Geology Field Trips in the Appalachian Mountains
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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 -
BACKPACKING Explore the Great Allegheny Passage with Us! We Will Pedal a Total of 30 Miles out and Back Along the GAP
April – June 2017 Schedule VENTURE OUTDOORS TRAILHEAD Everyone Belongs Outdoors! Board of Directors Did You Know… Alice Johnston, Board Chair Venture Outdoors is a 501(c)3 charitable nonprofit organization. We believe everyone Amanda Beamon, Vice Chair deserves the chance to experience how incredibly fun the outdoors can be, so we provide Darlene Schiller, Co-Secretary the gear, guidance and inspiration to make outdoor recreation part of people’s lives. Robert J. Standish, Co-Secretary Drew Lessard, Treasurer We believe everyone belongs outdoors! Todd Owens, Past Chair Abby Corbin Dennis Henderson David Hunt Support Venture Outdoors and Save with a Yearly Membership Lindsay Patross Go to ventureoutdoors.org/join-us or call 412.255.0564 x.224 to become a New or Marty Silverman Geoff Tolley Renewing Venture Outdoors Member. W. Jesse Ward Your Support Helps Venture Outdoors: David Wolf Membership Levels Student / Senior – $15 • Fund the outings and events that Staff Individual – $25 get you and your family outdoors year-round Joey–Linn Ulrich, Executive Director Dual – $35 Family – $50 • Enable underserved children to PROGRAM DEPARTMENT Trailblazer – $75 learn more about nature and the Lora Woodward, Director environment while developing Paddler – $100 Liz Fager, Community Program Manager outdoor recreation skills Jim Smith, Equipment and Facilities Manager Ranger – $125 Lora Hutelmyer, Youth Program Manager Steward – $250 • Turn volunteers into accomplished Jake Very, Custom Program Coordinator trip leaders while enhancing their Trustee – $500 Billy Dixon, Program Administrator leadership skills and safety training Ken Sikora, Head Trip Leader Specialist Pathfinder – $1,000 KAYAK PITTSBURGH Benefits to You Include: Vanessa Bashur, Director • Discounts on outings, Kayak Pittsburgh Mike Adams, Equipment and Training rentals and season passes Specialist • Shopping savings at Eddie Bauer DEVELOPMENT AND COMMUNICATIONS and Gander Mountain Donna L. -
Tobacco Settlement Report: FY 2017-18
THE TOBACCO SETTLEMENT ANNUAL REPORT TO THE GENERAL ASSEMBLY JULY 1, 2017 – JUNE 30, 2018 Tom Wolf Teresa D. Miller Governor Secretary of Human Services THE TOBACCO SETTLEMENT ANNUAL REPORT TO THE GENERAL ASSEMBLY JULY 1, 2017 – June 30, 2018 Page Executive Summary 3 Uncompensated Care for Hospitals (2017-2018) 4 Attachment 1 – Hospitals eligible for tobacco payment 7 Attachment 2 – Hospitals qualified to receive UC payments 12 Attachment 3 – Hospitals qualified to receive EE payments 16 Attachment 4 – Hospitals affiliations for tobacco payments 19 Attachment 5 – Hospitals with potential DSH-UPL issues 24 Attachment 6 – Total expenditures for each fiscal year 25 Attachment 7 – Uncompensated care (UC) payment method 28 Home and Community-Based Services to Older Pennsylvanians 30 Chart 1 - Aging Waiver Allocation Direct Service Costs 31 Table 1 - Summary of the Aging Waiver 32 Table 2 - Number of Applicants 33 Table 3 - Funded Individuals (Aging Waiver Program) 35 Table 4 - Total Expenditure by PSA 37 Table 5 - Aging Waiver Costs, Number of Claims and Consumers by Service Category for Fiscal Year 2017-2018 39 Table 6 - Costs, Number of Claims and Number of Unduplicated Consumers by Service Category for FY 2017-2018 40 Table 7 - Average State and Federal Costs per Individual 40 Medical Assistance for Workers with Disabilities (MAWD) 41 2 EXECUTIVE SUMMARY The Commonwealth of Pennsylvania joined 45 other states in November 1998 in a master settlement agreement (MSA) with the tobacco industry, estimated to total $206 billion over the first 25 years. Pennsylvania’s share was estimated to be about $11 billion between the years 2000 and 2025. -
Chapter Title
Centre County Demographics and Travel Patterns The purpose of this chapter is to describe Centre County in terms of demographics, major and minor trip generators, planning and zoning, and travel patterns. This information, when considered relative to the inventory of available transportation modes in Centre County, helps to identify specific areas that present the greatest need for transportation improvements. The large land area of Centre County (almost 1,100 square miles), and the County’s mountain ridges and valleys impact the physical layout of transportation infrastructure. Demographic indicators must also be considered within the context of these geographic attributes. Within this chapter, socioeconomic data at the census tract level from the 2010 US Census, 2009-13 American Community Survey (ACS), and the information from Chamber of Business and Industry of Centre County (CBICC) is presented relative to the following categories: • Population and Density • Vehicle Availability • Income and Poverty • Labor Force and Unemployment • Public Assistance and SSI Income • Educational Attainment • Distribution of Jobs • Distribution of Age 65 and Older Population and Social Security Income • Distribution of Disabled Population • Housing Figure 2, which is a map of census tracts within Centre County, is presented on the following page. Centre County Long Range Transportation Plan 2044 Page II- 1 Centre County Demographics & Travel Patterns Figure 2 A map of Centre County planning regions is presented on the following page as Figure 3. Planning -
Further Paleomagnetic Evidence for Oroclinal Rotation in the Central Folded Appalachians from the Bloomsburg and the Mauch Chunk Formations
TECTONICS, VOL. 7, NO. 4, PAGES 749-759, AUGUST 1988 FURTHER PALEOMAGNETIC EVIDENCE FOR OROCLINAL ROTATION IN THE CENTRAL FOLDED APPALACHIANS FROM THE BLOOMSBURG AND THE MAUCH CHUNK FORMATIONS Dennis V. Kent Lamont-DohertyGeological Observatory and Departmentof GeologicalSciences ColumbiaUniversity, Palisades, New York Abstract.Renewed paleomagnetic investigations of red fromthe Bloomsburg, Mauch Chunk, and revised results bedsof theUpper Silurian Bloomsburg and the Lower recentlyreported for theUpper Devonian Catskill Formation Carboniferous Mauch Chunk Formations were undertaken togetherindicate 22.8•>+_11.9 oof relativerotation, accounting with theobjective of obtainingevidence regarding the for approximatelyhalf thepresent change in structuraltrend possibilityof oroclinalbending as contributing to thearcuate aroundthe Pennsylvania salient. The oroclinalrotation can be structuraltrend of thePennsylvania salient. These formations regardedas a tightenS.*'.3 o/'a lessarcuate depositional package cropout on both limbs of thesalient and earlier, but less thatdeveloped across a basementreentrant, to achievea definitivepaleomagnetic studies on these units indicate that curvaturecloser to that of the earlierzigzag continental margin earlyacquired magnetizations can be recovered. Oriented outline. sampleswere obtained from nine sites on the southern limb of thesalient and eight sites from the northern limb in the INTRODUCTION Bloomsburg.The naturalremanent magnetizations are multivectorial,dominated by a component(B) with a A testof the oroclinehypothesis -
Stratigraphic Framework of Cambrian and Ordovician Rocks in The
Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Medina County, Ohio, through Southwestern and South-Central Pennsylvania to Hampshire County, West Virginia U.S. GEOLOGICAL SURVEY BULLETIN 1839-K Chapter K Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Medina County, Ohio, through Southwestern and South-Central Pennsylvania to Hampshire County, West Virginia By ROBERT T. RYDER, ANITA G. HARRIS, and JOHN E. REPETSKI Stratigraphic framework of the Cambrian and Ordovician sequence in part of the central Appalachian basin and the structure of underlying block-faulted basement rocks U.S. GEOLOGICAL SURVEY BULLETIN 1839 EVOLUTION OF SEDIMENTARY BASINS-APPALACHIAN BASIN U.S. 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 UNITED STATES GOVERNMENT PRINTING OFFICE: 1992 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging in Publication Data Ryder, Robert T. Stratigraphic framework of Cambrian and Ordovician rocks in the central Appalachian Basin from Medina County, Ohio, through southwestern and south-central Pennsylvania to Hampshire County, West Virginia / by Robert T. Ryder, Anita C. Harris, and John E. Repetski. p. cm. (Evolution of sedimentary basins Appalachian Basin ; ch. K) (U.S. Geological Survey bulletin ; 1839-K) Includes bibliographical references. Supt. of Docs, no.: I 19.3:1839-K 1. Geology, Stratigraphic Cambrian. -
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. -
Nittany Valley Fact Sheet.Pub
NITTANY VALLEY REGION UNEMPLOYMENT RATES 7.8% LABOR FORCE DATA 6.2% 5.9% 5.7% 5.5% The majority of residents from the Nittany Valley work 30 4.3% 3.6% minutes or less from their residence and drive to work. 3.8% Nittany Valley has a strong workforce with low unemployment rates. The employees are highly educated with higher percent- ages of high school graduates than the State and Nation. Bellefonte Benner Marion Spring Walker Centre PA U.S. County COMMUTING TO WORK NITTANY VALLEY EDUCATIONAL Drove to Public Worked at ATTAINMENT COMPARISON Work Carpooled Transportation Walked Other Home Bellefonte 73.3% 13.5% 2.7% 8.3% 0.5% 1.6% % Bachelor's % High School Benner 87.5% 8.7% 0.0% 0.0% 0.0% 3.8% Degree or Graduate or Marion 78.8% 11.8% 0.0% 2.1% 0.0% 7.3% Higher Higher Spring 84.1% 9.2% 0.1% 2.8% 0.8% 3.0% Walker 83.0% 11.0% 0.2% 1.7% 1.1% 3.0% U.S. 24.4% 80.4% Nittany Valley 81.1% 10.8% 0.8% 3.7% 0.6% 3.0% Pennsylvania 22.4% 81.9% Nittany Valley 18.3% 82.2% TRAVEL TIME TO WORK 30.0 LABOR FORCE POPULATION 25.0 Not in In Labor Labor 20.0 Force s Force e t u 15.0 Bellefonte 3,240 1,932 n i M Benner 1,850 2,754 10.0 Marion 512 188 Spring 3,356 1,454 5.0 Walker 1,769 767 0.0 Nittany Valley 10,727 7,095 Bellefonte Benner Marion Spring Walker Centre County Prepared by the Centre County Planning & Community Development Office, 2008 Source: U.S. -
U.S. Geological Survey Bulletin 1839-G, H
Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Morrow County, Ohio, to Pendleton County, West Virginia Depositional Environment of the Fincastle Conglomerate near Roanoke, Virginia U.S. GEOLOGICAL SURVEY BULLETIN 1839-G, H i i i I ' i ' i ' X- »-v l^,:^ Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Morrow County, Ohio, to Pendleton County, West Virginia By ROBERT T. RYDER Depositional Environment of the Fincastle Conglomerate near Roanoke, Virginia By CHRYSA M. CULLATHER Chapters G and H are issued as a single volume and are not available separately U.S. GEOLOGICAL SURVEY BULLETIN 1839-G, H EVOLUTION OF SEDIMENTARY BASINS-APPALACHIAN BASIN U.S. 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 UNITED STATES GOVERNMENT PRINTING OFFICE: 1992 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25425 Denver, CO 80225 Library of Congress Cataloging in Publication Data (revised for vol. G-H) Evoluation of sedimentary basins Appalachian basin. (U.S. Geological Survey bulletin ; 1839 A-D, G-H) Includes bibliographies. Supt. of Docs. no.:19.3:1839-G Contents: Horses in fensters of the Pulaski thrust sheet, southwestern Virginia / by Arthur P. Schultz [etc.] Stratigraphic framework of Cam brian and Ordovician rocks in central Appalachian basin from Morrow County, Ohio, to Pendleton County, West Virginia / by Robert T. -
Lock Haven PA Water Street Historic District
Lock Haven PA Water Street Historic District The Water Street Historic District was listed on the National Register of Historic Places in 1973. Portions of the text below were adapted from a copy of the original nomination document. [ †] The lands between the West Branch of the Susquehanna River and the Bald Eagle Creek being especially desirable, due to their fertility and location, attracted those seeking frontier homes, and by 1800 there developed quite a prosperous settlement on the site of the present Lock Haven. Commercial lumbering was started about the time of the completion of the canal (1834). This industry grew in importance throughout the rest of the century. Most of the historic structures in this district remain on their original sites and are well-preserved. The most significant buildings are: The L. A. Mackey House, 1854, is a Federal-Tuscan Transitional, two-story, Flemish bond brick dwelling with the main section measuring 44.5' by 39.5'. The symmetric facade has five windows across the front, a bracketed cornice with dentils (which is carried along the sides of the building), a decorated frieze with five oblong windows, and a deeply recessed entrance with circular paneled door flanked by side lights and topped by a large rectangular space filled with a semi-circular window. This front entrance is framed with a hood supported by heavy brackets and topped with a balustraded balcony. There are twin chimneys in both gable ends of the main section of this building which is close to original and in excellent condition. The David Carskaddon Homestead, 1858, is an Italian Villa style, two-story dwelling, brick with stucco finish and constructed in the form of a Y. -
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. -
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.