U.S. Geological Survey Bulletin 2163

Total Page:16

File Type:pdf, Size:1020Kb

U.S. Geological Survey Bulletin 2163 Availability of Publications of the U.S. Geological Survey Order U.S. Geological Survey (USGS) publications from the Documents. Check or money order must be payable to the offices listed below. Detailed ordering instructions, along with Superintendent of Documents. Order by mail from— prices of the last offerings, are given in the current-year issues of the catalog “New Publications of the U.S. Geological Survey.” Superintendent of Documents Government Printing Office Books, Maps, and Other Publications Washington, D.C. 20402 By Mail Information Periodicals Books, maps, and other publications are available by mail Many Information Periodicals products are available through from— the systems or formats listed below: USGS Information Services Printed Products Box 25286, Federal Center Denver, CO 80225 Printed copies of the Minerals Yearbook and the Mineral Commodity Summaries can be ordered from the Superinten- Publications include Professional Papers, Bulletins, Water- dent of Documents, Government Printing Office (address Supply Papers, Techniques of Water-Resources Investigations, above). Printed copies of Metal Industry Indicators and Min- Circulars, Fact Sheets, publications of general interest, single eral Industry Surveys can be ordered from the Center for Dis- copies of permanent USGS catalogs, and topographic and ease Control and Prevention, National Institute for thematic maps. Occupational Safety and Health, Pittsburgh Research Center, Over the Counter P.O. Box 18070, Pittsburgh, PA 15236-0070. Mines FaxBack: Return Fax Service Books, maps, and other publications of the U.S. Geological Survey are available over the counter at the following USGS Earth Science Information Centers (ESIC’s), all of which are 1. Use the touch-tone handset attached to your fax machine’s authorized agents of the Superintendent of Documents. telephone jack. (ISDN [digital] telephones cannot be used with fax machines.) • Anchorage, Alaska—Rm. 101, 4230 University Dr. 2. Dial (703) 648-4999. • Denver, Colorado—Bldg. 810, Federal Center 3. Listen to the menu options and punch in the number of • Menlo Park, California—Rm. 3128, Bldg. 3, your selection, using the touch-tone telephone. 345 Middlefield Rd. 4. After completing your selection, press the start button on • Reston, Virginia—Rm. 1C402, USGS National Center, your fax machine. 12201 Sunrise Valley Dr. • Salt Lake City, Utah—2222 West, 2300 South (books and CD-ROM maps available for inspection only) • Spokane, Washington—Rm. 135, U.S. Post Office A disc containing chapters of the Minerals Yearbook (1933– Bldg., 904 West Riverside Ave. 95), the Mineral Commodity Summaries (1995–97), a statisti- • Washington, D.C.—Rm. 2650, Main Interior Bldg., cal compendium (1970–90), and other publications is updated 18th and C Sts., NW. three times a year and sold by the Superintendent of Docu- ments, Government Printing Office (address above). Maps only may be purchased over the counter at the following USGS office: World Wide Web • Rolla, Missouri—1400 Independence Rd. Minerals information is available electronically at http://minerals.er.usgs.gov/minerals/ Electronically Subscription to the Catalog “New Publications of the Some USGS publications, including the catalog “New Publi- U.S. Geological Survey” cations of the U.S. Geological Survey,” are also available elec- tronically on the USGS’s World Wide Web home page at Those wishing to be placed on a free subscription list for the http://www.usgs.gov catalog “New Publications of the U.S. Geological Survey” should write to— Preliminary Determination of Epicenters U.S. Geological Survey Subscriptions to the periodical “Preliminary Determination of 903 National Center Epicenters” can be obtained only from the Superintendent of Reston, VA 20192 U.S. Department of the Interior U.S. Geological Survey Lateral Ramps in the Folded Appalachians and in Overthrust Belts Worldwide—A Fundamental Element of Thrust-Belt Architecture By Howard A. Pohn U.S. GEOLOGICAL SURVEY BULLETIN 2163 Lateral ramps in the subsurface can be detected from changes in surface folds. Such changes occur in fold-and-thrust belts worldwide and probably indicate lateral ramps. U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 2000 Published in the Eastern Region, Reston, Va. Manuscript approved for publication August 10, 1998 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 For sale by U.S. Geological Survey Information Services Box 25286, Federal Center Denver, CO 80225 or call the toll-free telephone number 1-888-ASK-USGS Library of Congress Cataloging-in-Publication Data Pohn, Howard A. Lateral ramps in the folded Appalachians and in overthrust belts worldwide— A fundamental element of thrust-belt architecture / by Howard A. Pohn. p. cm. — (U.S. Geological Survey bulletin ; 2163) Includes bibliographical references. Supt. of Docs. no.: I19.3:2163 1. Thrust faults (Geology)—Appalachian Mountains. I. Title. II. Series. QE75.B9 no. 2163 [QE606.5.I5] 557.3 s—dc21 98-48485 [551.8′72′0974] CIP CONTENTS Abstract........................................................................................................................... 1 Introduction ....................................................................................................................1 Purpose and Scope.................................................................................................. 2 Acknowledgments .................................................................................................. 2 Geometric Considerations of Lateral Ramps.................................................................. 4 Overview ................................................................................................................ 4 The Basic Model..................................................................................................... 5 Field Examples and Supporting Data ............................................................................. 7 Susquehanna Lateral Ramp .................................................................................... 7 Stratigraphic and Structural Setting................................................................ 7 Seismic Evidence............................................................................................ 10 Dip-Line Section..................................................................................... 10 Strike-Line Section................................................................................. 11 Pennsylvania-Maryland-West Virginia Lateral Ramp ........................................... 11 Mathias Lateral Ramp ............................................................................................ 11 Surface Evidence ............................................................................................ 11 Seismic Evidence............................................................................................ 11 Highland County Lateral Ramp.............................................................................. 19 Surface and Geophysical Evidence ................................................................ 19 Seismic Evidence............................................................................................ 19 Igneous Intrusions Associated with Lateral Ramps ............................................... 19 Additional Lateral Ramps in the Central Appalachians ................................................. 19 Wilkes-Barre Lateral Ramp.................................................................................... 19 Seven Mountains Lateral Ramp ............................................................................. 26 Tyrone-Mount Union Lateral Ramp....................................................................... 27 Bedford Lateral Ramp ............................................................................................ 27 Lexington Lateral Ramp......................................................................................... 27 Roanoke Lateral Ramp ........................................................................................... 27 Fincastle Conglomerate: An Indicator of the Roanoke Lateral Ramp .......... 30 Changes in Unit Thickness and Lithologies................................................... 31 Coarse-Pebble Conglomerates Related to Other Ramps ........................................ 31 Lateral Ramps in the Southern Appalachians................................................................. 31 Lineament Swarms of Eastern Tennessee and Western North Carolina........................ 37 Lateral Ramps and Tectonic Windows........................................................................... 37 Lateral Ramps and Frequency of Disturbed Zones ........................................................ 46 Lateral Ramps and Possible Basement Faulting............................................................. 49 Movement Along Lateral Ramps Through Time ........................................................... 50 Observed Association of Lateral Ramps and Giant Landslides ..................................... 51 Possible Relationship of Lateral Ramps to Offshore Transform Faults......................... 51 The Presence of Lateral Ramps Worldwide................................................................... 52 Lateral
Recommended publications
  • A Taxonomic Revision of Rhododendron L. Section Pentanthera G
    A TAXONOMIC REVISION OF RHODODENDRON L. SECTION PENTANTHERA G. DON (ERICACEAE) BY KATHLEEN ANNE KRON A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 1987 , ACKNOWLEDGMENTS I gratefully acknowledge the supervision and encouragement given to me by Dr. Walter S. Judd. I thoroughly enjoyed my work under his direction. I would also like to thank the members of my advisory committee, Dr. Bijan Dehgan, Dr. Dana G. Griffin, III, Dr. James W. Kimbrough, Dr. Jonathon Reiskind, Dr. William Louis Stern, and Dr. Norris H. Williams for their critical comments and suggestions. The National Science Foundation generously supported this project in the form of a Doctoral Dissertation Improvement Grant;* field work in 1985 was supported by a grant from the Highlands Biological Station, Highlands, North Carolina. I thank the curators of the following herbaria for the loan of their material: A, AUA, BHA, DUKE, E, FSU, GA, GH, ISTE, JEPS , KW, KY, LAF, LE NCSC, NCU, NLU NO, OSC, PE, PH, LSU , M, MAK, MOAR, NA, , RSA/POM, SMU, SZ, TENN, TEX, TI, UARK, UC, UNA, USF, VDB, VPI, W, WA, WVA. My appreciation also is offered to the illustrators, Gerald Masters, Elizabeth Hall, Rosa Lee, Lisa Modola, and Virginia Tomat. I thank Dr. R. Howard * BSR-8601236 ii Berg for the scanning electron micrographs. Mr. Bart Schutzman graciously made available his computer program to plot the results of the principal components analyses. The herbarium staff, especially Mr. Kent D. Perkins, was always helpful and their service is greatly appreciated.
    [Show full text]
  • 7. Mineral Resources
    7. Mineral Resources The primary mineral resources extracted for human use in Allegany County are coal, sandstone, and limestone. Coal bearing formations are concentrated in the Georges Creek Basin in the western part of the county. Mineral resources present in Cumberland occur primarily in association with Shriver Ridge, Haystack Mountain, and Wills Mountain. All three of these landforms contain sandstone deposits of varying quality. Limestone formations occur between Shriver Ridge and Wills Mountain in the Valley Road area and extend across Wills Creek to the West Side. There are no current mining operations within the City of Cumberland. The limestone deposits in the Valley Road area and on the West Side have been quarried in the past. Outside of the City limits, there is an active sandstone mining operation on the northwest slope of Wills Mountain. This operation does not currently affect views of Wills Mountain from Cumberland. There is historic evidence that drilling for natural gas was unsuccessfully conducted in the Narrows at one time. However, the lithology of this area indicates that it is unlikely to be a potential source of natural gas. Issues: • Mineral extraction is not a use compatible with Cumberland's position as a regional urban center. Less developed areas of Allegany County have ample deposits to meet regional needs for mineral resources. Moreover, the mineral resources in Cumberland occur in association with landforms (Shriver Ridge, Haystack Mountain, and Wills Mountain) that are important to the City's visual setting. Mineral extraction is not currently a permitted use in any zoning district within Cumberland. • It is possible that mining on the northwest side of Wills Mountain could affect views of the mountain from Cumberland over the long term, depending upon the extent of future extraction and its potential to undermine slopes along the ridgetop.
    [Show full text]
  • Bedford County Parks, Recreation and Open Space Plan
    Bedford County Parks, Recreation and Open Space Plan December 18, 2007 Adopted by the Bedford County Board of Commissioners Prepared by the Bedford County Planning Commission With technical assistance provided by This plan was financed in part by a grant from the Community Conservation Partnership Program, Environmental Stewardship fund, under the administration of the Pennsylvania Department of Conservation and Natural Resources, Bureau of Recreation and Conservation. Intentionally Blank Table of Contents Introduction ............................................................................................................................................1-1 Plan Purpose and Value Planning Process Plan Overview by Chapter Setting and Study Area.........................................................................................................................2-1 Regional Setting County Characteristic and Trends Major Communities and Corridors Significant and Sizable Features Development and Conservation Policy Open Space Resources.............................................................................................................. 3-1 Sensitive Natural Resources Resources for Rural Industries Resources for Rural Character Regulation and Protection of Natural Resources Conclusions and Options Parks & Recreation Facilities ................................................................................................... 4-1 State Parks and Recreation Resources Local Public Park and Recreation Facility Assessment Analysis
    [Show full text]
  • View of Valley and Ridge Structures from ?:R Stop IX
    GIJIDEBOOJ< TECTONICS AND. CAMBRIAN·ORDO'IICIAN STRATIGRAPHY CENTRAL APPALACHIANS OF PENNSYLVANIA. Pifftbutgh Geological Society with the Appalachian Geological Society Septembet, 1963 TECTONICS AND CAMBRIAN -ORDOVICIAN STRATIGRAPHY in the CENTRAL APPALACHIANS OF PENNSYLVANIA FIELD CONFERENCE SPONSORS Pittsburgh Geological Society Appalachian Geological Society September 19, 20, 21, 1963 CONTENTS Page Introduction 1 Acknowledgments 2 Cambro-Ordovician Stratigraphy of Central and South-Central 3 Pennsylvania by W. R. Wagner Fold Patterns and Continuous Deformation Mechanisms of the 13 Central Pennsylvania Folded Appalachians by R. P. Nickelsen Road Log 1st day: Bedford to State College 31 2nd day: State College to Hagerstown 65 3rd day: Hagerstown to Bedford 11.5 ILLUSTRATIONS Page Wagner paper: Figure 1. Stratigraphic cross-section of Upper-Cambrian 4 in central and south-central Pennsylvania Figure 2. Stratigraphic section of St.Paul-Beekmantown 6 rocks in central Pennsylvania and nearby Maryland Nickelsen paper: Figure 1. Geologic map of Pennsylvania 15 Figure 2. Structural lithic units and Size-Orders of folds 18 in central Pennsylvania Figure 3. Camera lucida sketches of cleavage and folds 23 Figure 4. Schematic drawing of rotational movements in 27 flexure folds Road Log: Figure 1. Route of Field Trip 30 Figure 2. Stratigraphic column for route of Field Trip 34 Figure 3. Cross-section of Martin, Miller and Rankey wells- 41 Stops I and II Figure 4. Map and cross-sections in sinking Valley area- 55 Stop III Figure 5. Panorama view of Valley and Ridge structures from ?:r Stop IX Figure 6. Camera lucida sketch of sedimentary features in ?6 contorted shale - Stop X Figure 7- Cleavage and bedding relationship at Stop XI ?9 Figure 8.
    [Show full text]
  • Wills Creek Preassessment
    Wills Creek Preassessment Eric Null Len Lichvar Produced by Somerset Conservation District, 6024 Glades Pike Road Suite 103, Somerset, PA 1 2 Wills Creek Preassessment Eric Null Len Lichvar March 2010 Somerset Conservation District Funding for this project provided by the Foundation for Pennsylvania Watersheds With special assistance from the Pennsylvania Fish and Boat Commission Photos by Len Lichvar, Eric Null, and Amanda Deal Copies of this report may be obtained by contacting the Somerset Conservation District 6024 Glades Pike Road, Suite 103 Somerset, PA 15501 Phone (814) 445-4652 ext.5 Fax (814) 445-2044 E-mail [email protected] Report text may be accessed on the Somerset Conservation District Website http://www.somersetcd.org/ 3 Table of Contents Forward/Acknowledgements………...……………………………………………….7 Introduction………………………………………………………..………………….8 Methods………………………………………………………………………………10 Results…………………………………………………..…………………………....14 Discussion…………………………………………..………………………………..29 Recommendations …………………………………….…………………………….30 Literature Cited……………………………………….……………………………...31 Appendix 1— Macroinvertebrates collected at each site Appendix 2—Fishes collected at each site Wills Creek Sampling Station 5 4 List of Figures Figure 1. The Wills Creek watershed………………………………………………………....8 Figure 2. Wills Creek Preassessment sampling points…………………………………...….11 Figure 3. Macroinvertebrate species richness of the Wills Creek Watershed……………….15 Figure 4. Shannon-Weaver Diversity Index for the macroinvertebrates communities of the Wills Creek Watershed……………………………………………………..16 Figure 5. HBI scores for the Wills Creek watershed………………………………………....17 Figure 6. Percent EPT taxa in the Wills Creek watershed…………………………………....18 Figure 7. Percent Dominant taxa in the Wills Creek watershed……………………………...18 Figure 8. Percent acid tolerant taxa in the Wills Creek watershed…………………………...19 Figure 9. Fish species richness in the Wills Creek watershed ………………………………..21 Figure 10. Shannon-Weaver diversity index for fish communities in the Wills Creek Watershed…………………………………………………………………...22 Figure 11.
    [Show full text]
  • Geologic Cross Section C–C' Through the Appalachian Basin from Erie
    Geologic Cross Section C–C’ Through the Appalachian Basin From Erie County, North-Central Ohio, to the Valley and Ridge Province, Bedford County, South-Central Pennsylvania By Robert T. Ryder, Michael H. Trippi, Christopher S. Swezey, Robert D. Crangle, Jr., Rebecca S. Hope, Elisabeth L. Rowan, and Erika E. Lentz Scientific Investigations Map 3172 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Ryder, R.T., Trippi, M.H., Swezey, C.S. Crangle, R.D., Jr., Hope, R.S., Rowan, E.L., and Lentz, E.E., 2012, Geologic cross section C–C’ through the Appalachian basin from Erie County, north-central Ohio, to the Valley and Ridge province, Bedford County, south-central Pennsylvania: U.S. Geological Survey Scientific Investigations Map 3172, 2 sheets, 70-p.
    [Show full text]
  • Structural Geology of the Transylvania Fault Zone in Bedford County, Pennsylvania
    University of Kentucky UKnowledge University of Kentucky Master's Theses Graduate School 2009 STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA Elizabeth Lauren Dodson University of Kentucky, [email protected] Right click to open a feedback form in a new tab to let us know how this document benefits ou.y Recommended Citation Dodson, Elizabeth Lauren, "STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA" (2009). University of Kentucky Master's Theses. 621. https://uknowledge.uky.edu/gradschool_theses/621 This Thesis is brought to you for free and open access by the Graduate School at UKnowledge. It has been accepted for inclusion in University of Kentucky Master's Theses by an authorized administrator of UKnowledge. For more information, please contact [email protected]. ABSTRACT OF THESIS STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA Transverse zones cross strike of thrust-belt structures as large-scale alignments of cross-strike structures. The Transylvania fault zone is a set of discontinuous right-lateral transverse faults striking at about 270º across Appalachian thrust-belt structures along 40º N latitude in Pennsylvania. Near Everett, Pennsylvania, the Breezewood fault terminates with the Ashcom thrust fault. The Everett Gap fault terminates westward with the Hartley thrust fault. Farther west, the Bedford fault extends westward to terminate against the Wills Mountain thrust fault. The rocks, deformed during the Alleghanian orogeny, are semi-independently deformed on opposite sides of the transverse fault, indicating fault movement during folding and thrusting. Palinspastic restorations of cross sections on either side of the fault zone are used to compare transverse fault displacement.
    [Show full text]
  • Where Is (And Was) Pennsylvania?”
    Essay: “Where Is (and Was) Pennsylvania?” W.E. Hamilton D.Y. Sillman Penn State University This work is licensed under a Creative Commons Attribution‐Noncommercial‐No Derivative Works 3.0 license. It may be distributed and shared, with attribution, but not altered or used commercially in any way. “Where Is (and Was) Pennsylvania?” Pennsylvania is a pretty obvious place to us. It’s a rectangular, politically defined piece of the eastern United States with a wiggly eastern border that follows the Delaware River and three, very straight other borders on the north, west, and south that were laboriously marked off after a great deal of social and legal travail and even some violence. It’s a hilly to mountainous, river‐rich place with forests and fields and cities. Its statistics are simple: it is about three hundred miles from east to west and a little less than one hundred and seventy miles from south to north. It comprises 46,058 square miles (although the number “45,308” shows up in some references). Its latitude range is thirty‐nine degrees forty‐three minutes N to forty‐two degrees N, and its longitude range is seventy‐four degrees and forty‐three minutes W to eighty degrees thirty‐one minutes W (Netstate 2008). This Pennsylvania, though, hasn’t always been all of that. The great rectangle of Pennsylvania has been, through the geological history of the Earth, in the southern hemisphere, on the equator, and in a great many places in between. It has been oriented with its long, three hundred mile axis east to west and also with this long axis running south to north.
    [Show full text]
  • Description of the Hollidaysburg and Huntingdon Quadrangles
    DESCRIPTION OF THE HOLLIDAYSBURG AND HUNTINGDON QUADRANGLES By Charles Butts INTRODUCTION 1 BLUE RIDGE PROVINCE topography are therefore prominent ridges separated by deep SITUATION The Blue Ridge province, narrow at its north end in valleys, all trending northeastward. The Hollidaysburg and Huntingdon quadrangles are adjoin­ Virginia and Pennsylvania, is over 60 miles wide in North RELIEF ing areas in the south-central part of Pennsylvania, in Blair, Carolina. It is a rugged region of hills and ridges and deep, The lowest point in the quadrangles is at Huntingdon, Bedford, and Huntingdon Counties. (See fig. 1.) Taken as narrow valleys. The altitude of the higher summits in Vir­ where the altitude of the river bed is about 610 feet above sea ginia is 3,000 to 5,700 feet, and in western North Carolina 79 level, and the highest point is the southern extremity of Brush Mount Mitchell, 6,711 feet high, is the highest point east of Mountain, north of Hollidaysburg, which is 2,520 feet above the Mississippi River. Throughout its extent this province sea level. The extreme relief is thus 1,910 feet. The Alle­ stands up conspicuously above the bordering provinces, from gheny Front and Dunning, Short, Loop, Lock, Tussey, Ter­ each of which it is separated by a steep, broken, rugged front race, and Broadtop Mountains rise boldly 800 to 1,500 feet from 1,000 to 3,000 feet high. In Pennsylvania, however, above the valley bottoms in a distance of 1 to 2 miles and are South Mountain, the northeast end of the Blue Ridge, is less the dominating features of the landscape.
    [Show full text]
  • Early History of Hamiltonban Township (1730 – 1860)
    Early History of Hamiltonban Township (1730 – 1860) The earliest European settlers came to the area in the 1730s. Before 1767, parts of what are now Adams and York Counties were claimed by both Maryland and Pennsylvania. Two disputed settlements in Adams County were "Digges Choice", in the vicinity of Littlestown and Hanover, and "Carroll's Delight," in the vicinity of Fairfield and Hamiltonban. Pennsylvania countered the claims of Maryland for the disputed areas by importing settlers. About 1729 the Governor of Pennsylvania, in order to stop further encroachment on the part of Maryland, sent word to the Penn brothers, sons of William Penn, to send him some fighting men. In response, they sent a colony of one hundred forty families from Ulster, Ireland, led by Captain Hance Hamilton. This colony of Scotch-Irish settlers landed at New Castle, Delaware, August 24, 1729, and went almost immediately to what is now Adams County, where they took up land and began to build their homes. Captain Hance Hamilton had a large family, including two daughters and six sons. One of his sons, also named Hance, became Sheriff of York County. In 1735, the proprietor of Maryland, Lord Baltimore, granted 5,000 acres in what is now Hamiltonban Township to Charles Carroll, who named it Carroll's Delight. In 1741 Archibald Beard, John Withrow, James McGinley and Jeremiah Lochery purchased Carroll's Delight. At that time, the purchasers believed that the land was in Maryland, and it was not until the Mason-Dixon line was surveyed in 1767 that it was determined that Carroll's Delight was actually in Pennsylvania.
    [Show full text]
  • Derry Township Municipal Directory
    i I i i i OFFICIAL I COMPREHENSIVE PbAN i I i DERRY TO WNSHIrlz) I MIFFLIN COUNTY, PA I I ADOPTED: JUNE, I 1997 I I I PREPARED BY: i GEHRINGER-ROTH ASSOCIATES i J I I I I I I I I I I I I 1 I I I ! I I DERRY TOWNSHIP MUNICIPAL DIRECTORY Board of Suwrvisors Planning Commission James F. Ripka, Chairman Maxwell Hook, Chairman John E. McCullough, Vice-chairman Edith Bartha, Secretary Gene W. Gilbert Donald Corbm Margaret M. Stewart, Appointed Secretary Ralph Kearns I Dave Richards I TownshiD Manager Margaret M. Stewart Eneineer Buchart-Horn, Inc. I1 1200 West College Avenue State College, PA 16801-2824 ZoninP Officer Telephone: (814) 237-7111 James L. Treaster Sewape Enforcement Oflicer I Solicitor Robert R. Rosenberry David W. Molek, Esquire 248-3795 P. 0. Box 42 I Burnham,PA 17009 Telephone: 248-%56 I DERRY TOWNSHIP MUNICIPAL OFFICE I P. 0. Box M Yeagertown, PA 17099 I Telephone: (717) 248-8151 FAX: (717) 248-0063 Hours: 8 A.M.- 12 P.M. & 1 P.M. - 5 P.M. (Monday - Friday) I I A I Gehringer-Roth Associates COMMUNITY PUNNING CONSULTAN'IS Eden Road. Lsaerter. PA 17601 I (717) X&XL?2. I I .I TABLE OF CONTENTS I. INTRODUCTION ............................................. 1 ~I A. Purpose ofthe Plan ..................................................... 1 B . HowtoUseThisPlan ................................................... 2 I C. Regional Context ....................................................... 3 D . HistoricSketch ........................................................ 3 I I1 . COMMUNITY PLANNING GOALS AND I ATLlTUDINAL SURVEY RESULTS
    [Show full text]
  • A NATURAL HERITAGE INVENTORY of MIFFLIN COUNTY, PENNSYLVANIA June 2007
    A NATURAL HERITAGE INVENTORY OF MIFFLIN COUNTY, PENNSYLVANIA June 2007 Prepared by: Pennsylvania Natural Heritage Program Western Pennsylvania Conservancy 208 Airport Drive Middletown, Pennsylvania 17057 Submitted to: Mifflin County Planning Commission 20 North Wayne Street Lewistown, PA 17044 This project was funded in part by a state grant from the Department of Conservation and Natural Resources Wild Resource Conservation Program. Additional support was provided by the Department of Community & Economic Development. Additional funding was provided by the U.S. Fish and Wildlife Service through State Wildlife Grants program grant T-2, administered through the Pennsylvania Game Commission and the Pennsylvania Fish and Boat Commission. ii A Natural Heritage Inventory of Mifflin County, Pennsylvania 2007 Prepared by: Pennsylvania Natural Heritage Program (PNHP) Western Pennsylvania Conservancy (WPC) 208 Airport Drive Middletown, PA 17057 Donna Bowers, Administration Lucy Boyce, Seasonal Field Ecologist Anthony F. Davis, Senior Ecologist Jeremy Deeds, Aquatic Zoology Coordinator Alice Doolittle, Conservation Assistant Charlie Eichelberger, Herpetologist Kathy Derge Gipe, Herpetologist William (Rocky) Gleason, County Inventory Coordinator Jim Hart, Mammalogist Rita Hawrot, Terrestrial Zoology Coordinator Denise Johnson, Assistant County Inventory Ecologist Susan Klugman, Conservation Information Manager John Kunsman, Senior Botanist Betsy Ray Leppo, Invertebrate Zoologist Trina Morris, County Inventory Ecologist Betsy Nightingale, Aquatic
    [Show full text]