonio, TX 78238-5166, USA b Geoscience Department, Trinity University, One Trinity Place, San Antonio, TX 78212, USA article info abstract Article history: Fine-grained low permeability sedimentary rocks, such as shale and mudrock, have drawn attention as Received 20 July 2016 unconventional hydrocarbon reservoirs. Fracturing e both natural and induced e is extremely important Received in revised form for increasing permeability in otherwise low-permeability rock. We analyze natural extension fracture 21 December 2016 networks within a complete measured outcrop section of the Ernst Member of the Boquillas Formation Accepted 7 January 2017 in Big Bend National Park, west Texas. Results of bed-center, dip-parallel scanline surveys demonstrate Available online 8 January 2017 nearly identical fracture strikes and slight variation in dip between mudrock, chalk, and limestone beds. Fracture spacing tends to increase proportional to bed thickness in limestone and chalk beds; however, Keywords: Mechanical stratigraphy dramatic differences in fracture spacing are observed in mudrock. A direct relationship is observed be- Natural fractures tween fracture spacing/thickness ratio and rock competence. Vertical fracture penetrations measured Fracture spacing from the middle of chalk and limestone beds generally extend to and often beyond bed boundaries into Fracture penetration the vertically adjacent mudrock beds.
    [Show full text]
  • The Geology of the Lyndonville Area, Vermont
    THE GEOLOGY OF THE LYNDONVILLE AREA, VERMONT By JOHN G. DENNIS VERMONT GEOLOGICAL SURVEY CHARLES G. DOLL, Stale Geologist Published by VERMONT DEVELOPMENT COMMISSION MONTPELIER, VERMONT BULLETIN NO. 8 1956 Lake Willoughby, seen from its north shore. TABLE OF CONTENTS ABSTRACT ......................... 7 INTRODUCTION 8 Location 8 Geologic Setting ..................... 8 Previous Work ...................... 8 Purpose of Study ..................... 9 Method of Study 10 Acknowledgments . 11 Physiography ...................... 11 STRATIGRAPHY ....................... 16 Lithologic Descriptions .................. 16 Waits River Formation ................. 16 General Statement .................. 16 Distribution ..................... 16 Age 17 Lithological Detail .................. 17 Gile Mountain Formation ................ 19 General Statement .................. 19 Distribution ..................... 20 Lithologic Detail ................... 20 The Waits River /Gile Mountain Contact ........ 22 Age........................... 23 Preliminary Remarks .................. 23 Early Work ...................... 23 Richardson's Work in Eastern Vermont .......... 25 Recent Detailed Mapping in the Waits River Formation. 26 Detailed Work in Canada ................ 28 Relationships in the Connecticut River Valley, Vermont and New Hampshire ................... 30 Summary of Presently Held Opinions ........... 32 Discussion ....................... 32 Conclusions ...................... 33 STRUCTURE 34 Introduction and Structural Setting 34 Terminology ......................
    [Show full text]
  • How Do Sedimentary Beds Form? – and Why Can We See Them? Demonstrating How the Beds in Sedimentary Rocks Are Deposited
    Earthlearningidea – https://www.earthlearningidea.com How do sedimentary beds form? – and why can we see them? Demonstrating how the beds in sedimentary rocks are deposited Sedimentary rock layers are called beds, if they are more than 1 cm thick*. Each bed was laid down by a single sedimentary event, so the beds in the photo below were laid down by many, many separate events of sand deposition. The junction between beds is called a bedding plane and is normally a flat horizontal surface. Bedding in a measuring cylinder, with sands of different colour on the left and sands of one colour (but added in several sedimentary episodes or spoonfuls) on the right. (Chris King). So, later when the sands have been compacted and cemented to form sandstones, the slight Bedding in 140 million year old sedimentary rocks, Morro differences between the top of one bed and the Solar, Lima, Peru. This series of beds has been tilted by bottom of another remain. These are later tectonic forces. attacked by weathering and erosion so that the Image licensed by Miguel Vera León under the Creative bedding plane and the beds can be seen. Commons Attribution 2.0 Generic license. Bedding planes are even clearer if there was an You can make your own beds by filling a 2 interval of time between the laying down of the measuring cylinder /3 full of water and adding upper and lower beds. In that time interval, the spoonfuls of sand. Each spoonful you add is a lower bed may have become more compacted, or single sedimentary episode and the junction partially eroded or sedimentary structures like between each layer is a bedding plane.
    [Show full text]
  • B-127 Lithostratigraphic Framework Of
    &A 'NlOO,G-3 &i flo, 12 7 g l F£i&f THE LITHOSTRATIGRAPHIC FRAMEWORK OF \;\ .-t "- THE UPPERMOST CRETACEOUS AND LOWER TERTIARY OF EASTERN BURKE COUNTY, GEORGIA Paul F. Huddlestun and Joseph H. Summerour Work Performed in Cooperation with United States Geological Survey (Cooperative Agreement Number 1434-92-A-0959) and U. S. Department of Energy (Cooperative Agreement Number DE-FG-09-92SR12868) GEORGIA DEPARTMENT OF NATURAL RESOURCES ENVIRONMENTAL PROTECTION DIVISION GEORGIA GEOLOGIC SURVEY Atlanta 1996 Bulletin 127 THE LITHOSTRATIGRAPHIC FRAMEWORK OF THE UPPERMOST CRETACEOUS AND LOWER TERTIARY OF EASTERN BURKE COUNTY, GEORGIA Paul F. Huddlestun and Joseph H. Summerour GEORGIA DEPARTMENT OF NATURAL RESOURCES Lonice C. Barrett, Commissioner ENVIRONMENTAL PROTECTION DIVISION Harold F. Reheis, Director GEORGIA GEOLOGIC SURVEY William H. McLemore, State Geologist Atlanta 1996 Bulletin 127 ABSTRACT One new formation, two new members, and a redefinition of an established lithostratigraphic unit are formally introduced here. The Oconee Group is formally recognized in the Savannah River area and four South Carolina Formations not previously used in Georgia by the Georgia Geologic Survey are recognized in eastern Burke County. The Still Branch Sand is a new formation and the two new members are the Bennock Millpond Sand Member of the Still Branch Sand and the Blue Bluff Member of the Lisbon Formation. The four South Carolina formations recognized in eastern Burke CountY include the Steel Creek Formation and Snapp Formation of the Oconee Group, the Black Mingo Formation (undifferentiated), and the Congaree Formation. The Congaree Formation and Still Branch Sand are considered to be lithostratigraphic components of the Claiborne Group.
    [Show full text]
  • GY 111 Lecture Notes Bed Attitude (AKA – Strike and Dip)
    GY 111 Lecture Notes D. Haywick (2008-09) 1 GY 111 Lecture Notes Bed Attitude (AKA – Strike and Dip) Lecture Goals: A) Beds in 3D space; the problem of orientation B) Strike and Dip C) Geological maps 1: horizontal and inclined bedding on map* Reference: Press et al., 2004, Chapter 11; Grotzinger et al., 2007, Chapter 7; p 152-154 GY 111 Lab manual Chapter 5 A) Beds in 3D space; the problem of orientation Up until now, I have been illustrating just about every important geological concept in two dimensions. For example, in the last lecture, I illustrated the Principle of Superposition with the adjacent cartoon: The thing is that beds are planes not lines and therefore, I really should have used a three dimensional or perspective cartoon to illustrate superposition. This one is more realistic, albeit a bit more annoying to draw on the fly during a lecture: GY 111 Lecture Notes D. Haywick (2008-09) 2 If you think about it, it is relatively easy to describe the orientation of horizontal bedding. All you have to say is "horizontal" and everyone immediately visualizes a flat surface ( e.g., a table, the floor, etc.). But we have a serious problem when it comes to describing the orientation of an inclined bed. Picture a tilted plane like the one drawn in the next cartoon. Were you to just say that the bed is inclined, every insightful person that you met (e.g., your fellow GY 111 classmates) would ask, "how much and in which direction?" After all, each of the beds in the next cartoon is inclined, but every one is inclined differently.
    [Show full text]
  • Vermont Geology History Slideshow
    Vermont’s Geologic History May 1st Earth’s Early History GEOLOGIC TIME SCALE The Archean and Proterozoic Eons make up the bulk of Earth’s history Oldest Rocks Found So Far The Formation of Earth: This date comes from rocky meteorites, similar in composition to Earth, that formed ~4.6 Ga (billion years ago). Rocks of Archean Age (3.8–2.5 Ga) occur on every continent. The closest Archean rocks to us are in northern Minnesota. During the Proterozoic Eon (2.5–0.54 Ga) plate tectonic processes similar to those operating today began. Rocks of Proterozoic Age (2.5–0.54 Ga) make up large parts of the continents. In combination with the older Archean rocks, these old rocks make up the core of most continents. Most rocks in New England formed during the Phanerozoic Eon. This is the time when fossils are abundant and pervasive. Stratigraphic Column: Sedimentary rocks occurring in the Champlain Valley are displayed as a vertical stack, oldest at the bottom and youngest at the top. Purple = Shale Blue = Limestone Grey = Dolostone Orange = Sandstone Continuous layers of sedimentary rock consisting of the same type or types of rock are given names, e.g. The “Glens Falls Limestone” or The “Monkton Formation.” You’ve seen some of these rocks on today’s field trip. Vermont Geologic History Dunham dolostone Cheshire Quartz Sandstone: ~530 million years old Gneiss: ~1,100 million years old The oldest rocks in Vermont are gneisses. These rocks are ~1.0–1.3 billion years old. Graph shows the Pressure/Temperature “environments” that different metamorphic rocks form in.
    [Show full text]
  • This Is the Bennington Museum Library's “History-Biography” File, with Information of Regional Relevance Accumulated O
    This is the Bennington Museum library’s “history-biography” file, with information of regional relevance accumulated over many years. Descriptions here attempt to summarize the contents of each file. The library also has two other large files of family research and of sixty years of genealogical correspondence, which are not yet available online. Abenaki Nation. Missisquoi fishing rights in Vermont; State of Vermont vs Harold St. Francis, et al.; “The Abenakis: Aborigines of Vermont, Part II” (top page only) by Stephen Laurent. Abercrombie Expedition. General James Abercrombie; French and Indian Wars; Fort Ticonderoga. “The Abercrombie Expedition” by Russell Bellico Adirondack Life, Vol. XIV, No. 4, July-August 1983. Academies. Reproduction of subscription form Bennington, Vermont (April 5, 1773) to build a school house by September 20, and committee to supervise the construction north of the Meeting House to consist of three men including Ebenezer Wood and Elijah Dewey; “An 18th century schoolhouse,” by Ruth Levin, Bennington Banner (May 27, 1981), cites and reproduces April 5, 1773 school house subscription form; “Bennington's early academies,” by Joseph Parks, Bennington Banner (May 10, 1975); “Just Pokin' Around,” by Agnes Rockwood, Bennington Banner (June 15, 1973), re: history of Bennington Graded School Building (1914), between Park and School Streets; “Yankee article features Ben Thompson, MAU designer,” Bennington Banner (December 13, 1976); “The fall term of Bennington Academy will commence (duration of term and tuition) . ,” Vermont Gazette, (September 16, 1834); “Miss Boll of Massachusetts, has opened a boarding school . ,” Bennington Newsletter (August 5, 1812; “Mrs. Holland has opened a boarding school in Bennington . .,” Green Mountain Farmer (January 11, 1811); “Mr.
    [Show full text]
  • SW Science 10 Unit 6 Relative Dating Worksheet
    SW Science 10 Unit 6 Relative Dating Worksheet Name: __________________________________ Student #: ____________ 6.2 Geologic Time 6.2.2 Relative Dating The Law of Superposition In any undisturbed sequence of strata, the oldest layer is at the bottom of the sequence, and the youngest layer is at the top of the sequence. The Cross-Cutting Law Any feature that cuts across a body of sediment or rock is younger than the body of sediment or rock that it cuts across. NOTE: • A fracture is a crack in rock. • A fault is a fracture along which movement has occurred. The Law of Inclusions If one rock body contains fragments of another rock body it must be younger than the fragments of rock it contains. OR…The inclusions are older than the rocks which contain them. Inclusions Inclusions of B are older than C. Page 2 Telling Relative Time Use the laws of superposition, inclusions and cross-cutting relationships to determine the relative ages of the following cross-sections. Determine the OLDEST bed FIRST. 1 2 3 SW SC10 UNIT 6 Earth Forces Relative Dating WS Page 3 H G F E C D B A 4 M 5 Outline the sequence of events in the cross sections below by numbering each rock unit or event in the order in which it occurred or was deposited. Youngest ________ ________ ________ ________ 6 Oldest ________ E SW SC10 UNIT 6 Earth Forces Relative Dating WS Page 4 C Refer to the cross-section on the left. For each of the following pairs of rock layers, identify the relative dating law that would be used to determine which bed was older and which was younger.
    [Show full text]
  • Primary Sedimentary Structures in Some Metamorphic Rocks
    Sedimentary Structures in Metamorphic Rocks Maine Geological Survey Maine Geologic Facts and Localities November, 2006 Primary Sedimentary Structures in Some Metamorphic Rocks Text by Thomas K. Weddle Maine Geological Survey, Department of Agriculture, Conservation & Forestry 1 Sedimentary Structures in Metamorphic Rocks Maine Geological Survey Introduction In most introductory geology classes, be it in an elementary school or at a college, students learn that there are three fundamental rock types: sedimentary, igneous, and metamorphic rocks. Sedimentary rocks are formed by the deposition of sediment by several processes, either by settling of sediment particles in a body of water, by chemical precipitation in water, or by transportation of the particles by water such as streams and rivers, or by wind (Figures 1-3). Maine Geological Survey Photo by Thomas K. Weddle K. Thomas by Photo Figure 1. Glacial marine sand beds with nearly parallel, horizontal layering, Buckfield, ME (entrenching tool for scale). Maine Geological Survey, Department of Agriculture, Conservation & Forestry 2 Sedimentary Structures in Metamorphic Rocks Maine Geological Survey Sedimentary Rocks Maine Geological Survey Photo by Thomas K. Weddle K. Thomas by Photo Figure 2. Fluvial trough cross bedding in slightly gravelly, coarse sand. The cross bed sets are incised into one another and highlighted by the darker colored layers (entrenching tool for scale), Buckfield, Maine. Maine Geological Survey, Department of Agriculture, Conservation & Forestry 3 Sedimentary Structures in Metamorphic Rocks Maine Geological Survey Sedimentary Rocks Maine Geological Survey Photo by Thomas K. Weddle K. Thomas by Photo Figure 3. Coarse cobble gravel in a glacial fluvial deposit, Kingfield, Maine (entrenching tool for scale).
    [Show full text]
  • Lithostratigraphic Units
    INTEGRATED STRATIGRAPHY Amalia Spina Amalia Spina, PhD. Office: Palazzina di Geologia, Second floor Tel. 0755852696 E-mail: [email protected] - Principles of stratigraphy - The time in stratigraphy; geological chronology (relative and absolute) the temporal sequence of events; standard global chronostratigraphical scale. Comparison between the stratigraphic scales in marine and continental successions. - Stratigraphic units standard (definition and principle): law of superimposition, principle of original horizontality, of lateral continuity and of biotic succession, the Stratigraphic Code. - The sedimentary cyclicity - Lithostratigraphy - Magnetostratigraphy - Biostratigraphy - Chemostratigraphy - Cronostratigraphy and geochronology - Astronomic cyclostratigraphy - Sequence stratigraphy - Palaeogeographic reconstructions. Prerequisites: In order to better comprehend the main topics of integrated stratigraphy, the students that follow this course must have: - knowledge of the fundamentals of geology; - knowledge of the sedimentary rocks (classification); - knowledge of the principle of stratigraphy; - knowledge of the principle of palaeontology; - knowledge of the principle of sedimentology; These preconditions are important for attending and not attending students. Written test: it consist of the solution of multiple choice test and graphic /practical exercises. The number of questions ranges between 15 and 30 on the basis of the difficulty.The test has a duration of no more than 80 minutes. The goal of the test is to verify the knowledge acquired on the course contents in order to ensure that the student learned the principles of integrated stratigraphy and its main applications. To complete the evaluation the test also consists on the discussion of a case study proposed by the Professor carried out individually or in small groups (max three students).It consists to discuss the stratigraphic features of a certain geological area and the implications for the subsurface hydrocarbon exploitation.
    [Show full text]