DOCSLIB.ORG

Hydrogeology and Ground-Water Flow

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Hydrogeology and Ground-Water Flow HYDROGEOLOGY AND GROUND-WATER FLOW, FRACTURED MESOZOIC STRUCTURAL-BASIN ROCKS, STONY BROOK, BEDEN BROOK, AND JACOBS CREEK DRAINAGE BASINS, WEST-CENTRAL NEW JERSEY by Jean C. Lewis-Brown and Eric Jacobsen U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 94-4147 APPALACHIAN VALLEYS-PIEDMONT REGIONAL AQUIFER-SYSTEMS ANALYSIS Wsst Trenton, New Jersey 1995 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary US. GEOLOGICAL SURVEY Gordon P. Eaton, Director For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey, WRD Earth Science Information Center 810 Bear Tavern Road Open-File Reports Section West Trenton, NJ 08628 Box 25286, MS 517 Denver Federal Center Denver, CO 80225 CONTENTS Page Abstract..........................................^ Introduction.......................................~^ Purpose and scope...................................................................................................................................... 2 Description of study area........................................................................................................................... 6 Location and extent...................................................................................................................... 6 Geologic setting............................................................................................................................ 6 Previous investigations............................................................................................................................10 Hydrogeology.......................................................................................................................................................... 10 Hydrogeologic framework.......................................................................................................................11 Hydraulic properties of aquifers............................................................................................................ 13 Spedfic capacity.......................................................................................................................... 15 Effect of lithology......................................................................................................... 15 Effect of depth............................................................................................................... 18 Transmissivity............................................................................................................................. 18 Storage coefficient....................................................................................................................... 18 Porosity........................................................................................................................................ 18 Ground-water flow.................................................................................................................................................20 Conceptual model of ground-water flow.............................................................................................. 20 Recharge and discharge areas................................................................................................... 23 Anisotropy of sedimentary aquifers........................................................................................ 24 Effect of diabase rocks................................................................................................................ 24 Source of water to wells............................................................................................................. 27 Simulation of ground-water flow........................................................................................................... 27 Description of digital model..................................................................................................... 27 Grid orientation and discretization........................................................................... 27 Boundary conditions................................................................................................... 29 Upper boundary and simulation of surface water................................... 29 Lateral boundaries......................................................................................... 31 Lower boundary............................................................................................32 Calibration of digital model...................................................................................................... 32 Water levels...................................................................................................................32 U.S. Geological Survey water-level data.................................................... 38 Well-completion-record data....................................................................... 39 Base flow....................................................................................................................... 40 Limitations of digital model..................................................................................................... 40 Prepumping water budgets..................................................................................................................... 41 Base flow and direct runoff .......................................................................................................41 Initial estimates ............................................................................................................41 Stony Brook drainage basin......................................................................... 41 Beden Brook and Jacobs Creek drainage basins .......................................44 Effect of anisotropy......................................................................................................44 Base-flow rates in the digital model.......................................................................... 45 Ground-water pumpage............................................................................................................45 Ground-water flow to and from adjoining drainage basins................................................48 Areal recharge............................................................................................................................. 49 Initial estimates............................................................................................................49 Effect of diabase rocks................................................................................................. 51 Effect of Hopewell Fault............................................................................................. 53 Areal recharge rates in the digital model................................................................. 53 CONTENTS-Continued Page Values of hydraulic conductivity and conductance from calibrated digital model........................ 53 Horizontal hydraulic conductivity in the direction of strike............................................... 55 Diabase rocks................................................................................................................55 Stockton Formation...................................................................................................... 55 Lockatong Formation..................................................................................................56 Passaic Formation........................................................................................................56 Fault zone...................................................................................................................... 56 Areas near streams.......................................................................................................56 Horizontal anisotropy ratio......................................................................................................57 Vertical hydraulic conductance................................................................................................ 57 Streambed hydraulic conductance...........................................................................................58 Vertical distribution of ground-water flow........................................................................................... 59 Summary and conclusions.....................................................................................................................................59 References cited.......................................................................................................................................................62 ILLUSTRATIONS Figures 1-4. Maps showing: 1. The Appalachian Valleys-Piedmont Regional Aquifer-Systems Analysis study area and physiographic provinces............................................................................. 3 2. Exposed Mesozoic basins in the eastern United States................................................... 4 3. Location of the study area.................................................................................................... 5 4. Geology of the study area, Stony Brook, Beden Brook, and Jacobs Creek drainage basins, west-central New Jersey................................................................................. 8 5. Generalized geologic section through the study area, Stony Brook, Beden Brook, and
Load more

Recommended publications
  • Montgomery Township N.R.I. Appendix – Nitrate Dilution
    Nitrate Dilution Modeling of Montgomery Township, Somerset County, NJ Prepared for: Montgomery Township Environmental Commission Somerset County, NJ 2261 Route 206 Belle Mead, NJ 08502 Prepared by: The GIS Center Stony Brook-Millstone Watershed Association 31 Titus Mill Road Pennington, NJ 08534 April 8, 2004 Introduction Nitrate from natural sources generally only occurs in ground water at low levels but anthropogenic sources can lead to elevated concentrations. Sources include fertilizers, animal waste, and sewage effluent. Nitrate is considered a contaminant in ground water because of various impacts to human health and aquatic ecology. For instance, high levels of nitrate intake in infants can lead to methemoglobinemia, or blue baby syndrome (Hem, 1985; U.S. EPA, 1991). Because of its low natural occurrence and solubility and stability in groundwater, nitrate can also serve as an indicator for possible bacterial, viral, or chemical contaminants of anthropogenic origin. Nitrogen is present in septic system effluent and is converted to nitrate through biological processes active in the soil below the drain field. Once this nitrification process is complete, nitrate is a stable and mobile compound in ground water under normal conditions (Hoffman and Canace, 2001). Nitrate concentrations resulting from septic effluent are mitigated by dilution if the septic effluent is combined over time with water entering the ground through infiltration during and after storm events. The extent of this dilution effect is clearly dependent on long-term rates of both infiltration and nitrate loading from septic system sources. The density of septic systems relative to infiltration rates in a particular area is therefore a critical factor controlling the ultimate nitrate level in ground water.
    [Show full text]
  • Triassic- Jurassic Stratigraphy Of
    Triassic- Jurassic Stratigraphy of the <JF C7 JL / Culpfeper and B arbour sville Basins, VirginiaC7 and Maryland/ ll.S. PAPER Triassic-Jurassic Stratigraphy of the Culpeper and Barboursville Basins, Virginia and Maryland By K.Y. LEE and AJ. FROELICH U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1472 A clarification of the Triassic--Jurassic stratigraphic sequences, sedimentation, and depositional environments UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1989 DEPARTMENT OF THE INTERIOR MANUEL LUJAN, Jr., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging in Publication Data Lee, K.Y. Triassic-Jurassic stratigraphy of the Culpeper and Barboursville basins, Virginia and Maryland. (U.S. Geological Survey professional paper ; 1472) Bibliography: p. Supt. of Docs. no. : I 19.16:1472 1. Geology, Stratigraphic Triassic. 2. Geology, Stratigraphic Jurassic. 3. Geology Culpeper Basin (Va. and Md.) 4. Geology Virginia Barboursville Basin. I. Froelich, A.J. (Albert Joseph), 1929- II. Title. III. Series. QE676.L44 1989 551.7'62'09755 87-600318 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 CONTENTS Page Page Abstract.......................................................................................................... 1 Stratigraphy Continued Introduction... ..........................................................................................
    [Show full text]
  • Hydrogeology and Ground-Water Quality of Northern Bucks County, Pennsylvania
    HYDROGEOLOGY AND GROUND-WATER QUALITY OF NORTHERN BUCKS COUNTY, PENNSYLVANIA by Ronald A. Sloto and Curtis L Schreftier ' U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 94-4109 Prepared in cooperation with NEW HOPE BOROUGH AND BRIDGETON, BUCKINGHAM, NOCKAMIXON, PLUMSTEAD, SOLEBURY, SPRINGFIELD, TINICUM, AND WRIGHTSTOWN TOWNSHIPS Lemoyne, Pennsylvania 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For additional information Copies of this report may be write to: purchased from: U.S. Geological Survey Earth Science Information Center District Chief Open-File Reports Section U.S. Geological Survey Box 25286, MS 517 840 Market Street Denver Federal Center Lemoyne, Pennsylvania 17043-1586 Denver, Colorado 80225 CONTENTS Page Abstract....................................................................................1 Introduction ................................................................................2 Purpose and scope ..................................................................... 2 Location and physiography ............................................................. 2 Climate...............................................................................3 Well-numbering system................................................................. 4 Borehole geophysical logging............................................................4 Previous investigations ................................................................. 6 Acknowledgments....................................................................
    [Show full text]
  • 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).
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • A Dinosaur Track from New Jersey at the State Museum in Trenton
    New Jersey Geological and Water Survey Information Circular What's in a Rock? A Dinosaur Track from New Jersey at the State Museum in Trenton Introduction a large dinosaur track (fig. 2) on the bottom. Most of the rock is sedimentary, sandstone from the 15,000-foot-thick Passaic A large, red rock in front of the New Jersey State Museum Formation. The bottom part is igneous, lava from the 525-foot- (NJSM) in Trenton (fig. 1) is more than just a rock. It has a thick Orange Mountain Basalt, which overspread the Passaic fascinating geological history. This three-ton slab, was excavated Formation. (The overspreading lava was originally at the top of from a construction site in Woodland Park, Passaic County. It the rock, but the rock is displayed upside down to showcase the was brought to Trenton in 2010 and placed upside down to show dinosaur footprint). The rock is about 200 million years old, from the Triassic footprints Period of geologic time. It formed in a rift valley, the Newark Passaic Formation Basin, when Africa, positioned adjacent to the mid-Atlantic states, began to pull eastward and North America began to pull westward contact to open the Atlantic Ocean. The pulling and stretching caused faults to move and the rift valley to subside along border faults including the Ramapo Fault of northeastern New Jersey, about 8 miles west of Woodland Park. Sediments from erosion of higher Collection site Orange Mountain Basalt top N Figure 1. Rock at the New Jersey State Museum. Photo by W. Kuehne Adhesion ripples DESCRIPTION OF MAP UNITS 0 1 2 mi Orange Mountain Basalt L 32 cm Jo (Lower Jurassic) 0 1 2 km W 25.4 cm contour interval 20 feet ^p Passaic Formation (Upper Triassic) Figure 3.
    [Show full text]
  • 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
    [Show full text]
  • ' Or ''Long'' Rhaetian? Astronomical Calibration of Austrian Key Sections
    ”Short” or ”long” Rhaetian ? Astronomical calibration of Austrian key sections Bruno Galbrun, Slah Boulila, Leopold Krystyn, Sylvain Richoz, Silvia Gardin, Annachiara Bartolini, Martin Maslo To cite this version: Bruno Galbrun, Slah Boulila, Leopold Krystyn, Sylvain Richoz, Silvia Gardin, et al.. ”Short” or ”long” Rhaetian ? Astronomical calibration of Austrian key sections. Global and Planetary Change, Elsevier, 2020, 192, pp.103253. 10.1016/j.gloplacha.2020.103253. hal-02884087 HAL Id: hal-02884087 https://hal.archives-ouvertes.fr/hal-02884087 Submitted on 29 Jun 2020 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. Galbrun B., Boulila S., Krystyn L., Richoz S., Gardin S., Bartolini A., Maslo M. (2020). « Short » or « long » Rhaetian ? Astronomical calibration of Austrian key sections. Global Planetary Change. Vol. 192C. https://doi.org/10.1016/j.gloplacha.2020.103253 « Short » or « long » Rhaetian ? Astronomical calibration of Austrian key sections Bruno Galbruna,*, Slah Boulilaa, Leopold Krystynb, Sylvain Richozc,d, Silvia Gardine, Annachiara
    [Show full text]
  • Brunswick Group and Lockatong Formation, Pennsylvania
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 2000 Fractured-Aquifer Hydrogeology from Geophysical Logs: Brunswick Group and Lockatong Formation, Pennsylvania Roger H. Morin Denver Federal Center, [email protected] Lisa A. Senior U.S. Geological Survey, Malvern Edward R. Decker University of Maine Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Earth Sciences Commons Morin, Roger H.; Senior, Lisa A.; and Decker, Edward R., "Fractured-Aquifer Hydrogeology from Geophysical Logs: Brunswick Group and Lockatong Formation, Pennsylvania" (2000). USGS Staff -- Published Research. 352. https://digitalcommons.unl.edu/usgsstaffpub/352 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Fractured-Aquifer Hydrogeology from Geophysical Logs: Brunswick Group and Lockatong Formation, Pennsylvania 3 b c by Roger H. Morin , Lisa A. Senior , and Edward R. Decker Abstract The Brunswick Group and the underlying Lockatong Formation are composed of lithified Mesozoic sediments that consti­ tute part of the Newark Basin in southeastern Pennsylvania. These fractured rocks form an important regional aquifer that con­ sists of gradational sequences of shale, siltstone, and sandstone, with fluid transport occurring primarily in fractures. An exten­ sive suite of geophysical logs was obtained in seven wells located at the borough of Lansdale, Pennsylvania, in order to better characterize the areal hydrogeologic system and provide guidelines for the refinement of numerical ground water models.
    [Show full text]
  • Term Behaviour of the Planets − Scale and the Long
    Downloaded from rsta.royalsocietypublishing.org on January 19, 2012 Long-period Milankovitch cycles from the Late Triassic and Early Jurassic of eastern North America and their implications for the calibration of the Early Mesozoic time−scale and the long −term behaviour of the planets Paul E. Olsen and Dennis V. Kent Phil. Trans. R. Soc. Lond. A 1999 357, 1761-1786 doi: 10.1098/rsta.1999.0400 Receive free email alerts when new articles cite this article - sign up in the box at the top right-hand Email alerting service corner of the article or click here To subscribe to Phil. Trans. R. Soc. Lond. A go to: http://rsta.royalsocietypublishing.org/subscriptions Downloaded from rsta.royalsocietypublishing.org on January 19, 2012 Long-period Milankovitch cycles from the Late Triassic and Early Jurassic of eastern North America and their implications for the calibration of the Early Mesozoic time-scale and the long-term behaviour of the planets By Paul E. Olsen1 and Dennis V. Kent2 1Lamont-Doherty Earth Observatory of Columbia University, Rt 9W, Palisades, NY 10964, USA ([email protected]) 2Department of Geological Sciences, Rutgers University, Piscataway, NJ 08854, USA and Lamont-Doherty Earth Observatory of Columbia University, Rt 9W, Palisades, NY 10964, USA ([email protected]) During the Late Triassic and Early Jurassic, the Newark rift basin of the northeastern US accumulated in excess of 5 km of continental, mostly lacustrine, strata that show a profound cyclicity caused by the astronomical forcing of tropical climate. The Newark record is known virtually in its entirety as a result of scientific and other coring and provides what is arguably one of the longest records of climate cyclicity available.
    [Show full text]
  • 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
    [Show full text]