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Bedrock Geologic Map of the Monmouth Junction Quadrangle, Water Resources Management U.S
DEPARTMENT OF ENVIRONMENTAL PROTECTION Prepared in cooperation with the BEDROCK GEOLOGIC MAP OF THE MONMOUTH JUNCTION QUADRANGLE, WATER RESOURCES MANAGEMENT U.S. GEOLOGICAL SURVEY SOMERSET, MIDDLESEX, AND MERCER COUNTIES, NEW JERSEY NEW JERSEY GEOLOGICAL AND WATER SURVEY NATIONAL GEOLOGIC MAPPING PROGRAM GEOLOGICAL MAP SERIES GMS 18-4 Cedar EXPLANATION OF MAP SYMBOLS cycle; lake level rises creating a stable deep lake environment followed by a fall in water level leading to complete Cardozo, N., and Allmendinger, R. W., 2013, Spherical projections with OSXStereonet: Computers & Geosciences, v. 51, p. 193 - 205, doi: 74°37'30" 35' Hill Cem 32'30" 74°30' 5 000m 5 5 desiccation of the lake. Within the Passaic Formation, organic-rick black and gray beds mark the deep lake 10.1016/j.cageo.2012.07.021. 32 E 33 34 535 536 537 538 539 540 541 490 000 FEET 542 40°30' 40°30' period, purple beds mark a shallower, slightly less organic-rich lake, and red beds mark a shallow oxygenated 6 Contacts 100 M Mettler lake in which most organic matter was oxidized. Olsen and others (1996) described the next longer cycle as the Christopher, R. A., 1979, Normapolles and triporate pollen assemblages from the Raritan and Magothy formations (Upper Cretaceous) of New 6 A 100 I 10 N Identity and existance certain, location accurate short modulating cycle, which is made up of five Van Houten cycles. The still longer in duration McLaughlin cycles Jersey: Palynology, v. 3, p. 73-121. S T 44 000m MWEL L RD 0 contain four short modulating cycles or 20 Van Houten cycles (figure 1). -
Lancaster County Geology
LancasterLancaster CountyCounty GeologyGeology gfgh µ OverOver TopographicTopographic ReliefRelief Om Miles Í897 0 10 hg Lebanon County Adamstown ¦¨§76 ! Berks County Oha ! Oo Denver ab322 Ephrata Csc Í501 ! Í72 TRh 272 TRn Oco Lititz Í ! Akron Elizabethtown Manheim ! Dauphin County! ! TRhc Cr TRs c Os Rn ! T Terre Hill TRg Trd 322 772 ab 10 Í 222 625 Í ab Í897 Í Í283 Ohm Í230 Oan Í241 East New Holland Oe 722 Petersburg Í Cbs ! Mount Joy ! ! Czc Cch Í23 Cm gga fl R 743 T Í Csb gg pg ggd Í441 Ck Cl 772 72 Í 23 Í ! Í Ca Marietta Ch Lancaster Mountville ! 340 ! Í Columbia 30 ! ! ba Í462 Í462 ab30 Í999 Millersville Ccc Strasburg ! ! Cv Í741 Í741 Í272 41 Í County Chester 896 222 Í gn Christiana ba mg ! oct Cah Í372 S u sq u e h a n n a R iv e r Y o rk C o u n ty gqm LEGEND COUNTY BOUNDARIES Í324 Source: Lancaster County GIS, Copyright (c) 2019 MAJOR ROADS This map to be used for reference or illustrative purposes only. This map FAULT is not a legally recorded plan, survey, or engineering schematic Quarryville and it is not intended to be used as such. For complete disclaimer see: RIVERS AND STREAMS ! http://www.co.lancaster.pa.us/gisdisclaimer DIKE wc ORDOVICIAN Í472 Oan, ANNVILLE FORMATION LIMESTONE TRIASSIC 372 Oco, COCALICO FORMATION DARK GRAY SHALE TRfl, LIMESTONE FANGLOMERATE Í TRg, GETTYSBURG FORMATION SHALE-SANDSTONE Oe, EPLER FORMATION LIMESTONE TRh, HAMMER CREEK FORMATION SANDSTONE-SHALE Oha, ANNVILLE, HERSHEY, AND MYERSTOWN FORMATION TRhc, HAMMER CREEK QUARTZ-CONGLOMERATE Ohm, HERSHEY AND MYERSTOWN FORMATION LIMESTONE 272 TRn, NEW -
THE JOURNAL of GEOLOGY March 1990
VOLUME 98 NUMBER 2 THE JOURNAL OF GEOLOGY March 1990 QUANTITATIVE FILLING MODEL FOR CONTINENTAL EXTENSIONAL BASINS WITH APPLICATIONS TO EARLY MESOZOIC RIFTS OF EASTERN NORTH AMERICA' ROY W. SCHLISCHE AND PAUL E. OLSEN Department of Geological Sciences and Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York 10964 ABSTRACT In many half-graben, strata progressively onlap the hanging wall block of the basins, indicating that both the basins and their depositional surface areas were growing in size through time. Based on these con- straints, we have constructed a quantitative model for the stratigraphic evolution of extensional basins with the simplifying assumptions of constant volume input of sediments and water per unit time, as well as a uniform subsidence rate and a fixed outlet level. The model predicts (1) a transition from fluvial to lacustrine deposition, (2) systematically decreasing accumulation rates in lacustrine strata, and (3) a rapid increase in lake depth after the onset of lacustrine deposition, followed by a systematic decrease. When parameterized for the early Mesozoic basins of eastern North America, the model's predictions match trends observed in late Triassic-age rocks. Significant deviations from the model's predictions occur in Early Jurassic-age strata, in which markedly higher accumulation rates and greater lake depths point to an increased extension rate that led to increased asymmetry in these half-graben. The model makes it possible to extract from the sedimentary record those events in the history of an extensional basin that are due solely to the filling of a basin growing in size through time and those that are due to changes in tectonics, climate, or sediment and water budgets. -
Somerset County, New Jersey Geology
Natural and Cultural Resource Inventory & Guide Somerset County, New Jersey Geology 456659 456613 Peapack- Bernardsville ab206 456525 Gladstone Borough Borough 456661 456624 456512 456657 ab202 Far Hills Borough 456512 Bernards 456640 [^287 Township Bedminster Township 456622 456655 456523 NOTES 1. This map was prepared using GIS data produced & distributed 456531 456652 ¤£22 by the New Jersey Geological Survey. 456665 Watchung 2. Depiction of environmental features is for general information 456653 Borough purposes only, and shall not be construed to define the legal ¦¨§78 ¦¨§78 geographic jurisdiction associated with any statutes or rules. 456651 3. Somerset County uses the following map projection & coordinate system when presenting GIS data: 456620 - Horizontal: North American Datum 1983 (NAD83) ab206 - Vertical: North American Vertical Datum 1987 (NAVD87) [^287 - Coordinate System: New Jersey State Plane Feet ab202 456618 DATA SOURCES Warren Township NEW JERSEY GEOLOGICAL SURVEY 638 641 456 456 636 649 - Geological Formations 456529 456 456 - Fault Lines Bridgewater Township North Plainfield NEW JERSEY DEPARTMENT OF Green Brook Borough ENVIRONMENTAL PROTECTION (NJDEP) 456614 - Streams ¤£22 Township 456616 NEW JERSEY DEPARTMENT OF TRANSPORTATION (NJDOT) 456679 456651 - Major Roads 456634 SOMERSET COUNTY GIS ENTERPRISE 456673 - County Boundaries - Municipal Boundaries 456527 - Parcel Boundaries (!28 ¤£22 456525 Raritan 456644 456643 Branchburg Borough Somerville 456633 456626 Bound Brook Township (!28 Borough Borough 637 456635 456 -
Jahresbericht 2013
Staatliches Museum für Naturkunde Stuttgart Jahresbericht Sammeln Bewahren Forschen Vermitteln 13 Impressum Herausgeber Prof. Dr. Johanna Eder Direktorin Staatliches Museum für Naturkunde Stuttgart Rosenstein 1 70191 Stuttgart Redaktion M.Sc. Lena Kempener Staatliches Museum für Naturkunde Stuttgart Jahresbericht/Dokumentarische Ausgabe ISSN 2191-7817 Berichtsjahr 2013, erschienen 2014 Copyright Diese Zeitschrift ist urheberrechtlich geschützt. Eine Verwertung ist nur mit schriftlicher Genehmi- gung des Herausgebers gestattet. Bildnachweis Coverfotos: U.Schmid (o.l.), U. Stübler (o.r.), S. Leidenroth (u.l.), M. Wahler (u.r.) Inhaltsverzeichnis 2 INHALTSVERZEICHNIS EDITORIAL 4 1 FORSCHUNG 6 1.1 Forschungsprojekte 6 1.1.1 Drittmittel-finanziert 6 1.1.2 Nicht Drittmittel-finanziert 8 1.2 Umfangreiche Freilandarbeiten, Grabungen 13 1.3 Studienaufenthalte 14 1.4 Tagungsbeiträge 15 1.4.1 International 15 1.4.2 National 17 1.5 Sonstige wissenschaftliche Vorträge 18 1.6 Organisation von Tagungen und Workshops 19 1.7 Organisierte wissenschaftliche Exkursionen 19 1.8 Gastforscher 20 1.8.1 National 20 1.8.2 International 22 2 SAMMLUNG UND BIBLIOTHEK 24 2.1 Bedeutende Sammlungsarbeiten 24 2.1.1 Wissenschaftliche Arbeiten 24 2.1.2 Präparatorische und konservatorische Arbeiten 25 2.1.3 Elektronische Sammlungserfassung 28 2.2 Bedeutende Sammlungszugänge 28 2.3 Führungen hinter die Kulissen 29 2.4 Bibliothek und Archiv 30 3 BILDUNG UND ÖFFENTLICHKEITSARBEIT 30 3.1 Führungen und Projekte 30 3.1.1 Dauerausstellung 30 3.1.2 Sonderausstellung 31 3.1.3 Neues -
Evaluation of Groundwater Resources of Bernards Township, Somerset County, New Jersey
Evaluation of Groundwater Resources of Bernards Township, Somerset County, New Jersey M2 Associates Inc. 56 Country Acres Drive Hampton, New Jersey 08827 EVALUATION OF GROUNDWATER RESOURCES OF BERNARDS TOWNSHIP SOMERSET COUNTY, NEW JERSEY APRIL 11, 2008 Prepared for: Bernards Township 1 Collyer Lane Basking Ridge, NJ 07920 Prepared by: Matthew J. Mulhall, P.G. M2 Associates Inc. 56 Country Acres Drive Hampton, New Jersey 08827-4110 908-238-0827 Fax: 908-238-0830 EVALUATION OF GROUNDWATER RESOURCES OF BERNARDS TOWNSHIP SOMERSET COUNTY, NEW JERSEY TABLE OF CONTENTS INTRODUCTION............................................................................................................. 1 GEOLOGY ...................................................................................................................... 5 PHYSIOGRAPHIC PROVINCE ............................................................................................ 5 SURFACE WATER .......................................................................................................... 6 Watersheds............................................................................................................. 6 Stream Classifications........................................................................................... 7 Headwaters............................................................................................................. 9 SOILS ......................................................................................................................... 10 BEDROCK................................................................................................................... -
Progress in the Gondwanan Carboniferous–Permian Palynology and Correlation of the Nilawahan Group of the Salt Range, Pakistan: a Brief Review
Progress in the Gondwanan Carboniferous–Permian palynology and correlation of the Nilawahan Group of the Salt Range, Pakistan: A brief review Irfan U Jan National Centre of Excellence in Geology, University of Peshawar, Peshawar, Pakistan. e-mail: irfan [email protected] This paper comprises of two sections. The first section describes challenges in the Carboniferous–Permian Gondwanan stratigraphic palynology, and progress in techniques such as presence of the ‘rare-marine intervals’, and ‘radiometric dating’ in some Gondwanan successions, e.g., South Africa, Australia and South America, as tools to confidently calibrate these palynozones. The second section describes devel- opments in the palynological work on the Carboniferous–Permian Nilawahan Group of the Salt Range, Pakistan, and summarises their correlation with the coeval succession of the Gondwana continents and with the Russian/International stages. 1. Introduction hydrocarbon-reserves and also bear remarkable traces of the advance and retreat of the ice from The Salt Range occupies a crucial position in the around the South Polar regions. However, the Salt geological history of Pakistan both in time and Range succession have received limited attention, space. In the time, because the late Palaeozoic although in this tectonic jigsaw puzzle, it repre- stratigraphy of the area represents the end of the sents a place near the very margin of the vast greatest glaciation of the Phanerozoic earth sys- glaciated region (Jan et al., in review). tem, the Carboniferous–Permian, and in space, Previously, some palynological taxonomic work because during that time it lay next to the land- was undertaken on the Salt Range units and mass now represented by Oman, Saudi Arabia attempts were made to understand their strati- and Yemen (Jan 2012; Stephenson et al. -
PSEG POWER, LLC (Site Safety Analysis Report), Rev. 0
Series Stratigraphic Unit Predominant Lithology Era System Holocene alluvial, coastal, marsh, and eolian deposits sand, gravel, silt, mud, and peat COASTAL AREAS INLAND, NORTHERN NEW JERSEY Wisconsin alluvium, Cape Wisconsin and pre- sand, gravel, silt, clay (statewide), till and till-like Pleistocene May Formation, colluvium Wisconsin alluvial, colluvial, glacial, lacustrine, and eolian deposits (northern New Jersey) Quaternary deposits Pensauken Formation sand, clayey silt Bridgeton Formation Beacon Hill Gravel gravel, sand Cohansey Sand sand, some clayey silt Miocene Kirkwood Formation sand, gravel, clayey silt CENOZOIC Tertiary ACGS Beta Unit (Piney Point) Oligocene sand, some glauconitic sand Mays Landing Unit Shark River Formation Eocene clayey silt, fine quartz sand, glauconitic sand Manasquan Formation Vincentown Formation sand, clayey silt, glauconitic sand, calcarenite Paleocene Hornerstown Formation glauconitic sand Tinton Sand sand, glauconitic sand Red Bank Sand sand, clayey silt, some glauconite sand Navesink Formation glauconite sand Mount Laurel Sand sand Wenonah Formation silty sand, some glauconite Marshalltown Formation clayey silt, glauconitic sand Upper Englishtown Formation sand, clayey silt Cretaceous Woodbury Clay clayey silt Merchantville Formation clayey silt, glauconitic sand Cretaceous Magothy Formation sand, clayey silt Raritan Formation Lower Potomac Group gravel, sand, silt, clay MESOZOIC Cretaceous Boonton Formation sandstone, siltstone, shale, conglomerate Hook Mountain Basalt basalt Lower Towaco Formation -
Petrofacies and Paleotectonic Evolution of Permo-Carboniferous Gondwanan Sequences of the Bengal Basin, Bangladesh
Petrofacies and Paleotectonic Evolution of Permo-Carboniferous Gondwanan Sequences of the Bengal Basin, Bangladesh by Md. Iftekhar Alam A thesis submitted to the Graduate Faculty of Auburn University in partial fulfillment of the requirements for the Degree of Master of Science Auburn, Alabama December 12, 2011 Keywords: Gondwanaland, Petrofacies, Paleotectonic, Permo-Carboniferous, Bangladesh Copyright 2011 by Md. Iftekhar Alam Approved by Ashraf Uddin, Chair, Professor of Geology Charles E. Savrda, Professor of Geology David T. King, Jr., Professor of Geology Willis E. Hames, Professor of Geology Abstract The Indian subcontinent, along with Australia and Antarctica, constituted Eastern Gondwananland. Permo-Carboniferous Gondwanan sequences have been reported from several isolated basins of the Peninsular India. These siliciclastic sequences were drilled in intra-cratonic basins in northwest Bengal Basin. This ~1-km-thick sequence consists primarily of massive and trough cross-bedded sandstones and laminated mudstones, with localized conglomerate and coal layers. Sandstone petrography, heavy mineral assemblage studies, heavy mineral geochemistry, and detrital geochronology were used in this study to decipher provenance history of Gondwanan sediments at two localities (Khalashpir and Barapukuria) from the Bengal Basin of Bangladesh. Petrographic studies suggest that these sequences are mostly immature and poorly sorted arkosic sandstones (Khalashpir-Qt58F30L12, Barapukuria-Qt52F31L17), with some compositions ranging from quartzarenite to litharenite. Although monocrystalline quartz is dominant, considerable polycrystalline quartz fragments have also been found. K-feldspars dominate over plagioclase feldspars. Among lithic fragments, sedimentary types are abundant. Significant amounts of chert are observed. Heavy minerals are volumetrically rare and of low diversity in sediments of northwest Bangladesh. However, samples from Khalashpir have higher heavy mineral concentrations than ii those from Barapukuria. -
78. Paleosol Caliche in the New Haven Arkose, Nweark Group, Connecticut
(This is a sample cover image for this issue. The actual cover is not yet available at this time.) This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Earth and Planetary Science Letters 323-324 (2012) 27–39 Contents lists available at SciVerse ScienceDirect Earth and Planetary Science Letters journal homepage: www.elsevier.com/locate/epsl Rapid emplacement of the Central Atlantic Magmatic Province as a net sink for CO2 Morgan F. Schaller a,⁎, James D. Wright a, Dennis V. Kent a,b, Paul E. Olsen b a Earth and Planetary Sciences, Rutgers University, 610 Taylor Rd. Piscataway, NJ 08854, USA b Lamont–Doherty Earth Observatory of Columbia University, Rt. 9W, Palisades, NY 10964, USA article info abstract Article history: Recent evidence from the ~201.5 Ma Central Atlantic Magmatic Province (CAMP) in the Newark rift basin demon- Received 8 June 2011 strates that this Large Igneous Province produced a transient doubling of atmospheric pCO2, followed by a falloff to Received in revised form 21 October 2011 pre-eruptive concentrations over ~300 kyr. -
Magnetic Records from Latest Triassic to Earliest Jurassic Red Beds, Utah and Arizona, and from Mid- Pleistocene Lake Beds, New Mexico Linda Lee Donohoo Hurley
University of New Mexico UNM Digital Repository Earth and Planetary Sciences ETDs Electronic Theses and Dissertations 2-1-2012 Magnetic records from latest Triassic to earliest Jurassic red beds, Utah and Arizona, and from mid- Pleistocene lake beds, New Mexico Linda Lee Donohoo Hurley Follow this and additional works at: https://digitalrepository.unm.edu/eps_etds Recommended Citation Hurley, Linda Lee Donohoo. "Magnetic records from latest Triassic to earliest Jurassic red beds, Utah and Arizona, and from mid- Pleistocene lake beds, New Mexico." (2012). https://digitalrepository.unm.edu/eps_etds/38 This Dissertation is brought to you for free and open access by the Electronic Theses and Dissertations at UNM Digital Repository. It has been accepted for inclusion in Earth and Planetary Sciences ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. Linda L. Donohoo-Hurley Candidate Department of Earth and Planetary Sciences Department This dissertation is approved, and it is acceptable in quality and form for publication: Approved by the Dissertation Committee: Dr. John W. Geissman , Chairperson Dr. Peter J. Fawcett Dr. Mousumi Roy Dr. Tim F. Wawrzyniec Dr. Spencer G. Lucas Dr. Fraser Goff i MAGNETIC RECORDS FROM LATEST TRIASSIC TO EARLIEST JURASSIC RED BEDS, UTAH AND ARIZONA, AND FROM MID-PLEISTOCENE LAKE BEDS, NEW MEXICO by LINDA L. DONOHOO-HURLEY B.A., Geology, Occidental College, 2000 M.S., Western Washington University, 2004 DISSERTATION Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy Earth and Planetary Sciences The University of New Mexico Albuquerque, New Mexico December, 2011 ii Dedication This dissertation is dedicated to my daughter, Kaleigh, husband John, brother Al and mother Juana. -
Basin-Centered Gas Systems of the U.S. by Marin A
Basin-Centered Gas Systems of the U.S. By Marin A. Popov,1 Vito F. Nuccio,2 Thaddeus S. Dyman,2 Timothy A. Gognat,1 Ronald C. Johnson,2 James W. Schmoker,2 Michael S. Wilson,1 and Charles Bartberger1 Columbia Basin Western Washington Sweetgrass Arch (Willamette–Puget Mid-Continent Rift Michigan Basin Sound Trough) (St. Peter Ss) Appalachian Basin (Clinton–Medina Snake River and older Fms) Hornbrook Basin Downwarp Wasatch Plateau –Modoc Plateau San Rafael Swell (Dakota Fm) Sacramento Basin Hanna Basin Great Denver Basin Basin Santa Maria Basin (Monterey Fm) Raton Basin Arkoma Park Anadarko Los Angeles Basin Chuar Basin Basin Group Basins Black Warrior Basin Colville Basin Salton Mesozoic Rift Trough Permian Basin Basins (Abo Fm) Paradox Basin (Cane Creek interval) Central Alaska Rio Grande Rift Basins (Albuquerque Basin) Gulf Coast– Travis Peak Fm– Gulf Coast– Cotton Valley Grp Austin Chalk; Eagle Fm Cook Inlet Open-File Report 01–135 Version 1.0 2001 This report is preliminary, has not been reviewed for conformity with U. S. Geological Survey editorial standards and stratigraphic nomenclature, and should not be reproduced or distributed. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U. S. Government. 1Geologic consultants on contract to the USGS 2USGS, Denver U.S. Department of the Interior U.S. Geological Survey BASIN-CENTERED GAS SYSTEMS OF THE U.S. DE-AT26-98FT40031 U.S. Department of Energy, National Energy Technology Laboratory Contractor: U.S. Geological Survey Central Region Energy Team DOE Project Chief: Bill Gwilliam USGS Project Chief: V.F.