(A) Placement Above Uppermost Aquifer
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Coal and Francis Creek Shale
University of Pennsylvania ScholarlyCommons Department of Earth and Environmental Departmental Papers (EES) Science January 1970 A comparison of the floras of the Colchester (No. 2) Coal and Francis Creek Shale R. A. Peppers Illinois State Geological Survey Hermann W. Pfefferkorn University of Pennsylvania, [email protected] Follow this and additional works at: https://repository.upenn.edu/ees_papers Recommended Citation Peppers, R. A., & Pfefferkorn, H. W. (1970). A comparison of the floras of the Colchester (No. 2) Coal and Francis Creek Shale. Retrieved from https://repository.upenn.edu/ees_papers/18 This material has been published in Smith, W.H., Nance, R.B., Hopkins, Johnson, R.G., and Shabica, C.W. Depositional environments in parts of the Carbondale formation, western and northern Illinois: Francis Creek Shale and associated strata and Mazon Creek biota, Illinois State Geological Survey Field Guidebook Series, No. 8, p. 61-74, 1970 NOTE: At the time of publication, author Hermann W. Pfefferkorn was affiliated with the Illinois State Geological Survey. Currently (September 2005) he is a faculty member in the Department of Earth and Environmental Science at the University of Pennsylvania. This paper is posted at ScholarlyCommons. https://repository.upenn.edu/ees_papers/18 For more information, please contact [email protected]. A comparison of the floras of the Colchester (No. 2) Coal and Francis Creek Shale Abstract Abundant data from spore studies of the Colchester (no. 2) Coal Member and from investigations of plant compressions in the Francis Creek Shale provide an opportunity to compare the flora of the coal with that of the overlying shale in the northeastern part of the Illinois Basin. -
Bedrock Geology of Carbondale Quadrangle
BEDROCK GEOLOGY OF CARBONDALE QUADRANGLE Prairie Research Institute JACKSON AND WILLIAMSON COUNTIES, ILLINOIS Illinois Geologic Quadrangle Map ILLINOIS STATE GEOLOGICAL SURVEY IGQ Carbondale-BG W. John Nelson 2013 89°15' 12'30" 10' 89°07'30" 720 000FEET (IL E) 3 000mE 3 3 3 3 3 3 R. 1 W. 2 590 000 FEET (IL W) R. 1 E. 3 37°45' 03 04 05 06 07 08 10 12 37°45' 51 4180 7 8 9 10 11 12 7 8 000m &c 4180 N 13 &c Creek d r a & h t c m r C CG 508 O &c k" m r a U.S. 366 41 b e" 79 Fish and 18 17 16 15 &t 18 17 &c 13 Wildlife Ho g an 14 Po i n t 4179 m O b r a c r h Pine C a Lo n g Vi ew Island 390000 r 13 d Park FEET (IL E) Sk" 98 390 000 Ck" 322 k" 97 FEET (IL W) m 152 E 4178 k e" K r o A F L 41 ¿ S 273 78 k" PO D ¿ m R e 13 A l C t H t r i CARBONDALE C L R EXPLANATION O 19 22 19 20 20 23 24 B m A 21 R ¿ C Holocene sm Surface mine 4177 k" 105 &t ¿ m c s ¿ 41 e &t 77 Univ ersity l i &c Carbondale Formation School P m » m Desmoinesian Tradewater Formation s s, Stonefort Limestone Member m m, Murphysboro Coal Member Pennsylvanian c c, Curlew Member Southern Illinois ¿ University S 62 &t k" &t-mb Murray Bluff Sandstone Member » &t s 4176 Atokan ¿ &t &t-o olive shale member 27 4176 29 &t-g Grindstaff Sandstone Member 29 C s am e 28 30 pus Lak À 26 25 30 42'30" À 42'30" ¿ 270 m À k" S 1201 &t 290 270 Ü k" k" ªNorth uthern Hill s m So 4175 s k"317 k" 137 s 4175 &t-mb ¿ Symbols Marberry Arboretum 40 Strike and dip of bedding; number indicates degree of dip Carbondale &t r ¿ Reservoi m Horizontal bedding &t r sm ¿ 31 Evergreen Terrace C 32 Vertical joints 4174 31 34 35 36 32 k r 33 ¿ c o ¿ » Shaft mine Sk" 250 F 51 4174 ¿ S ¿ y ¿ Slope mine &t-mb c a m o ¿ À » r m Drift mine c e s m le ¿ ¿ i & ¿ t-mb m ¿ P sm ( À T. -
Bedrock Geology of Edwardsville Quadrangle
Rod R. Blagojevich, Governor BEDROCK GEOLOGY OF EDWARDSVILLE QUADRANGLE Department of Natural Resources Joel Brunsvold, Director MADISON COUNTY, ILLINOIS Illinois State Geological Survey William W. Shilts, Chief Joseph A. Devera and F. Brett Denny 2003 BUNKER HILL 12 MI. 2 000m. 2 2 2 2 2 2 2 90°00' 40 E. 41 42 1.6 MI. TO ILL. 140 57' 30" 44 45 R. 8 W. 46 R. 7 W. 55' 48 49 580 000 FEET 89°52'30'' 38°52'30" 38°52'30" 159 Psb 400 Eberhart Cem St James Cem 4306 21 22 23 24 19 20 21 4306000m.N. HENKE LANDING STRIP 375 Psb Shelburn Formation 400 350 Pennsylvanian Desmoinsian ek 800 000 re C FEET Pcb Carbondale Formation Gard Pcb 400 I M Quercus Grove 4 Maple . 2 Cem L E 157 M A Quercus Grove H Park 4305 Line symbols: dashed where inferred Petroleum and Coal Resources a h i c 26 k 28 n o a h of Madison County 27 r a C 25 B Barnett (Resources have been removed) 30 29 Contact 375 28 43 Macoupin County 04 475 Bedrock topography (elevation in feet) Madison County 325 350 4304 325 Coal test (depth in feet) Oil test, dry hole (depth in feet) s Golf gh ou Course rr u 43 Oil test, show of oil (depth in feet) B 03 . I . I 33 M 35 M 2 7 1 2 N 36 31 D O 34 32 L Edwardsville T Mine shaft, abandoned E 33 I . S I F G M H Quadrangle N I C 5 V T I I . -
Kentucky Oversize/ Overweight Permit Manual
Oversize/ Overweight Permit Manual Kentucky Foreword The Specialized Carriers & Rigging Association is pleased to publish this Oversize/ Overweight Permit Manual. Each state analysis includes information in a standardized format: contact, legal limits, special permit limits, general restrictions, types of permits available, fees, escort needs, fines, and restricted travel areas. Telephone numbers, locations, and hours of operation are listed for ports of entry and permit branches. However, readers are always advised to check with the state offices on current laws and procedures. This project could not have been completed without the advice and consultation of many state officials. We thank all of those who provided permit manuals, maps, laws, regulations, and various other forms of documentation. Legal Notice This SC&RA Oversize/Overweight Permit Manual is intended only to provide concise, easily read information, useful in planning movements of overdimensional and overweight loads. This Permit Manual is not intended to be an accurate summary of all the applicable laws and regulations. Users of the Permit Manual should confirm the information contained herein before dispatching vehicles and loads. The SC&RA cautions Permit Manual users that state laws and regulations are subject to change without notice, and that some time elapses between the effective date of such changes and the amendment of the Permit Manual to reflect those changes. The SC&RA assumes no responsibility for accident, injury, loss or claim, penalties or any other damage resulting from reliance on the contents of this Permit Manual. Specialized Carriers & Copyright 1987-2015 by the Specialized Carriers & Rigging Association. All rights reserved. No part of this publication may Rigging Association be reproduced, stored in a retrieval system, or transmitted in any 5870 Trinity Parkway, Suite 200 form or by any means, electronic, mechanical, photocopying, Centreville, VA 20120 recording, scanning, or otherwise, without the prior written PHONE: (703) 698-0291 permission of the publisher, Joel M. -
A CONCURRENT RESOLUTION Urging the United States Government to 2 Designate a Portion of the Edward T
UNOFFICIAL COPY 17 RS BR 1556 1 A CONCURRENT RESOLUTION urging the United States government to 2 designate a portion of the Edward T. Breathitt Pennyrile Parkway as Interstate 169. 3 WHEREAS, the Edward T. Breathitt Pennyrile Parkway opened as a toll road on 4 Kentucky's Parkway system in 1969, providing a fast and efficient connection between 5 the cities of Henderson and Hopkinsville; and 6 WHEREAS, in 2006, the section of the Edward T. Breathitt Pennyrile Parkway 7 from Henderson to the Western Kentucky Parkway was designated as a portion of 8 Interstate 69, and in 2015, legislation directed that the route be signed as Interstate 69; 9 and 10 WHEREAS, designating the remainder of the Edward T. Breathitt Pennyrile 11 Parkway as an interstate spur would provide increased connectivity between Interstate 69 12 and Interstate 24; and 13 WHEREAS, designation of the remainder of the Edward T. Breathitt Pennyrile 14 Parkway as an interstate spur could save the federal government and the Commonwealth 15 nearly $200 million and maximize investments already made, like the $100 million 16 invested in the road in the 1990s to achieve this ultimate goal ; and 17 WHEREAS, designation of the remainder of the Edward T. Breathitt Pennyrile 18 Parkway as an interstate spur will enhance the region by helping to bring in much needed 19 economic and tourism dollars, especially since so many businesses emphasize connection 20 to the interstate highway system when researching site selection; and 21 WHEREAS, designation of the remainder of the Edward T. Breathitt -
Exploring Phylogenomic Relationships Within Myriapoda: Should High Matrix Occupancy Be the Goal?
bioRxiv preprint doi: https://doi.org/10.1101/030973; this version posted November 9, 2015. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Exploring phylogenomic relationships within Myriapoda: should high matrix occupancy be the goal? ROSA FERNÁNDEZ1, GREGORY D. EDGECOMBE2 AND GONZALO GIRIBET1 1Museum of Comparative Zoology & Department of Organismic and Evolutionary Biology, Harvard University, 26 Oxford Street, Cambridge, MA 02138, USA 2Department of Earth Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK 1 bioRxiv preprint doi: https://doi.org/10.1101/030973; this version posted November 9, 2015. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Abstract.—Myriapods are one of the dominant terrestrial arthropod groups including the diverse and familiar centipedes and millipedes. Although molecular evidence has shown that Myriapoda is monophyletic, its internal phylogeny remains contentious and understudied, especially when compared to those of Chelicerata and Hexapoda. Until now, efforts have focused on taxon sampling (e.g., by including a handful of genes in many species) or on maximizing matrix occupancy (e.g., by including hundreds or thousands of genes in just a few species), but a phylogeny maximizing sampling at both levels remains elusive. In this study, we analyzed forty Illumina transcriptomes representing three myriapod classes (Diplopoda, Chilopoda and Symphyla); twenty-five transcriptomes were newly sequenced to maximize representation at the ordinal level in Diplopoda and at the family level in Chilopoda. -
Chapter 180 1
CHAPTER 180 1 CHAPTER 180 ( HCR 90 ) A CONCURRENT RESOLUTION urging the United States government to designate a portion of the Edward T. Breathitt Pennyrile Parkway as Interstate 169. WHEREAS, the Edward T. Breathitt Pennyrile Parkway opened as a toll road on Kentucky's Parkway system in 1969, providing a fast and efficient connection between the cities of Henderson and Hopkinsville; and WHEREAS, in 2006, the section of the Edward T. Breathitt Pennyrile Parkway from Henderson to the Western Kentucky Parkway was designated as a portion of Interstate 69, and in 2015, legislation directed that the route be signed as Interstate 69; and WHEREAS, designating the remainder of the Edward T. Breathitt Pennyrile Parkway as an interstate spur would provide increased connectivity between Interstate 69 and Interstate 24; and WHEREAS, designation of the remainder of the Edward T. Breathitt Pennyrile Parkway as an interstate spur could save the federal government and the Commonwealth nearly $200 million and maximize investments already made, like the $100 million invested in the road in the 1990s to achieve this ultimate goal ; and WHEREAS, designation of the remainder of the Edward T. Breathitt Pennyrile Parkway as an interstate spur will enhance the region by helping to bring in much needed economic and tourism dollars, especially since so many businesses emphasize connection to the interstate highway system when researching site selection; and WHEREAS, designation of the remainder of the Edward T. Breathitt Pennyrile Parkway as an interstate spur would continue to improve the vital role that the interstate highway system plays in our national defense logistics system especially as it pertains to Fort Campbell; and WHEREAS, current projects in Kentucky's Six Year Road Plan address intersection issues that pose potential obstacles to an interstate designation; and WHEREAS, legislation has passed the United States Senate that would designate the remainder of the Edward T. -
Geology for Planning in St. Clair County, Illinois
465 � JSGS-- -OIL & 6AS s SECJIGN--=fltES 14.GS: STATE OF ILLINOIS CIR465 c.4 DEPARTMENT OF REGISTRATION AND ED UCATION GEOLOGY FOR PLANNING IN ST. CLAIR COUNTY, ILLINOIS Alan M. Jacobs, compiler ILLINOIS ST ATE GEOLOGIC AL SURVEY John C. Frye, Chief Urbana, IL 61801 CIRCULAR 465 1971 GEOLOGY FOR PLANNING IN ST. CLAIR COUNTY, ILLINOIS Alan M. Jacobs, compiler ABSTRACT St. Clair County lies in southwestern Illinois across the Mississippi River from St. Louis, Missouri . One-fifth of the total land surface of 673 square miles is on flood plains of the Mississippi and Kaskaskia Rivers and Silver Creek. The floodplains are underlain by as much as 120 feet of gravel, sand, silt, and clay. The remaining fo ur fifths of the land surface is on uplands that contain flat or dissected plains, low ridges and mound-shaped hills, about 20 square miles of strip mines , and an area of karst topog raphy. The uplands are underlain by as much as 75 feet of till and sand and gravel, and generally 12 to 3 0 feet of loess and related silt; however, near the Mississippi River bluffs there are more than 100 feet of loes s and related silt. These deposits have been redistributed into spoil piles in the strip mines. Ben<ilath these deposits or cropping out in places are gently sloping beds of limestone, shale, sand stone, siltstone, clay stone, and coal. Thinly layered, frac tured limestone underlies the area of karst topography. Mineral and water resources are abundant in the county . Limestone of the St. -
Detailed Sedimentological Study of the West Franklin Limestone Member
Detailed Sedimentological Study of the West Franklin Limestone Member (Desmoinesian to Missourian) of the Shelburn Formation (Upper Pennsylvanian) of southwestern Indiana Grace L. Stone and William S. Elliott, Jr. Department of Geology and Physics, University of Southern Indiana, 8600 University Blvd., Evansville, Indiana 47712; [email protected] Introduction Results Discussion The West Franklin Limestone is a key marker bed in correlating Middle to Upper Southwest Indiana is underlain by gently, westward dipping (2° to 3°) Middle to Upper Photomicrograph of skeletal 76.4 to 76.9 feet depth: tan to gray, Pennsylvanian strata in the Illinois Basin (Wier & Ault, 1986; Brown & Rexroad, 2009). It is Pennsylvanian strata on the southern margin of the Illinois Basin consisting of recurring packstone showing broken bioturbated, skeletal packstone with typically identified by two limestone benches separated by an interval of siliciclastic deposits of limestone, sandstone, shale, and coal (Fig. 1). USI 1-32, an exploratory USI 1-32 Core Upper Bench of skeletal fragments that include, broken crinoid, brachiopod, sediment, but the number of benches is variable from the absence of the limestone to four coalbed methane well drilled in 2009, is located at 37.951° N and 87.670°W south of 75 bryozoans, gastropods, forams, West Franklin bryozoan, and gastropod fossils with discrete limestone intervals (Anderson, 1956; King, 1994; Heckel et al., 1998; Rexroad et al., the campus of the University of Southern Indiana in Vanderburgh County, Indiana (Fig. and algae, with a micrite mud traces of disseminated pyrite. 2008; Gray, 2011). 2). The total depth of the well is 780 feet with a core recovered from the West Franklin Limestone matrix from 76.45 feet depth. -
B2150-B FRONT Final
Bedrock Geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Kentucky, and Missouri By W. John Nelson THE PADUCAH CUSMAP QUADRANGLE: RESOURCE AND TOPICAL INVESTIGATIONS Martin B. Goldhaber, Project Coordinator T OF EN TH TM E U.S. GEOLOGICAL SURVEY BULLETIN 2150–B R I A N P T E E R D . I O S . R A joint study conducted in collaboration with the Illinois State Geological U Survey, the Indiana Geological Survey, the Kentucky Geological Survey, and the Missouri M 9 Division of Geology and Land Survey A 8 4 R C H 3, 1 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1998 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Mark Schaefer, Acting Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 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 Nelson, W. John Bedrock geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Ken- tucky, and Missouri / by W. John Nelson. p. cm.—(U.S. Geological Survey bulletin ; 2150–B) (The Paducah CUSMAP Quadrangle, resource and topical investigations ; B) Includes bibliographical references. Supt. of Docs. no. : I 19.3:2150–B 1. Geology—Middle West. I. Title. II. Series. III. Series: The Paducah CUSMAP Quadrangle, resource and topical investigations ; B QE75.B9 no. 2150–B [QE78.7] [557.3 s—dc21 97–7724 [557.7] CIP CONTENTS Abstract .......................................................................................................................... -
I-69 Ohio River Crossing DEIS, Appendix H-1 Farmland Coordination
I-69 Ohio River Crossing Project Draft Environmental Impact Statement APPENDIX H-1 Farmland Coordination Page Indiana Letter February 20, 2018 ................................................................................. 1 Form NRCS‐CPA‐106 Indiana ................................................................................... 10 Kentucky Letter February 20, 2018 ........................................................................... 20 Form NRCS‐CPA Kentucky ....................................................................................... 22 NRCS Response March 19, 2018 ................................................................................ 48 Form NRCS‐CPA‐106 Indiana April 4, 2018 ............................................................ 54 Form NRCS‐CPA‐106 Kentucky March 19, 2018 .................................................... 55 Clarification Note for Central Alternative 1: Central Alternatives 1A and 1B as described in the DEIS are physically the same alternative. The only difference between them is that Central Alternative 1A would include tolls on both the new I-69 bridge and on the US 41 bridge. Central Alternative 1B would only include tolls on the new I-69 bridge. Any reference in this document to Central Alternative 1 applies to both Central Alternative 1A and Central Alternative 1B. Appendices OHIO RIVER CROSSING 16SDHIDRIVERCR0SSING.CDM February 20, 2018 Ms. Jane Hardisty State Conservationist Natural Resources Conservation Service - Indiana US Department of Agriculture 6013 Lakeside Boulevard -
Fossil Calibrations for the Arthropod Tree of Life
bioRxiv preprint doi: https://doi.org/10.1101/044859; this version posted June 10, 2016. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. FOSSIL CALIBRATIONS FOR THE ARTHROPOD TREE OF LIFE AUTHORS Joanna M. Wolfe1*, Allison C. Daley2,3, David A. Legg3, Gregory D. Edgecombe4 1 Department of Earth, Atmospheric & Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA 2 Department of Zoology, University of Oxford, South Parks Road, Oxford OX1 3PS, UK 3 Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PZ, UK 4 Department of Earth Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK *Corresponding author: [email protected] ABSTRACT Fossil age data and molecular sequences are increasingly combined to establish a timescale for the Tree of Life. Arthropods, as the most species-rich and morphologically disparate animal phylum, have received substantial attention, particularly with regard to questions such as the timing of habitat shifts (e.g. terrestrialisation), genome evolution (e.g. gene family duplication and functional evolution), origins of novel characters and behaviours (e.g. wings and flight, venom, silk), biogeography, rate of diversification (e.g. Cambrian explosion, insect coevolution with angiosperms, evolution of crab body plans), and the evolution of arthropod microbiomes. We present herein a series of rigorously vetted calibration fossils for arthropod evolutionary history, taking into account recently published guidelines for best practice in fossil calibration.