Historical Geology Contents

Total Page:16

File Type:pdf, Size:1020Kb

Historical Geology Contents Historical Geology Contents 0.1 Introduction .............................................. 1 0.1.1 What is historical geology? .................................. 1 0.1.2 Pre-requisites for reading this book .............................. 1 0.1.3 The purpose of this book ................................... 1 0.1.4 The introductory nature of this book ............................. 2 0.1.5 Selection of material ..................................... 2 0.1.6 Arrangement of material ................................... 2 0.1.7 Vocabulary in this book .................................... 2 0.1.8 Note on references ...................................... 2 0.1.9 Note to potential editors ................................... 3 0.1.10 Acknowledgements ...................................... 3 1 Minerals and rocks 4 1.1 Minerals ................................................ 4 1.1.1 Minerals ............................................ 4 1.1.2 Mineraloids .......................................... 4 1.1.3 Rocks ............................................. 5 1.2 Silicate minerals ............................................ 5 1.2.1 Silicate structures ....................................... 5 1.2.2 Aluminosilicates ....................................... 6 1.2.3 Felsic and mafic silicates ................................... 6 1.2.4 Note on vocabulary ...................................... 6 1.3 Rocks ................................................. 6 1.3.1 Igneous, sedimentary, and metamorphic rocks ........................ 6 1.3.2 The rock cycle ........................................ 7 1.3.3 How do we know? ...................................... 7 1.4 Igneous rocks ............................................. 7 1.4.1 Intrusive and extrusive igneous rocks ............................. 7 1.4.2 Texture ............................................ 7 1.4.3 Chemistry ........................................... 8 1.4.4 Igneous structures ....................................... 8 1.4.5 How do we know? ...................................... 9 1.4.6 Note on vocabulary ...................................... 9 i ii CONTENTS 1.5 Sedimentary rocks ........................................... 9 1.5.1 Types of sedimentary rocks .................................. 10 1.5.2 Clastic sedimentary rocks ................................... 10 1.5.3 Chemical sedimentary rocks ................................. 11 1.5.4 Biochemical sedimentary rocks ................................ 11 1.5.5 Modes of deposition ..................................... 11 1.5.6 Bedding ............................................ 11 1.5.7 How do we know? ...................................... 11 1.5.8 Note on vocabulary ...................................... 12 1.6 Metamorphic rocks .......................................... 12 1.6.1 Types of metamorphism ................................... 12 1.6.2 Chemical changes ....................................... 12 1.6.3 Metasomatism ........................................ 13 1.6.4 Textural changes ....................................... 13 1.6.5 How do we know? ...................................... 14 2 Erosion and deposition 15 2.1 Mechanical weathering and erosion .................................. 15 2.1.1 Definitions .......................................... 15 2.1.2 Mechanical weathering .................................... 15 2.1.3 Mechanical erosion ...................................... 15 2.1.4 Modes of erosion ....................................... 15 2.1.5 Transport of sediment ..................................... 16 2.1.6 How do we know? ...................................... 16 2.2 Chemical weathering ......................................... 16 2.2.1 Agents of chemical weathering ................................ 16 2.2.2 Chemical weathering of common minerals .......................... 16 2.2.3 Summary ........................................... 17 2.2.4 How do we know? ...................................... 18 2.3 Glaciers ................................................ 18 2.3.1 Formation and motion of glaciers ............................... 18 2.3.2 Types of glacier ........................................ 19 2.3.3 Erosion associated with glaciers ................................ 19 2.3.4 Deposition associated with glaciers .............................. 20 2.3.5 Former glaciers: how do we know? .............................. 21 2.4 Deserts ................................................. 22 2.4.1 Definition of a desert ..................................... 22 2.4.2 Causes of deserts ....................................... 22 2.4.3 Deserts and water ....................................... 22 2.4.4 Deserts and wind ....................................... 23 2.4.5 Lithified deserts: how do we know? .............................. 24 2.5 Volcanic ash .............................................. 24 CONTENTS iii 2.5.1 Origin and dispersal of volcanic ash ............................. 24 2.5.2 Tuff .............................................. 24 2.5.3 Volcanic ash: the igneous sediment .............................. 25 2.5.4 Volcanic ash and tuff: how do we know? ........................... 25 2.6 Soils and paleosols ........................................... 26 2.6.1 Soil: what is it? ........................................ 26 2.6.2 Paleosols: definition ...................................... 27 2.6.3 Paleosols: how do we know? ................................. 27 2.7 Rivers ................................................. 27 2.7.1 Braided and meandering rivers ................................ 28 2.7.2 Sedimentary structures .................................... 28 2.7.3 Vanished rivers: how do we know? .............................. 29 2.7.4 Note on superposed and antecedent rivers .......................... 29 2.8 Deltas ................................................. 30 2.8.1 The dynamics of a delta .................................... 30 2.8.2 Types of delta ......................................... 30 2.8.3 Former deltas: how do we know? ............................... 31 2.9 Lakes ................................................. 31 2.9.1 Lakes ............................................. 31 2.9.2 Lacustrine sedimentary rocks: how do we know? ....................... 31 2.9.3 Note on identifying freshwater organisms ........................... 32 2.10 Peat and coal ............................................. 32 2.10.1 Some definitions ....................................... 32 2.10.2 Deposition of peat ...................................... 32 2.10.3 Peatification and coalification ................................. 33 2.10.4 Coal from swamps: how do we know? ............................ 34 2.11 Nearshore sediments .......................................... 35 2.11.1 Waves and the nearshore ................................... 35 2.11.2 A note on terminology .................................... 35 2.11.3 Varieties of nearshore environment .............................. 35 2.11.4 Some nearshore sedimentary structures ............................ 35 2.11.5 Lithified nearshore sediment: how do we know? ....................... 36 2.12 Marine sediments ........................................... 37 2.12.1 The sea in profile ....................................... 37 2.12.2 Distribution of marine sediments ............................... 38 2.12.3 Types of marine sediment .................................. 38 2.12.4 Marine sediments and plate tectonics ............................. 38 2.13 Turbidites ............................................... 39 2.13.1 Turbidity currents ....................................... 39 2.13.2 Turbidity sediments and turbidites .............................. 39 2.13.3 Turbidites: how do we know? ................................. 40 iv CONTENTS 2.14 Reefs ................................................. 41 2.14.1 What is a reef? ........................................ 41 2.14.2 Reef-forming organisms ................................... 41 2.14.3 Ancient reefs: how do we know? ............................... 41 2.14.4 A puzzle and a solution .................................... 42 2.15 Ooids and oolite ............................................ 42 2.15.1 Ooids and oolite ........................................ 42 2.15.2 Oolite: how do we know? ................................... 43 2.16 Calcareous ooze ............................................ 43 2.16.1 Calcareous ooze: what is it? .................................. 43 2.16.2 The CCD ........................................... 44 2.16.3 Rocks from calcareous ooze: how do we know? ....................... 45 2.17 Siliceous ooze ............................................. 45 2.17.1 Siliceous ooze ......................................... 45 2.17.2 The opal compensation depth ................................. 46 2.17.3 Rocks from siliceous ooze: how do we know? ........................ 46 2.18 Pelagic clay .............................................. 47 2.18.1 Origin and distribution of pelagic clay ............................ 47 2.18.2 Appearance .......................................... 47 2.18.3 Lithified pelagic clay: how do we know? ........................... 48 2.19 Deposition rates ............................................ 48 2.19.1 How do we know? ...................................... 48 2.20 Glacial marine sediment ........................................ 49 2.20.1 Deposition of glacial marine sediment ............................ 49 2.20.2 Glacial marine sedimentary rocks: how do we know? .................... 49
Recommended publications
  • History of Geology
    FEBRUARY 2007 PRIMEFACT 563 (REPLACES MINFACT 60) History of geology Mineral Resources Early humans needed a knowledge of simple geology to enable them to select the most suitable rock types both for axe-heads and knives and for the ornamental stones they used in worship. In the Neolithic and Bronze Ages, about 5000 to 2500 BC, flint was mined in the areas which are now Belgium, Sweden, France, Portugal and Britain. While Stone Age cultures persisted in Britain until after 2000 BC, in the Middle East people began to mine useful minerals such as iron ore, tin, clay, gold and copper as early as 4000 BC. Smelting techniques were developed to make the manufacture of metal tools possible. Copper was probably the earliest metal to be smelted, that is, extracted from its ore by melting. Copper is obtained easily by reducing the green copper carbonate mineral malachite, itself regarded as a precious stone. From 4000 BC on, the use of clay for brick-making became widespread. The Reverend William Branwhite Clarke (1798-1878), smelting of iron ore for making of tools and the ‘father’ of geology in New South Wales weapons began in Asia Minor at about 1300 BC but did not become common in Western Europe until Aristotle believed volcanic eruptions and nearly 500 BC. earthquakes were caused by violent winds escaping from the interior of the earth. Since earlier writers had ascribed these phenomena to The classical period supernatural causes, Aristotle's belief was a By recognising important surface processes at marked step forward. Eratosthenes, a librarian at work, the Greek, Arabic and Roman civilisations Alexandria at about 200 BC, made surprisingly contributed to the growth of knowledge about the accurate measurements of the circumference of earth.
    [Show full text]
  • Standards for Geochemical Analysis of Major, Minor, and Trace Elements in Rock Powders
    50th Lunar and Planetary Science Conference 2019 (LPI Contrib. No. 2132) 1396.pdf STANDARDS FOR GEOCHEMICAL ANALYSIS OF MAJOR, MINOR, AND TRACE ELEMENTS IN ROCK POWDERS. M. Darby Dyar1, Cai R. Ytsma1, and Kate Lepore1, 1Dept. of Astronomy, Mount Holyoke Col- lege, 50 College St., South Hadley, MA 01075, [email protected]. Introduction: Analytical geochemistry has long group, Massachusetts; depended on availability of robust suites of rock stand- 2. rhyolitic volcanic glass from Mexico; locality un- ards with well-characterized compositions. Standard known, but likely from Tequila Volcano; rock powders were initially characterized and supplied 3. Hawaiian basalt collected from Kīlauea by Tim Orr to the community by the U.S. Geological Survey, (USGS, HVO); which continues to distribute a few dozen standards. 4. washed SiO2 sea sand (Fisher Scientific); Many other rock standards have subsequently been 5. Columbia River continental flood basalt collected developed by organizations such as the Centre de Re- in Moscow, Idaho by Mickey Gunter; cherches Pétrographiques et Géochimiques (CRPG) 6. rhyolite from Newberry Volcano in Oregon; and Brammer Standard Company, Inc. 7. a 50:50 by weight mixture of diopside and forsterit- Existing standards from terrestrial rocks contain ic olivine to simulate an ultramafic rock; and concentration ranges that may not cover what is present 8. granite from the Vinalhaven intrusive complex, on other bodies. Notably, Ni is a primary constituent of Maine collected by Sheila Seaman. meteorites, and thus may be abundant on ancient sur- For dopants, we used reagent-grade chemicals in the faces with impact craters [1,2]. Yet no commercial form of BN, CBaO3, C, CeO2, CoO, Cr2O3, Cs2TiO3, terrestrial rock standards come close to covering the CuO, Ga2O3, La2O3, LiCl, MnO2, MoS2, Nb2O5, NiO, possible extremes of Ni concentration that could result OPb, RbCl, CaSO4, Sc2O3, SeO2, SnO2, SrO, Y2O3, from impact contamination.
    [Show full text]
  • GE OS 1234-101 Historical Geology Lecture Syllabus Instructor
    G E OS 1234-101 Historical Geology Lecture Syllabus Instructor: Dr. Jesse Carlucci ([email protected]), (940) 397-4448 Class: MWF, 10am -10:50am, BO 100 Office hours: Bolin Hall 131, MWF, 11am ± 2pm, Tuesday, noon - 2pm. You can arrange to meet with me at any time, by appointment. Textbook: Earth System History by Steven M. Stanley, 3rd edition. I will occasionally post articles and other readings on blackboard. I will also upload Power Point presentations to blackboard before each class, if possible. Course Objectives: Historical Geology provides the student with a comprehensive survey of the history of life, and major events in the physical development of Earth. Most importantly, this class addresses how processes like plate tectonics and climate interact with life, forming an integrated system. The first half of the class focuses on concepts, and the second on a chronologic overview of major biological and physical events in different geologic periods. L E C T UR E SC H E DU L E Aug 27-31: Overview of course; what is science? The Earth as a planet Stanley (pg. 244-247) Sep 5-7: Earth materials, rocks and minerals Stanley (pg. 13-17; 25-34) Sep 10-14: Rocks & minerals continued; plate tectonics. Stanley (pg. 3-12; 35-46; 128-141; 175-186) Sep 17-21: Geological time and dating of the rock record; chemical systems, the climate system through time. Quiz 1 (Sep 19; 5%). Stanley (pg. 187-194; 196-207; 215-223; 232-238) Sep 24-28: Sedimentary environments and life; paleoecology. Stanley (pg. 76-80; 84-96; 99-123) Oct 1-5: Biological evolution and the fossil record.
    [Show full text]
  • GEOL 1104 Historical Geology
    Administrative Master Syllabus Course Information Course Title Historical Geology Laboratory Course Prefix, Num. and Title GEOL 1104 Division Life Sciences Department Geology Course Type Academic WCJC Core Course Course Catalog Description This laboratory-based course accompanies GEOL 1304, Historical Geography. Laboratory activities will introduce methods used by scientists to interpret the history of life and major events in the physical development of Earth from rocks and fossils. Pre-Requisites Credit for or concurrent enrollment in GEOL1304 Co-Requisites Enter Co-Requisites Here. Semester Credit Hours Total Semester Credit Hours (SCH): Lecture Hours: 1:0:2 Lab/Other Hours Equated Pay Hours 1.2 Lab/Other Hours Breakdown: Lab Hours 2 Lab/Other Hours Breakdown: Clinical Hours Enter Clinical Hours Here. Lab/Other Hours Breakdown: Practicum Hours Enter Practicum Hours Here. Other Hours Breakdown List Total Lab/Other Hours Here. Approval Signatures Title Signature Date Prepared by: Department Head: Division Chair: Dean/VPI: Approved by CIR: Rev. January 2020 Additional Course Information Topical Outline: Each offering of this course must include the following topics (be sure to include information regarding lab, practicum, and clinical or other non-lecture instruction). 1. The Sedimentary Environment 2. Geochronology Part I: Relative Dating of Strata 3. Geochronology Part II: Absolute or Radiometric Dating of Strata 4. Fossils, Taxonomy, and the Species Concept 5. The Sponges: Early Multi-celled Animals 6. The Corals and their Relatives 7. The Bryozoans: “Lacy Animals” 8. The Brachiopods: Bivalved Lophophorates 9. The Bivalves: Clams, Oysters, and Relatives 10. The Gastropods: Snails, Slugs, and Relativesacticum, and clinical or other non-lecture instruction).
    [Show full text]
  • Bedrock Geology Glossary from the Roadside Geology of Minnesota, Richard W
    Minnesota Bedrock Geology Glossary From the Roadside Geology of Minnesota, Richard W. Ojakangas Sedimentary Rock Types in Minnesota Rocks that formed from the consolidation of loose sediment Conglomerate: A coarse-grained sedimentary rock composed of pebbles, cobbles, or boul- ders set in a fine-grained matrix of silt and sand. Dolostone: A sedimentary rock composed of the mineral dolomite, a calcium magnesium car- bonate. Graywacke: A sedimentary rock made primarily of mud and sand, often deposited by turbidi- ty currents. Iron-formation: A thinly bedded sedimentary rock containing more than 15 percent iron. Limestone: A sedimentary rock composed of calcium carbonate. Mudstone: A sedimentary rock composed of mud. Sandstone: A sedimentary rock made primarily of sand. Shale: A deposit of clay, silt, or mud solidified into more or less a solid rock. Siltstone: A sedimentary rock made primarily of sand. Igneous and Volcanic Rock Types in Minnesota Rocks that solidified from cooling of molten magma Basalt: A black or dark grey volcanic rock that consists mainly of microscopic crystals of pla- gioclase feldspar, pyroxene, and perhaps olivine. Diorite: A plutonic igneous rock intermediate in composition between granite and gabbro. Gabbro: A dark igneous rock consisting mainly of plagioclase and pyroxene in crystals large enough to see with a simple magnifier. Gabbro has the same composition as basalt but contains much larger mineral grains because it cooled at depth over a longer period of time. Granite: An igneous rock composed mostly of orthoclase feldspar and quartz in grains large enough to see without using a magnifier. Most granites also contain mica and amphibole Rhyolite: A felsic (light-colored) volcanic rock, the extrusive equivalent of granite.
    [Show full text]
  • Weathering, Erosion, and Susceptibility to Weathering Henri Robert George Kenneth Hack
    Weathering, erosion, and susceptibility to weathering Henri Robert George Kenneth Hack To cite this version: Henri Robert George Kenneth Hack. Weathering, erosion, and susceptibility to weathering. Kanji, Milton; He, Manchao; Ribeira e Sousa, Luis. Soft Rock Mechanics and Engineering, Springer Inter- national Publishing, pp.291-333, 2020, 9783030294779. 10.1007/978-3-030-29477-9. hal-03096505 HAL Id: hal-03096505 https://hal.archives-ouvertes.fr/hal-03096505 Submitted on 5 Jan 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Published in: Hack, H.R.G.K., 2020. Weathering, erosion and susceptibility to weathering. 1 In: Kanji, M., He, M., Ribeira E Sousa, L. (Eds), Soft Rock Mechanics and Engineering, 1 ed, Ch. 11. Springer Nature Switzerland AG, Cham, Switzerland. ISBN: 9783030294779. DOI: 10.1007/978303029477-9_11. pp. 291-333. Weathering, erosion, and susceptibility to weathering H. Robert G.K. Hack Engineering Geology, ESA, Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente Enschede, The Netherlands e-mail: [email protected] phone: +31624505442 Abstract: Soft grounds are often the result of weathering. Weathering is the chemical and physical change in time of ground under influence of atmosphere, hydrosphere, cryosphere, biosphere, and nuclear radiation (temperature, rain, circulating groundwater, vegetation, etc.).
    [Show full text]
  • Geologic Timeline
    SCIENCE IN THE PARK: GEOLOGY GEOLOGIC TIME SCALE ANALOGY PURPOSE: To show students the order of events and time periods in geologic time and the order of events and ages of the physiographic provinces in Virginia. BACKGROUND: Exact dates for events change as scientists explore geologic time. Dates vary from resource to resource and may not be the same as the dates that appear in your text book. Analogies for geologic time: a 24 hour clock or a yearly calendar. Have students or groups of students come up with their own original analogy. Before you assign this activity, you may want to try it, depending on the age of the student, level of the class, or time constraints, you may want to leave out the events that have a date of less than 1 million years. ! Review conversions in the metric system before you begin this activity ! References L.S. Fichter, 1991 (1997) http://csmres.jmu.edu/geollab/vageol/vahist/images/Vahistry.PDF http://pubs.usgs.gov/gip/geotime/age.html Wicander, Reed. Historical Geology. Fourth Edition. Toronto, Ontario: Brooks/Cole, 2004. Print. VIRGINIA STANDARDS OF LEARNING ES.10 The student will investigate and understand that many aspects of the history and evolution of the Earth can be inferred by studying rocks and fossils. Key concepts include: relative and absolute dating; rocks and fossils from many different geologic periods and epochs are found in Virginia. Developed by C.P. Anderson Page 1 SCIENCE IN THE PARK: GEOLOGY Building a Geologic Time Scale Time: Materials Meter stick, 5 cm adding machine tape, pencil, colored pencils Procedure 1.
    [Show full text]
  • GEOLOGY THEME STUDY Page 1
    NATIONAL HISTORIC LANDMARKS Dr. Harry A. Butowsky GEOLOGY THEME STUDY Page 1 Geology National Historic Landmark Theme Study (Draft 1990) Introduction by Dr. Harry A. Butowsky Historian, History Division National Park Service, Washington, DC The Geology National Historic Landmark Theme Study represents the second phase of the National Park Service's thematic study of the history of American science. Phase one of this study, Astronomy and Astrophysics: A National Historic Landmark Theme Study was completed in l989. Subsequent phases of the science theme study will include the disciplines of biology, chemistry, mathematics, physics and other related sciences. The Science Theme Study is being completed by the National Historic Landmarks Survey of the National Park Service in compliance with the requirements of the Historic Sites Act of l935. The Historic Sites Act established "a national policy to preserve for public use historic sites, buildings and objects of national significance for the inspiration and benefit of the American people." Under the terms of the Act, the service is required to survey, study, protect, preserve, maintain, or operate nationally significant historic buildings, sites & objects. The National Historic Landmarks Survey of the National Park Service is charged with the responsibility of identifying America's nationally significant historic property. The survey meets this obligation through a comprehensive process involving thematic study of the facets of American History. In recent years, the survey has completed National Historic Landmark theme studies on topics as diverse as the American space program, World War II in the Pacific, the US Constitution, recreation in the United States and architecture in the National Parks.
    [Show full text]
  • The Breakdown of Rocks Mechanical Weathering
    Weathering: The Breakdown of Rocks Mechanical Weathering: Breaks rocks into smaller particles Chemical Weathering: Alters rock by chemical reactions Mechanical Weathering 1) Ice Wedging *Results from 9% expansion when water turns to ice. *High stress (110kg/cm2, about the wedge of a sledge) *It occurs when: >Adequate supply of moisture >Have preexisting fractures, cracks, and voids >Temperature rises above and below freezing *Was even used in some quarry operations to break up rock 2) Sheeting *Results from release of confining pressures *Has been observes directly in quarries and mines, even in roadways *Sheeting from heat results in a rock spalling *Spalling: surface of rock expands due to extreme heating but core of rock remains cool 3) Disintegration *Breakdown of rock into smaller pieces by critters, plants, etc. Results of Mechanical Weathering Talus Cones (From ice wedging mostly) Boulder fields (From ice wedging mostly) Jointing: Cracks in the rock from ice wedging and sheeting Chemical Weathering: Rocks are decomposed and the internal structure of the minerals is destroyed, and new minerals are created. 1) Hydrolysis: Chemical union of water and a mineral *Ex. Feldspar → clay mineral Water first form carbonic acid by combining with carbon dioxide in the reaction: H2 O + CO2 = H2 CO3 Then the mineral is broken down: 4NaAl3Si3O8 + 4H2CO3 + 18H2O → 4Na + 4HCO3 + 8H4SiO4 + Al4O10(OH)3 (Plagioclase) (carbonic acid) (water) (Dissolved components) (clay mineral) Sodium becomes displaced 2) Dissolution: Process where by rock material passes directly into solution, like salt in water *Most important minerals to do this: CARBONATES (Calcite;dolomite) Dissolution (continue) Water is a universal solvent due to its polar nature Behaves like a magnet A good example is limestone which is made of calcite or dolomite In wet areas, it forms valleys In arid areas, it forms cliffs Some rock types can be completely dissolved and leached (flushed away by water) Best examples are natural salt (halite) and gypsum.
    [Show full text]
  • History of Geological Science – Silvia F
    GEOLOGY – History of Geological Science – Silvia F. de M. Figueiroa HISTORY OF GEOLOGICAL SCIENCE Silvia F. de M. Figueirôa Department of Geological Education, Institute of Geosciences / University of Campinas (UNICAMP), P.O. box 6152 13083-970, Campinas-SP, Brazil Keywords: history, geology, mineralogy, paleontology, earth, mining, geological surveys, maps, gemstones, stratigraphy, fossils. Contents 1. Beginnings 2. Middle Ages and the Renaissance 3. The ‘Scientific revolution’ and its long-lasting impacts 4. Industrial Revolution, the search for raw materials and the survey of territories Glossary Bibliography Biographical Sketch Summary This chapter aims to provide a broad picture of the development of geological science, as detailed as possible. Geology as a modern science started roughly around two centuries ago. But as knowledge of the Earth it has existed since the beginnings of humankind. We begin by mentioning the ideas of ancient peoples – Greeks and Romans. We continue up to the Renaissance (15th century), explaining that practically all schools of thought shared a fairly integrated and unified vision of all the Cosmos. In a Geocentric world, Earth suffered the influence of all other planets and stars and so did everything in it, whether it was human, animal, vegetal or mineral. The planet was not composed only of its own element, but also by fire, water and air, as Aristotle had already postulated. The context of the so-called ‘Scientific Revolution’ implicated profound changes and discoveries that led to a conceptual revision of the knowledge about the Earth: Astronomy redefined by Copernicus denied the central place of the earth in the planetary system. At the same time, the construction and use of the telescope showed that the world was almost infinitely large, and that Earth and the Solar System did not occupy a special place in the Universe.
    [Show full text]
  • GEOL 5 Historical Geology & Paleontology(C-ID GEOL 111)
    Lassen Community College Course Outline GEOL-5 Historical Geology & Paleontology 4.0 Units I. Catalog Description This course is designed to provide a descriptive geological history of the earth using the principles and methods of interpretation and reconstruction of the changes that have occurred on the earth in the fossil record. Recommended Preparation: Successful completion of ENGL105 or equivalent multiple measures placement. Transfers to both UC/CSU General Education Area: A CSU GE Area: B1 & B3 IGETC GE Area: 5A & 5C C-ID GEOL 111 51 Hours Lecture, 51 Hours Lab Scheduled: Spring II. Coding Information Repeatability: Not Repeatable, Take 1 Time Grading Option: Graded or Pass/No Pass Credit Type: Credit - Degree Applicable TOP Code: 191400 III. Course Objectives A. Course Student Learning Outcomes Upon completion of this course the student will be able to: 1. Outline the earth's history through construction of a geological time scale and evolution of organisms. 2. Apply proper lab techniques and knowledge of theoretical concepts in geology to acquire and interpret geologic data and formulate new questions in a laboratory setting. B. Course Objectives Upon completion of this course the student will be able to: 1. Explain and practically apply the principles of the scientific method. 2. Discuss earth's origin and evolution. 3. Identify the basic physical features of the earth. 4. Describe how the record of the past is expressed in the sedimentary rocks of the earth. 5. Examine and interpret evidence of geologic activity and the presence of life in the major areas of geologic time. 6. Discuss how the past is the key to the present.
    [Show full text]
  • World Deserts
    HISTORY AND GEOGRAPHY World Deserts Reader Frog in the Australian Outback Joshua tree in the Mojave Desert South American sheepherder Camel train across the Sahara Desert THIS BOOK IS THE PROPERTY OF: STATE Book No. PROVINCE Enter information COUNTY in spaces to the left as PARISH instructed. SCHOOL DISTRICT OTHER CONDITION Year ISSUED TO Used ISSUED RETURNED PUPILS to whom this textbook is issued must not write on any page or mark any part of it in any way, consumable textbooks excepted. 1. Teachers should see that the pupil’s name is clearly written in ink in the spaces above in every book issued. 2. The following terms should be used in recording the condition of the book: New; Good; Fair; Poor; Bad. World Deserts Reader Creative Commons Licensing This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License. You are free: to Share—to copy, distribute, and transmit the work to Remix—to adapt the work Under the following conditions: Attribution—You must attribute the work in the following manner: This work is based on an original work of the Core Knowledge® Foundation (www.coreknowledge.org) made available through licensing under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License. This does not in any way imply that the Core Knowledge Foundation endorses this work. Noncommercial—You may not use this work for commercial purposes. Share Alike—If you alter, transform, or build upon this work, you may distribute the resulting work only under the same or similar license to this one. With the understanding that: For any reuse or distribution, you must make clear to others the license terms of this work.
    [Show full text]