Characterising Pre-Vegetation Paralic Sedimentary Systems and Developing Improved Architectural Reservoir Models

Total Page:16

File Type:pdf, Size:1020Kb

Characterising Pre-Vegetation Paralic Sedimentary Systems and Developing Improved Architectural Reservoir Models Characterising pre-vegetation paralic sedimentary systems and developing improved architectural reservoir models A thesis submitted to the University of Manchester for the degree of Doctor of Philosophy in the Faculty of Science and Engineering 2019 Ginny-Marie Bradley University of Manchester Faculty of Science and Engineering School of Earth and Environmental Sciences Basin Studies and Petroleum Geoscience/Engineering Funded by NERC CDT in Oil and Gas Table of Contents List of figures ..................................................................................................................... 5 List of tables ...................................................................................................................... 8 List of abbreviations .......................................................................................................... 9 Abstract ........................................................................................................................... 10 Declaration ...................................................................................................................... 12 Copyright statement ....................................................................................................... 13 Acknowledgements......................................................................................................... 14 Status of papers .............................................................................................................. 15 Chapter 1: Introduction .................................................................................................. 17 1.1 Aims of the thesis .................................................................................................. 18 1.2 Rationale................................................................................................................ 18 1.3 The Tumblagooda Sandstone................................................................................ 21 1.4 The advancement to pre-vegetation paralic studies ............................................ 21 1.5 Key aims of the project ......................................................................................... 22 1.6 Thesis structure ..................................................................................................... 22 1.7 Architectural Definition ......................................................................................... 24 Chapter 2: Previous Work ............................................................................................... 26 2.0 Introduction to braided fluvial systems. ............................................................... 27 2.1 Pre-vegetation fluvial systems .............................................................................. 29 2.2 Pre-vegetation tidal systems ................................................................................. 33 2.3 Impact of vegetation ............................................................................................. 34 2.4 Fluvio-paralic stratigraphy..................................................................................... 37 2.5 The Tumblagooda Sandstone................................................................................ 40 2.5.1 Geological history ........................................................................................... 40 2.5.2 Tumblagooda Sandstone ................................................................................ 41 2.5.3 Previous interpretations ................................................................................. 45 2.5.4 Fauna .............................................................................................................. 50 Chapter 3: Dataset and methodology............................................................................. 53 3.0 Introduction........................................................................................................... 54 3.1 Fieldwork ............................................................................................................... 54 3.1.1 Logging ............................................................................................................ 54 3.1.2 Sampling ......................................................................................................... 56 3.1.3 Photogrammetry............................................................................................. 59 3.2 Data processing and analysis ................................................................................ 62 3.2.1 Facies Analysis ................................................................................................ 62 3.2.2 Petrography .................................................................................................... 62 3.2.3 Digital outcrop modelling ............................................................................... 65 3.2.4 Annotating models and obtaining channel size statistics .............................. 66 3.2.5 Stochastic modelling ....................................................................................... 67 3.3 Limitations ............................................................................................................. 69 Chapter 4: The applicability of modern tidal analogues to pre-land plant paralic depositional models........................................................................................................ 72 Abstract ....................................................................................................................... 74 4.1 Introduction........................................................................................................... 75 4.2 Geological setting .................................................................................................. 77 2 4.3 Previous work ........................................................................................................ 79 4.3.1 A mixed marine to non-marine interpretation ............................................... 79 4.3.2 Non-marine interpretation ............................................................................. 80 4.4 Methodology ......................................................................................................... 81 4.5 Lithofacies descriptions ......................................................................................... 82 4.6 Facies associations................................................................................................. 98 4.6.1 Facies Association 1 ........................................................................................ 98 4.6.2 Facies Association 2 ........................................................................................ 99 4.7 Depositional system ............................................................................................ 101 4.7.1 Fluvial braidplain ........................................................................................... 101 4.7.2 Tidal dominance ............................................................................................ 102 4.7.3 Intertidal sandflat.......................................................................................... 103 4.7.4 Intertidal sand-bar to shallow subtidal ......................................................... 105 4.7.5 Stacking patterns .......................................................................................... 105 4.8 Discussion ............................................................................................................ 106 4.8.1 Interpretation of the depositional system.................................................... 106 4.8.2 Significance of Heimdallia assemblages ....................................................... 107 4.8.3 Early Palaeozoic depositional controls in a pre-plant world ........................ 108 4.8.4 Application of modern analogues................................................................. 116 4.9 Conclusions .......................................................................................................... 117 Chapter 5: Reassessing the sedimentology and architecture of pre-vegetation fluvial successions using large digital outcrop models. ........................................................... 120 Abstract ..................................................................................................................... 122 5.1 Introduction ......................................................................................................... 123 5.2 Background .......................................................................................................... 124 5.3 Geological Setting ................................................................................................ 128 5.4 Methods............................................................................................................... 129 5.5 Results ................................................................................................................. 132 5.5.1 Lithofacies ..................................................................................................... 132 5.5.2 Facies associations (FA)................................................................................. 146 5.5.3 Architectural elements ................................................................................. 151 5.5.4 Sequence
Recommended publications
  • Holocene Progradation and Retrogradation of the Central Texas Coast Regulated by Alongshore and Cross-Shore Sediment Flux Variability
    Received: 4 May 2020 | Revised: 8 October 2020 | Accepted: 15 October 2020 DOI: 10.1002/dep2.130 ORIGINAL RESEARCH ARTICLE Holocene progradation and retrogradation of the Central Texas Coast regulated by alongshore and cross-shore sediment flux variability Christopher I. Odezulu1 | Travis Swanson2 | John B. Anderson1 1Department of Earth, Environmental and Planetary Science, Rice University, Abstract Houston, TX, USA Fifteen transects of sediment cores located off the central Texas coast between 2Department of Geology and Geography, Matagorda Peninsula and North Padre Island were investigated to examine the off- Georgia Southern University, Statesboro, shore record of Holocene evolution of the central Texas coast. The transects extend GA, USA from near the modern shoreline to beyond the toe of the shoreface. Lithology, grain *Correspondence size and fossil content were used to identify upper shoreface, lower shoreface, ebb- Christopher I. Odezulu, Department tidal delta and marine mud lithofacies. Interpretations of these core transects show of Earth, Environmental and Planetary Science, Rice University, Houston, TX, a general stratigraphic pattern across the study area that indicates three major epi- USA. sodes of shoreface displacement. First, there was an episode of shoreface prograda- Email: [email protected] tion that extended up to 5 km seaward. Second, an episode of landward shoreline Funding information displacement is indicated by 3–4 km of marine mud onlap. Third, the marine muds Rice University Shell Center for Sustainability. are overlain by shoreface sands, which indicates another episode of shoreface pro- gradation of up to 5 km seaward. Radiocarbon ages constrain the onset of the first episode of progradation to ca 6.5 ka, ending at ca 5.0 ka when the rate of sea-level rise slowed from an average rate of 1.6–0.5 mm/yr.
    [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]
  • Resilience of River Deltas in the Anthropocene
    manuscript submitted to JGR: Earth Surface 1 Resilience of river deltas in the Anthropocene 1 2 3 4 2 A.J.F. Hoitink , J.A. Nittrouer , P. Passalacqua , J.B. Shaw , E.J. 5 6 6 3 Langendoen , Y. Huismans & D.S. van Maren 1 4 Wageningen University & Research, Wageningen, The Netherlands 2 5 Rice University, Houston, Texas USA 3 6 University of Texas at Austin, Austin, Texas USA 4 7 Department of Geosciences, University of Arkansas, Fayetteville, Arkansas USA 5 8 National Sedimentation Laboratory, United States Department of Agriculture, Oxford, Mississippi USA 6 9 Deltares, Delft, The Netherlands 10 Key Points: 11 • The predictive capacity of morphodynamic models needs to improve to better an- 12 ticipate global change impacts on deltas 13 • Information theory and dynamical system theory offer complementary analysis frame- 14 works to improve understanding of delta resilience 15 • The sediment balance in a delta channel network needs to be closed such that pre- 16 dictions match with independent observations Corresponding author: Ton Hoitink, [email protected] {1{ manuscript submitted to JGR: Earth Surface 17 Abstract 18 At a global scale, delta morphologies are subject to rapid change as a result of direct and 19 indirect effects of human activity. This jeopardizes the ecosystem services of deltas, in- 20 cluding protection against flood hazards, facilitation of navigation and biodiversity. Di- 21 rect manifestations of delta morphological instability include river bank failure, which 22 may lead to avulsion, persistent channel incision or aggregation, and a change of the sed- 23 imentary regime to hyperturbid conditions. Notwithstanding the in-depth knowledge de- 24 veloped over the past decades about those topics, existing understanding is fragmented, 25 and the predictive capacity of morphodynamic models is limited.
    [Show full text]
  • The Stratigraphic Architecture and Evolution of the Burdigalian Carbonate—Siliciclastic Sedimentary Systems of the Mut Basin, Turkey
    The stratigraphic architecture and evolution of the Burdigalian carbonate—siliciclastic sedimentary systems of the Mut Basin, Turkey P. Bassanta,*, F.S.P. Van Buchema, A. Strasserb,N.Gfru¨rc aInstitut Franc¸ais du Pe´trole, Rueil-Malmaison, France bUniversity of Fribourg, Switzerland cIstanbul Technical University, Istanbul, Turkey Received 17 February 2003; received in revised form 18 November 2003; accepted 21 January 2004 Abstract This study describes the coeval development of the depositional environments in three areas across the Mut Basin (Southern Turkey) throughout the Late Burdigalian (early Miocene). Antecedent topography and rapid high-amplitude sea-level change are the main controlling factors on stratigraphic architecture and sediment type. Stratigraphic evidence is observed for two high- amplitude (100–150 m) sea-level cycles in the Late Burdigalian to Langhian. These cycles are interpreted to be eustatic in nature and driven by the long-term 400-Ka orbital eccentricity-cycle-changing ice volumes in the nascent Antarctic icecap. We propose that the Mut Basin is an exemplary case study area for guiding lithostratigraphic predictions in early Miocene shallow- marine carbonate and mixed environments elsewhere in the world. The Late Burdigalian in the Mut Basin was a time of relative tectonic quiescence, during which a complex relict basin topography was flooded by a rapid marine transgression. This area was chosen for study because it presents extraordinary large- scale 3D outcrops and a large diversity of depositional environments throughout the basin. Three study transects were constructed by combining stratal geometries and facies observations into a high-resolution sequence stratigraphic framework. 3346 m of section were logged, 400 thin sections were studied, and 145 biostratigraphic samples were analysed for nannoplankton dates (Bassant, P., 1999.
    [Show full text]
  • 1 Cyclical Shoreline Erosion: the Impact of a Jettied River Mouth on the Downdrift Barrier Island
    CYCLICAL SHORELINE EROSION: THE IMPACT OF A JETTIED RIVER MOUTH ON THE DOWNDRIFT BARRIER ISLAND ANDREW R. FALLON1, CHRISTOPHER J. HEIN2, PETER S. ROSEN3, HALEY L. GANNON4 1. Virginia Institute of Marine Science, College of William and Mary, 1375 Greate Rd, Gloucester Point, Virginia 23062, [email protected] 2. Virginia Institute of Marine Science, College of William and Mary, 1375 Greate Rd, Gloucester Point, Virginia 23062, [email protected] 3. Northeastern University, 360 Huntington Ave, Boston Massachusetts, 02115, [email protected] 4. College of William and Mary, 200 Stadium Drive, Williamsburg, VA 23186, [email protected] Abstract: Beaches and inlets throughout the U.S. have been stabilized for purposes of navigation, erosion mitigation, and economic resilience, commonly leading to changes in shoreline dynamics and downdrift erosion/accretion patterns. The developed beach of Plum Island, Massachusetts is highly dynamic, experiencing regular complex erosion / accretion patterns along much of the shoreline. We analyzed > 100 years of high-water line positions derived from satellite imagery, t-sheets, historical maps, and aerial photography. Unlike most beaches, the river-proximal sections of Plum Island are not uniformly retreating. Rather, the beach undergoes short-term erosion, followed by periods of accretion and return to a long-term mean stable shoreline position. These cycles occur over different timeframes and in different segments of the beach, creating an ephemeral erosion ‘hotspot’ lasting as briefly as one year. The highly dynamic and spatially diverse nature of erosion along Plum Island provides insight into the complex nature of coupled inlet-beach dynamics over multiple timescales. Introduction Coastlines throughout the world have been highly developed, creating high risk areas due to the dynamic nature of beaches, tidal inlets and barrier islands.
    [Show full text]
  • Published Version
    PUBLISHED VERSION Lewis, Megan Mary; White, Davina Cherie; Gotch, Travis Bruce (eds.) 2013, Allocating water and maintaining springs in the Great Artesian Basin. Volume IV. Spatial survey and remote sensing of artesian springs of the western Great Artesian Basin, Canberra, National Water Commission © Commonwealth of Australia 2013 This work is copyright. The Copyright Act 1968 permits fair dealing for study, research, news reporting, criticism or review and the National Water Commission supports and encourages the dissemination and exchange of its information. Selected passages, tables or diagrams may be reproduced for such purposes provided you attribute the National Water Commission as the source. Reproduction for commercial use or sale requires prior written permission from the National Water Commission. Requests and enquiries concerning reproduction and rights should be addressed to the Communication Director, National Water Commission, 95 Northbourne Avenue, Canberra ACT 2600 or email [email protected] PERMISSIONS This document is made available with special permission from the National Water Commission. 14.05.2013. The full report is available at the National Water Commission’s Archive site: http://archive.nwc.gov.au/library/topic/groundwater/allocating-water-and-maintaining- springs-in-the-great-artesian-basin ‘Allocating Water and Maintaining Springs in the GAB’ http://hdl.handle.net/2440/77601 Volume IV: Spatial Survey and Remote Sensing of Artesian Springs of the Western Great Artesian Basin Allocating Water and Maintaining Springs 6 in the Great Artesian Basin Evaluation of remote sensing approaches Megan M Lewis School of Earth and Environmental Sciences, The University of Adelaide Davina White School of Earth and Environmental Sciences, The University of Adelaide Volume IV: Spatial Survey and Remote Chapter 6: Evaluation of Sensing of Artesian Springs of the remote sensing approaches Western Great Artesian Basin Allocating Water and Maintaining Springs in the Great Artesian Basin 6 6.
    [Show full text]
  • Zellman Mines 0052E 11720.Pdf (6.993Mb)
    INVESTIGATING LINKS BETWEEN CLIMATE PERTURBATIONS, RIVER DISCHARGE VARIABILITY AND FLUVIAL FANS IN THE PALEOGENE SAN JUAN BASIN, NEW MEXICO, USA by Kristine L. Zellman © Copyright by Kristine L. Zellman, 2019 All Rights Reserved A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Geology). Golden, Colorado Date Signed: Kristine L. Zellman Signed: Dr. Piret Plink-Bj¨orklund Thesis Advisor Golden, Colorado Date Signed: Dr. M. Stephen Enders Professor and Head Department of Geology and Geological Engineering ii ABSTRACT The San Juan Basin in New Mexico preserves the southernmost sedimentary record of the Paleocene and early-Eocene in North America, and thus represents a critical point for comparison for climatic and biotic change during the Paleogene. This dissertation combines basin-scale 3D outcrop analyses of fluvial architecture and preliminary stable carbon isotope records from the Paleocene upper Nacimiento Formation and the early-Eocene San Jose Formation to investigate the link between Paleogene climate perturbations and depositional trends. Through these investigations, we 1) identify the succession as deposits of variable dis- charge river systems, 2) observe a long-term stratigraphic trend toward increasingly well- drained floodplain deposits, and thus successively more arid conditions from Paleocene into the early-Eocene that we suggest may indicate a long-term shift from a monsoonal climate in the Paleocene to fluctuating humid and arid subtropical and then semi-arid/arid conditions in the early Eocene, 3) identify the Paleocene uppermost Nacimiento Formation and early- Eocene Cuba Mesa and Regina Members of the San Jose Formation as deposits of a large fluvial fan and identify at least two vertical packages of fan progradation, and 4) identify at least two negative carbon isotope excursions that may record the Paleocene-Eocene Thermal Maximum (PETM) and one or more post-PETM hyperthermal events.
    [Show full text]
  • Figure 3A. Major Geologic Formations in West Virginia. Allegheney And
    82° 81° 80° 79° 78° EXPLANATION West Virginia county boundaries A West Virginia Geology by map unit Quaternary Modern Reservoirs Qal Alluvium Permian or Pennsylvanian Period LTP d Dunkard Group LTP c Conemaugh Group LTP m Monongahela Group 0 25 50 MILES LTP a Allegheny Formation PENNSYLVANIA LTP pv Pottsville Group 0 25 50 KILOMETERS LTP k Kanawha Formation 40° LTP nr New River Formation LTP p Pocahontas Formation Mississippian Period Mmc Mauch Chunk Group Mbp Bluestone and Princeton Formations Ce Obrr Omc Mh Hinton Formation Obps Dmn Bluefield Formation Dbh Otbr Mbf MARYLAND LTP pv Osp Mg Greenbrier Group Smc Axis of Obs Mmp Maccrady and Pocono, undivided Burning Springs LTP a Mmc St Ce Mmcc Maccrady Formation anticline LTP d Om Dh Cwy Mp Pocono Group Qal Dhs Ch Devonian Period Mp Dohl LTP c Dmu Middle and Upper Devonian, undivided Obps Cw Dhs Hampshire Formation LTP m Dmn OHIO Ct Dch Chemung Group Omc Obs Dch Dbh Dbh Brailler and Harrell, undivided Stw Cwy LTP pv Ca Db Brallier Formation Obrr Cc 39° CPCc Dh Harrell Shale St Dmb Millboro Shale Mmc Dhs Dmt Mahantango Formation Do LTP d Ojo Dm Marcellus Formation Dmn Onondaga Group Om Lower Devonian, undivided LTP k Dhl Dohl Do Oriskany Sandstone Dmt Ot Dhl Helderberg Group LTP m VIRGINIA Qal Obr Silurian Period Dch Smc Om Stw Tonoloway, Wills Creek, and Williamsport Formations LTP c Dmb Sct Lower Silurian, undivided LTP a Smc McKenzie Formation and Clinton Group Dhl Stw Ojo Mbf Db St Tuscarora Sandstone Ordovician Period Ojo Juniata and Oswego Formations Dohl Mg Om Martinsburg Formation LTP nr Otbr Ordovician--Trenton and Black River, undivided 38° Mmcc Ot Trenton Group LTP k WEST VIRGINIA Obr Black River Group Omc Ordovician, middle calcareous units Mp Db Osp St.
    [Show full text]
  • Deciphering the Origin of Cyclical Gravel Front and Shoreline Progradation and Retrogradation in the Stratigraphic Record
    Deciphering the origin of cyclical gravel front and shoreline progradation and retrogradation in the stratigraphic record John J. Armitage1, Peter A. Burgess2, Gary J. Hampson3, and Philip A. Allen3 1Department of Earth Science, Royal Holloway, University of London, Egham, UK; Now at Institut de Physique du Globe de Paris, 1 rue Jussieu, Paris, 75005, France; e-mail: [email protected] 2Department of Earth Science, Royal Holloway, University of London, Egham, UK 3Department of Earth Science and Engineering, Imperial College London, London, UK May 4, 2016 1 1 Abstract 2 Nearly all successions of near-shore strata exhibit cyclical movements of the shoreline, which 3 have commonly been attributed to cyclical oscillations in relative sea level (combining eustasy 4 and subsidence) or, more rarely, to cyclical variations in sediment supply. It has become accepted 5 that cyclical change in sediment delivery from source catchments may lead to cyclical movement 6 of boundaries such as the gravel front, particularly in the proximal segments of sediment routing 7 systems. In order to quantitatively assess how variations in sediment transport as a consequence 8 of change in relative sea-level and surface run-off control stratigraphic architecture, we develop a 9 simple numerical model of sediment transport and explore the sensitivity of moving boundaries 10 within the sediment routing system to change in upstream (sediment flux, precipitation rate) and 11 downstream (sea level) controls. We find that downstream controls impact the shoreline and sand 12 front, while the upstream controls can impact the whole system depending on the amplitude of 13 change in sediment flux and precipitation rate.
    [Show full text]
  • Cross Section
    U.S. DEPARTMENT OF THE INTERIOR SCIENTIFIC INVESTIGATIONS MAP 3425 U.S. GEOLOGICAL SURVEY (SHEET 2 OF 2) Explanatory pamphlet accompanies map A' Allegheny structural front Valley Allegheny and Plateau Ridge province province LAUREL FERNEY- SECOND- SABINSVILLE MARSHLANDS WELLSBORO SLATE RUN HILL-HYNER WATERVILLE TOMBS RUN TORBERT NIPPENOSE ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE (NITTANY ANTICLINORIUM) CLEARFIELD-ENGLISH SHORT COWANESQUE PINE CREEK KETTLE CREEK BLOSSBURG CENTER-MCINTYRE-BARCLAY JERSEY MILLS SNOW SHOE MOUNTAIN WHITE DEER SYNCLINE SYNCLINE SYNCLINE SYNCLINE SYNCLINE SYNCLINE SYNCLINE SYNCLINE SYNCLINE Bend in section Bend in section West Branch of New York Susquehanna Pennsylvania Cowanesque NE SW Kettle NE SE Pine River Creek Creek River FEET 100 110 120 130 140 150 160 170 180 3,000 80° 79° 78° 77° 7 8 9 10 Amoco Production Company Consolidated Gas Supply Corporation Texaco-Marathon, Inc. California Company Huntley OSWEGO Allegheny No. 1 Harry P. Dewey Mountain No. 1 Pa. Dept. of Forest and Water Tract 129 No. 1 Pa. State Forest Tract 285-1 No. 1 W.E. Snyder NEW YORK COUNTY Huntley Formation Huntley API No. 37-117-20057 Formation API No. 37-105-20182 API No. 37-035-20276 API No. 37-081-90002 ONTARIO LAKE ONTARIO Mountain Pottsville Mountain Huntley EXPLANATION Huntley Formation Formation Formation Tioga Co., Pennsylvania Potter Co., Pennsylvania Clinton Co., Pennsylvania Lycoming Co., Pennsylvania Mountain Huntley Mauch Burgoon Mountain Formation Huntley Burgoon Mauch A–A’ line of cross section Huntley Mountain Chunk Mauch Chunk Sandstone Catskill Formation Mountain Sandstone Formation Mauch Chunk Physiographic province boundary Formation Mountain Formation Formation Pottsville Formation Hilton Huntley Formation 0 Chunk Formation Burgoon Sandstone ORLEANS COUNTY Formation Burgoon Formation 2,000 River or stream Pine Mountain Sandstone Brockport Webster Cross Formation 0 m.
    [Show full text]
  • Xsec A-A Sht1of2 Layout FINAL V
    U.S. DEPARTMENT OF THE INTERIOR SCIENTIFIC INVESTIGATIONS MAP 3425 U.S. GEOLOGICAL SURVEY (SHEET 1 OF 2) Explanatory pamphlet accompanies map A Ontario Allegheny Lowlands Plateau province province SEVERNE WATKINS-BEAVER LODI POINT FIRTREE DAMS ALPINE VAN ETTEN ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE GLENORA SYNCLINE UNNAMED COHOCTON CORBETT POINT ENFIELD CAYUTA SYNCLINE SYNCLINE SYNCLINE SYNCLINE SYNCLINE Bend in section Bend in section Bend in section New York W SE Oatka Genesee NW SE Canisteo NW SW Pennsylvania Black Creek River Canaseraga River Tuscarora Creek Creek Creek FEET MILES 0 10 20 30 40 50 60 70 80 90 3,000 1 2 3 4 5 6 William Duchscherer, Jr. E.F. Blair and Associates NYS Natural Gas Company E.F. Blair and Associates Bowdoin Storage Service Inc. NYS Natural Gas Company No. 1 J. Klotzbach No. 1 L. Tyler No. 1 Albert McClurg No. 1 Arthur N. Kennedy No. 1 Hubbard No. 1 Robert Olin API No. 31-037-05117 API No. 31-037-04593 API No. 31-051-04552 API No. 31-051-04630 API No. 31-101-21496 API No. 31-101-03924 Genesee Co., New York Genesee Co., New York Livingston Co., New York Livingston Co., New York Steuben Co., New York Steuben Co., New York Perrysburg Formation Dunkirk Dunkirk Shale Shale 2,000 Member Wiscoy Sandstone Member Java Perrysburg West River Shale, Nunda Wiscoy Sandstone Member Formation Formation Genundewa Sandstone Member unnamed Pipe Creek 0 Pipe Creek shale member Limestone, Penn Member Shale Member Shale Member Perrysburg Yan Shale, and rmation Formation 0 Dun West River Shale, Java Fo kirk
    [Show full text]
  • Drill Cores Through the Table Mountain Latite Near Knights Ferry Carolyn Gornya, Cathy Busbya*, Christopher J
    International Geology Review Vol. 51, Nos. 9–11, September–November 2009, 824–842 An in-depth look at distal Sierra Nevada palaeochannel fill: drill cores through the Table Mountain Latite near Knights Ferry Carolyn Gornya, Cathy Busbya*, Christopher J. Pluharb, Jeanette Hagana and Keith Putirkab aDepartment of Earth Science, University of California, Santa Barbara, CA 93101, USA; bDepartment of Earth and Environmental Sciences, California State University, Fresno, CA 93740, USA (Accepted 24 March 2009) The ,10.4 Ma Table Mountain Latite (TML) consists of high-K trachyandesite lavas that likely erupted from the Little Walker Center near Sonora Pass and flowed 80 miles (130 km) through the palaeo-Stanislaus river channel to Knights Ferry in the Sierra Nevada foothills. Complete sections through the proximal facies of the flow stratigraphy are common in the high-Sierra and along range-front faults, but in much of its distal facies in the Sierra Nevada foothills, the internal features of the unit are poorly exposed. Condor Earth Technologies offered us the opportunity to study three complete vertical sections through the distal facies of the TML through access to three drill cores. These cores, spaced 1500 0 (457 m) apart and oriented oblique to inferred flow direction by 308, are referred to here as cores A, B, and C, in a down-palaeoflow direction. Previous outcrop studies of the distal TML over the past century have concluded that the distal TML consists of a single flow. This is true of core B, which is dominated by a single 1440 (44 m) thick flow, underlain by a thin (,50, 1.5 m) flow with a vesiculated top, inferred to represent a toe of the thick flow, inasmuch as there is no baked zone or weathered contact between them.
    [Show full text]