References Cited in the Database (Asbestos Sites.Xls)
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
RI37 Stratigraphic Nomenclature Of
,--' ( UNIVERSITY OF DELAWARE DELAWARE GEOLOGICAL SURVEY REPORT OF INVESTIGATIONS NO.37 STRATIGRAPHIC NOMENCLATURE OF NONMARINE CRETACEOUS ROCKS OF INNER MARGIN OF COASTAL PLAIN IN DELAWARE AND ADJACENT STATES BY ROBERT R. JORDAN STATE OF DELAWARE.. NEWARK, DELAWARE JUNE 1983 STRATIGRAPHIC NOMENCLATURE OF NONMARINE CRETACEOUS ROCKS OF INNER MARGIN OF COASTAL PLAIN IN DELAWARE AND ADJACENT STATES By Robert R. Jordan Delaware Geological Survey June 1983 TABLE OF CONTENTS Page ABSTRACT. ....... 1 INTRODUCTION ..... 2 Purpose and Scope. 2 Acknowledgments.. 4 REGIONAL SETTING. 4 Regional Relationships . 4 Structural Features. 5 DESCRIPTIONS OF UNITS .. 8 Historical Summary 8 Potomac Formation. 13 Nomenclature. 13 Extent. 13 Lithology . 14 Patuxent Formation . 18 Nomenclature. 18 Extent.. 18 Lithology .... 18 Arundel Formation. 19 Nomenclature.. 19 Extent. .• 19 Lithology • 20 Page Patapsco Formation. .. 20 Nomenclature . 20 Extent .. 20 Lithology.. 20 Raritan Formation . 21 Nomenclature .. 21 Extent .. 22 Lithology.. 23 Magothy Formation .. 24 Nomenclature . 24 Extent .. 24 Lithology.. 25 ENVIRONMENTS OF DEPOSITION 28 AGES .... 29 SUBDIVISIONS AND CORRELATIONS .. 32 REFERENCES . 34 ILLUSTRATIONS Figure 1. Geologic map of nonmarine Cretaceous deposits .. ..•.• •.. 3 2. Structural features of the Coastal Plain. ............ 6 3. Schematic diagram of lateral and vertical relationships of nonmarine Cretaceous deposits•....•... 34 TABLES Page Table 1. Usage of group and formation names. 9 STRATIGRAPHIC NOMENCLATURE OF NONMARINE CRETACEOUS ROCKS OF INNER MARGIN OF COASTAL PLAIN IN DELAWARE AND ADJACENT STATES ABSTRACT Rocks of Cretaceous age deposited in continental and marginal environments, and now found along the inner edge of the northern Atlantic Coastal Plain, have historically been classified as the Potomac Group and the Potomac, Patuxent, Arundel, Patapsco, Raritan, and Magothy forma tions. -
A Review of the Structural Architecture of Tellurium Oxycompounds
Mineralogical Magazine, May 2016, Vol. 80(3), pp. 415–545 REVIEW OPEN ACCESS A review of the structural architecture of tellurium oxycompounds 1 2,* 3 A. G. CHRISTY ,S.J.MILLS AND A. R. KAMPF 1 Research School of Earth Sciences and Department of Applied Mathematics, Research School of Physics and Engineering, Australian National University, Canberra, ACT 2601, Australia 2 Geosciences, Museum Victoria, GPO Box 666, Melbourne, Victoria 3001, Australia 3 Mineral Sciences Department, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, CA 90007, USA [Received 24 November 2015; Accepted 23 February 2016; Associate Editor: Mark Welch] ABSTRACT Relative to its extremely low abundance in the Earth’s crust, tellurium is the most mineralogically diverse chemical element, with over 160 mineral species known that contain essential Te, many of them with unique crystal structures. We review the crystal structures of 703 tellurium oxysalts for which good refinements exist, including 55 that are known to occur as minerals. The dataset is restricted to compounds where oxygen is the only ligand that is strongly bound to Te, but most of the Periodic Table is represented in the compounds that are reviewed. The dataset contains 375 structures that contain only Te4+ cations and 302 with only Te6+, with 26 of the compounds containing Te in both valence states. Te6+ was almost exclusively in rather regular octahedral coordination by oxygen ligands, with only two instances each of 4- and 5-coordination. Conversely, the lone-pair cation Te4+ displayed irregular coordination, with a broad range of coordination numbers and bond distances. -
Ii. Natural Resources of the Greenwood Lake Watershed
II. NATURAL RESOURCES II. NATURAL RESOURCES OF THE GREENWOOD LAKE WATERSHED A. LAND RESOURCES Geologic History The Greenwood Lake Watershed is located in the Highlands Physiographic Province, as shown in Figure II.A-1. The Highlands are underlain by the oldest rocks in New Jersey. These Precambrian igneous and metamorphic rocks were formed between 1.3 billion and 750 million years ago by the melting and recrystallization of sedimentary rocks that were deeply buried, subjected to high pressure and temperature, and intensely deformed.1 The Precambrian rocks are interrupted by several elongate northeast-southwest trending belts of folded Paleozoic sedimentary rocks equivalent to the rocks of the Valley and Ridge Province. Figure II.A-1 - Physiographic Provinces of New Jersey 1 New Jersey Geological Survey, NJ Department of Environmental Protection. 1999. The Geology of New Jersey. II-1 II. NATURAL RESOURCES The Highlands ridges in New Jersey are a southward continuation of the Green or Taconic Mountains of Vermont and Massachusetts, the New England Upland of Connecticut, and the Hudson Highlands of New York.2 The ridges continue through Pennsylvania to the vicinity of Reading. This Reading Prong of the New England Physiographic Province plunges beneath the surface of younger rocks for a distance of about fifty miles southwest of Reading and reappears where the northern end of the Blue Ridge Mountains begins to rise above the surrounding country. The Blue Ridge Mountains of the Virginia Appalachians, the mountains of New England, and the Highlands of New Jersey and New York all have a similar geologic history and character. Topography The granites and gneisses of the Highlands are resistant to erosion and create a hilly upland dissected by the deep, steep-sided valleys of major streams.3 The Highlands can be characterized as broad high ridges composed of complex folded and faulted crystalline rocks and separated by deep narrow valleys.4 The topography follows the northeast-southwest trend of the geologic structure and rock formations. -
Bedrock Geologic Map of New Jersey
O O O 74 00’ BEDROCK GEOLOGIC MAP 75 00’ 74 30’ OF NEW JERSEY DESCRIPTION OF MAP UNITS SUSSEX Sedimentary Rocks Franklin CENOZOIC PASSAIC Mahwah Holocene: beach and Newton 41O 00’ estuarine deposits Andover Paleogene and Neogene: sand, silt, clay Delaware Water Gap Boonton BERGEN MESOZOIC WARREN Paterson Cretaceous: sand, silt, clay Hackensack Jurassic: siltstone, shale, Belvidere MORRIS sandstone, conglomerate ESSEX Morristown Triassic: siltstone, shale, HUDSON Newark sandstone, conglomerate Jersey City Gladstone Phillipsburg PALEOZOIC UNION Devonian: conglomerate, sandstone, Elizabeth shale, limestone Somerville Carteret Silurian: conglomerate, sandstone, Milford shale, limestone HUNTERDON New Brunswick 40O 30’ Ordovician: shale, limestone Flemington SOMERSET Cambrian: limestone, sandstone MIDDLESEX Igneous and Metamorphic Rocks MESOZOIC Jurassic and Triassic: basalt MERCER Jurassic: diabase Freehold MONMOUTH PALEOZOIC N Trenton Asbury Park Ordovician and Cambrian: schist, gneiss MESOPROTEROZOIC marble gneiss, granite O Mount Holly 40 00’ DESCRIPTION OF MAP SYMBOLS Toms River limit of late Wisconsinan glaciation Camden OCEAN limit of Illinoian glaciation BURLINGTON limit of pre-Illinoian glaciation Woodbury CAMDEN GLOUCESTER SALEM Salem O O 39 30’ ATLANTIC 39 30’ Bridgeton Mays Landing ICAL A OG ND L EO W CUMBERLAND G A T Y E E R Atlantic City S S R U E J R V E W E Y N 1835 0 5 10 15 20 mi Department of Environmental Protection CAPE MAY NEW JERSEY GEOLOGICAL AND WATER SURVEY 0 10 20 30 km Cape May 2017 Court House scale 1:1,000,000 39O 00’ O O O O O 76 00’ 75 30’ 75 00’ 74 30’ 74 00’ BEDROCK GEOLOGY OF NEW JERSEY For an area of its size, New Jersey has a uniquely diverse and interesting basalt and diabase are more resistant to erosion than the enclosing sandstone geology. -
By Michael Fleischer and Constance M. Schafer Open-File Report 81
U.S. DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY THE FORD-FLEISCHER FILE OF MINERALOGICAL REFERENCES, 1978-1980 INCLUSIVE by Michael Fleischer and Constance M. Schafer Open-File Report 81-1174 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards 1981 The Ford-Fleischer File of Mineralogical References 1978-1980 Inclusive by Michael Fleischer and Constance M. Schafer In 1916, Prof. W.E. Ford of Yale University, having just published the third Appendix to Dana's System of Mineralogy, 6th Edition, began to plan for the 7th Edition. He decided to create a file, with a separate folder for each mineral (or for each mineral group) into which he would place a citation to any paper that seemed to contain data that should be considered in the revision of the 6th Edition. He maintained the file in duplicate, with one copy going to Harvard University, when it was agreed in the early 1930's that Palache, Berman, and Fronde! there would have the main burden of the revision. A number of assistants were hired for the project, including C.W. Wolfe and M.A. Peacock to gather crystallographic data at Harvard, and Michael Fleischer to collect and evaluate chemical data at Yale. After Prof. Ford's death in March 1939, the second set of his files came to the U.S. Geological Survey and the literature has been covered since then by Michael Fleischer. Copies are now at the U.S. Geological Survey at Reston, Va., Denver, Colo., and Menlo Park, Cal., and at the U.S. -
Cambridge University Press 978-1-107-10626-0 — Minerals 2Nd Edition Index More Information
Cambridge University Press 978-1-107-10626-0 — Minerals 2nd Edition Index More Information Index Bold entries are mineral names. Page numbers in bold refer to minerals with detailed descriptions. Page numbers in italics refer to pictures. Abbe refractometer, 170, 191 American Mineralogist Crystal Structure Database, 143 aberrations in lenses, 172 amethyst, 50, 308, Plate 2c absorption, 217 amosite, 529 absorption of light, 186 optical micrograph, 532 absorption spectra, supernovae, 537 TEM image, 532 abundance of elements, 16 amphibole, 445 acetic acid, structure, 474 extinction angle, 212 acetone, structure, 474 minerals and composition, 439 acid mine drainage, 533 optical orientation, 211 actinolite, 449, 529 optical properties, 209 acute bisectrix, 199 quadrilateral, 444 adularia, 309 structure, 438 from Alps, Plate 21a amphibolite facies, 415 African Copper Belt, 374 analcime, 469 agate, 308 from Italy, SEM image, 465 aggregate, 518 analyzer, 173, 176 aggregation, 127 anatase, 392 of crystals, 127 from Swiss Alps, Plate 28d Agricola, 5, 481 structure and symmetry, 104 Airy’s spiral, 202 andalusite, 408 Al2SiO5, phase diagram, 276 optical orientation, 214 alabandite, 539 optical properties, 215 albite, 301, 310 porphyroblast, Plate 5c from New Mexico, Plate 21d andesine, 301 Albite twin law, 112, 311 anglesite, 355 Algoma-type iron deposits, 491 anhedral shape, 49 alite, 519 anhydrite, 355 alkali feldspars, 301, 309 animal nutrition, zeolites, 471 optical indicatrix, 205 aniom, 19 phase diagram, 306, 314 anisotropy, 149 alkali–silica -
A History of Millburn Township Ebook
A History of Millburn Township eBook A History of Millburn Township »» by Marian Meisner Jointly published by the Millburn/Short Hills Historical Society and the Millburn Free Public Library. Copyright, July 5, 2002. file:///c|/ebook/main.htm9/3/2004 6:40:37 PM content TABLE OF CONTENTS I. Before the Beginning - Millburn in Geological Times II. The First Inhabitants of Millburn III. The Country Before Settlement IV. The First English Settlements in Jersey V. The Indian Deeds VI. The First Millburn Settlers and How They Lived VII. I See by the Papers VIII. The War Comes to Millburn IX. The War Leaves Millburn and Many Loose Ends are Gathered Up X. The Mills of Millburn XI. The Years Between the Revolution and the Coming of the Railroad XII. The Coming of the Railroad XIII. 1857-1870 XIV. The Short Hills and Wyoming Developments XV. The History of Millburn Public Schools XVI. A History of Independent Schools XVII. Millburn's Churches XVIII. Growing Up file:///c|/ebook/toc.htm (1 of 2)9/3/2004 6:40:37 PM content XIX. Changing Times XX. Millburn Township Becomes a Centenarian XXI. 1958-1976 file:///c|/ebook/toc.htm (2 of 2)9/3/2004 6:40:37 PM content Contents CHAPTER I. BEFORE THE BEGINNING Chpt. 1 MILLBURN IN GEOLOGICAL TIMES Chpt. 2 Chpt. 3 The twelve square miles of earth which were bound together on March 20, Chpt. 4 1857, by the Legislature of the State of New Jersey, to form a body politic, thenceforth to be known as the Township of Millburn, is a fractional part of the Chpt. -
Triassic and Jurassic Formations of the Newark Basin
TRIASSIC AND JURASSIC FORMATIONS OF THE NEWARK BASIN PAUL E. OLSEN Bingham Laboratories, Department of Biology, Yale University, New Haven, Connecticut Abstract Newark Supergroup deposits of the Newark Basin 1946), makes this deposit ideal for studying time-facies (New York, New Jersey and Pennsylvania) are divided relationships and evolutionary phenomena. These into nine formations called (from bottom up): Stockton recent discoveries have focused new interest on Newark Formation (maximum 1800 m); Lockatong Formation strata. (maximum 1150 m); Passaic Formation (maximum 6000 m); Orange Mountain Basalt (maximum 200 m); The Newark Basin (Fig. 1 and 2) is the largest of the Feltville Formation (maximum 600 m); Preakness exposed divisions of the Newark Supergroup, covering Basalt (maximum + 300 m); Towaco Formation (max- about 7770 km2 and stretching 220 km along its long imum 340 m); Hook Mountain Basalt (maximum 110 axis. The basin contains the thickest sedimentary se- m); and Boonton Formation (maximum + 500 m). Each quence of any exposed Newark Supergroup basin and formation is characterized by its own suite of rock correspondingly covers the greatest continuous amount - types, the differences being especially obvious in the of time. Thus, the Newark Basin occupies a central posi- number, thickness, and nature of their gray and black tion in the study of the Newark Supergroup as a whole. sedimentary cycles (or lack thereof). In well over a century of study the strata of Newark Fossils are abundant in the sedimentary formations of Basin have received a relatively large amount of atten- the Newark Basin and provide a means of correlating tion. By 1840, the basic map relations were worked out the sequence with other early Mesozoic areas. -
The Glacial Geology of New York City and Vicinity, P
Sanders, J. E., and Merguerian, Charles, 1994b, The glacial geology of New York City and vicinity, p. 93-200 in A. I. Benimoff, ed., The Geology of Staten Island, New York, Field guide and proceedings, The Geological Association of New Jersey, XI Annual Meeting, 296 p. John E. Sanders* and Charles Merguerian Department of Geology 114 Hofstra University Hempstead, NY 11549 *Office address: 145 Palisade St. Dobbs Ferry, NY 10522 ABSTRACT The fundamental question pertaining to the Pleistocene features of the New York City region is: "Did one glacier do it all? or was more than one glacier involved?" Prior to Fuller's (1914) monographic study of Long Island's glacial stratigraphy, the one-glacier viewpoint of T. C. Chamberlin and R. D. Salisbury predominated. In Fuller's classification scheme, he included products of 4 glacial advances. In 1936, MacClintock and Richards rejected two of Fuller's key age assignments, and made a great leap backward to the one-glacier interpretation. Subsequently, most geologists have accepted the MacClintock-Richards view and have ignored Fuller's work; during the past half century, the one-glacial concept has become a virtual stampede. What is more, most previous workers have classified Long Island's two terminal- moraine ridges as products of the latest Pleistocene glaciation (i. e., Woodfordian; we shall italicize Pleistocene time terms). Fuller's age assignment was Early Wisconsinan. A few exceptions to the one-glacier viewpoint have been published. In southern CT, Flint (1961) found two tills: an upper Hamden Till with flow indicators oriented NNE-SSW, and a lower Lake Chamberlain Till with flow indicators oriented NNW-SSE, the same two directions of "diluvial currents" shown by Percival (1842). -
Morristown National Historical Park Geologic Resources Inventory Report
National Park Service US Department of the Interior Natural Resource Stewardship and Science Morristown National Historical Park Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2014/841 ON THE COVER Cannon at Fort Nonsense overlooking Morristown. Photograph by Jared Kofsky (Creative Commons Attribution-Share Alike 3.0 Unported [CC BY-SA 3.0] license) available at: http://commons.wikimedia.org/wiki/File:Fort_Nonsense_of_Morristown.JPG (accessed 12 August 2014) THIS PAGE Split-rail fence at Jockey Hollow in the winter. Photograph by Daniel Beards, available at: http://albums.phanfare.com/isolated/CUUsqZbg/1/6144461_7039483 (accessed 12 August 2014) Morristown National Historical Park Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2014/841 Trista L. Thornberry-Ehrlich Colorado State University Research Associate National Park Service Geologic Resources Division Geologic Resources Inventory PO Box 25287 Denver, CO 80225 August 2014 US Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. -
Download the Scanned
American Mineralogist, Volume 65, pages 599-623, 1980 Microstructures and reaction mechanismsin biopyriboles Devro R. VnnreN AND PETERR. BusEcK Departmentsof Geologysnd Chemistry,Arizona State University Tempe,Arizona 85281 Abstract High-resolution transmission electron microscopy of ferromagnesian chain and sheet sili- cates from a metamorphosed ultramafic body at Chester, Vermont has revealed a wide vari- ety of structural defects.Images of thesemicrostructures have been interpreted by analogy with images of ordered chain silicates and with the aid of dynamical diflraction and imaging calculations.Most of the defectsare concentratedin regionsof chain-width disorder;they ap- parently result from retrogradereaction ofanthophyllite to talc and from deformation of the ultramafic body. The most common defects are the terminations of (010) slabs having a given chain width. Theseslabs, referred to as "zippers," in most casesterminate coherently,with no displacive planar defects associated with the termination. Two theoretically-derived rules must be obeyedfor coherenttermination. Rule l: the terminating zipper must have the samenumber of subchains as the material it replaces.Rule 2: the numbers of silicate chains in the zipper and in the material it replacesmust both be even, or they must both be odd. Where these rules are disobeyed, zipper terminations are usually associatedwith planar faults having dis- placementsprojected on (001) of either % [010] or t/+[fi)], referred to an anthophyllite cell. In rare cases,violation of the replacement rules results in severestructural distortion, rather than the creation of displacive planar faults. These replacement rules hold for all pyriboles and may [s s6ahqlling factors not only in reactionsinvolving amFhib,ole,but in pyroxene hydration reactions as well. -
Physiography, Topography and Geology
3: PHYSIOGRAPHY, TOPOGRAPHY AND GEOLOGY A. Physiography New Jersey can be divided into four regions, known as physiographic provinces, which are areas with similar sequences of rock types, geologic structures and a common geologic history (see Figure 3a). The northwestern section of New Jersey is part of the Valley and Ridge Province, which is characterized by long, parallel ridges and valleys formed by folded and faulted limestones, shales and sandstones of early and middle Paleozoic age. Erosion-resistant sandstone and siltstone bedrock lie beneath the ridges of the Appalachian Mountains while shale and limestone underlie the valleys. Bordering the Valley and Ridge Province to the southeast, the Highlands Province consists of metamorphic rocks of Precambrian age. The granites and gneisses are resistant to erosion and create a hilly upland with deep, steep-sided valleys carved by streams. These folds are seen in the northern half of Holland Township (see Figure 3a). The Highlands Province is separated from the Piedmont Province by a series of major faults which cross Holland Township and reach the Delaware River near Church Road (see Figure 3a). The Piedmont Province is characterized by gently rolling hills. The rocks of the Piedmont are of Late Triassic and Early Jurassic age. As sediments eroded from adjacent uplands, and were deposited along rivers and lakes within the basin, they became compacted and cemented to form conglomerate, sandstone, siltstone and shale. Diabase is a rock formed by the cooling of magma at some depth in the crust (i.e. the magma did not erupt at the surface), while basalt formed when the magma was extruded onto the surface.