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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. -
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. -
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. -
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. -
Watershed 11A, Little Juniata River
08/22/01 DEP Bureau of Watershed Management Watershed Restoration Action Strategy (WRAS) State Water Plan Subbasin 11A Little Juniata River and Frankstown Branch Watersheds Blair, Huntingdon, Bedford, Cambria, and Centre Counties Introduction The 738-square mile Subbasin 11A consists of two major parts, the 395-square mile Frankstown Branch of the Juniata River watershed and its major tributaries Beaverdam Branch, Blair Gap Run, Canoe Creek, Piney Creek, and Clover Creek, and the 343-square mile Little Juniata River watershed and its major tributaries, Bald Eagle Creek, Sinking Creek, and Spruce Creek. A total of 1,051 streams flow for 1,314 miles through the subbasin. The subbasin is included in HUC Area 2050302, Upper Juniata River, a Category I, FY99/2000 Priority watershed under the Unified Watershed Assessment developed by the Department in 1998. The Frankstown Branch and the Little Juniata River join to form the man stem Juniata River at the eastern edge of the subbasin. Geology/Topography The topography and geology of the subbasin is varied, as is typical of the Ridge and Valley Ecoregion, which comprises most of the subbasin. This area consists of a series of narrow northeast-southwest trending ridges and steep, narrow valleys formed during the uplift of the Appalachian Mountain chain. Most of the mountains are folded into tight loops and form dead- end valleys. The numerous folds in the mountains result in repetition of rock types throughout the basin, with sandstone-quartzite on the ridges and limestone and shale in the valleys. The steeply sloping topography can lead to increased runoff during storm events and discourage infiltration to the groundwater. -
Illustration.Pdf
exio GENERALIZED SECTION OF THE ROCKS IN THE HOLLIDAYSBURG AND HUNTINGDON QUADRANGLES SCALE: 1 INCH = 1000 FEET SYSTEM SERIES GROUP THICKNESS FORMATION. SYMBOL SECTION IN FEET MINOR DIVISIONS CHARACTER OF MEMBERS GENERAL CHARACTER OF FORMATIONS PENNSYL- Brookville coal member. Probably 41 to 5 feet thick. Impure; inferior quality. Shale and sandstone with workable coal beds. VANIAN Allegheny formation. Ca ^-^^50 Homewood sandstone member Coarse thick -bedded sandstone. Mercer shale member Clay, coal, and shale 130 300 Mainly coarse sandstone with shale, coal, and clay in middle. Pottsville formation Cpv ^JcrorgTqoijuuuuiMranacxx Connoquenessing sandstone member. Coarse thick-bedded sandstone. _ -~ '~^^~^~=^ In Hollidaysburg quadrangle coarse, lumpy, red and green shale, mostly red; 80 feet of sandstone at bottom. CARBONIFEROUS Mauch Chunk formation. Cmc 180-1000 In Huntingdon quadrangle a little yellowish-green sandstone in midst of red shale and at top; at bottom, V-'i' -V-' r'-'i'.v: 'i ' '!' ' Trough Creek limestone member, red and gray, coarsely crystalline. ~~~~^-- _ ^&>;&^:^&;& Siliceous cross-bedded limestone. (Cb) (300-500) Burgoon sandstone member Rather coarse micaceous, arkosic yellowish or greenish-gray thick-bedded MISSISSIPPI sandstone. Patton shale member. _- - - -- - Red shale on Allegheny Front and westward. Pocono formation. Cpo 990 Lower 700 feet in Hollidaysburg quadrangle, shale and sandstone, considerable red shale. Lower 900 feet in Huntingdon quadrangle, shale, sandstone, and conglomerate, very little red shale. Shale mostly stiff, imperfectly fissile, greenish. ^-j-i-^-'. ' "*" '.. '' _» =y^=-^-- "ZZT??*?1^^ - .-T^ ' ' - ' ' ' ^ About 80 percent bright red shale, alternating with layers of reddish or brown sandstone, which is generally 8000- thick-bedded and medium-grained. Some laminated layers. The red .shale is in places mottled with Hampshire formation. -
Bedford County Natural Heritage Inventory, 1998
BEDFORD COUNTY NATURAL HERITAGE INVENTORY Prepared for: The Bedford County Planning Commission Russell Building, 203 S. Juliana Street Bedford, PA 15522 Prepared by: Western Pennsylvania Conservancy 209 Fourth Avenue Pittsburgh, Pennsylvania 15222 September 1998 This project was funded by the Department of Conservation and Natural Resources, Bureau of Recreation and Conservation, by the Southwestern Pennsylvania Heritage Preservation Commission under the Grant Agreement #GA-4174-6-0024 and by the Western Pennsylvania Conservancy. Cover illustration: Topographic Settings map of Bedford County – hilltop upper slope lower slope valley bottom . Source: Bedford County Planning Commission. Printed on recycled paper PREFACE The Bedford County Natural Heritage Inventory identifies and maps Bedford County’s most significant natural places. The study investigated plant and animal species and natural communities that are unique or uncommon in the county; it also explored areas important for general wildlife habitat and scientific study. The inventory does not confer protection to any of the areas listed in the report. It is, however, a tool for informed and responsible decision-making. Public and private organizations may use the inventory to guide land acquisition and conservation decisions. Local municipalities and the County may use it to help with comprehensive planning, zoning and the review of development proposals. Developers, utility companies and government agencies alike may benefit from access to this environmental information prior to the creation of detailed development plans. Although the inventory was conducted using a tested and proven methodology, it is best viewed as a preliminary report rather than the final word on the subject of Bedford County’s natural heritage. -
Geology and Mineral Resources of the Bellefonte Quadrangle, Pennsylvania
PLEASE DO NOT DESTROY OR THROW AWAY THIS PUBLICATION. If you have no further use for it, write to the Geological Survey at Washington and ask for a frank to return it UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGY AND MINERAL RESOURCES OF THE BELLEFONTE QUADRANGLE, PENNSYLVANIA GEOLOGICAL SURVEY BULLETIN 855 UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 855 GEOLOGY AND MINEEAL BESOUECES OF THE BELLEFONTE QUADRANGLE, PENNSYLVANIA BY CHARLES BUTTS AND ELWOOD S. MOORE UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1936 For sale by the Superintendent of Documents, Washington, D. C. -------- Price 50 cents CONTENTS Page Abstract ___ -- 1 Introduction ._________________________________________________ 4 Location and area___-__--_---_-_------________________________ 4 Appalachian Highlands___-_______----_________________________ 4 Piedmont province._______________________________________ 5 Blue Ridge province ---_--_------_-__-__..-_-_-.________ 5 Valley and Ridge province_ _--___._______________ 6 Appalachian Plateaus____________________________________ 7 Drainage of the Appalachian Highlands____-__----_-_-_-.____ 8 Topography....--...- _------__--_--_____ . _ _ .... 8 General features.._______.______________ 8 Relief____ --- ---------------- ___-____------. ._ 9 Allegheny Plateau and Allegheny Mountains-_--_-----_______ 9 Bald Eagle Mountain____________________________________ 9 Nittany Mountain._______________________________________ 9 Tussey Mountain___-_____-__--___-________.______________ -
Juniata River Water Trail (Miles Correspond to River Mileage on Map)
ALONG THE WAY– UPPER JUNIATA RIVER WATER TRAIL (MILES CORRESPOND TO RIVER MILEAGE ON MAP) Frankstown Branch Mile 94, Portstown Park Access (river left) - This Huntingdon Juniata River Mile 126, Canoe Creek State Park- This 958-acre park contains a 155- Borough park was once part of Huntingdon’s commercial waterfront. acre lake that provides excellent year-round fishing, a popular swimming Today, the park features a pavilion, walking trail, playground, skate area, and access for small pleasure boats. Hiking trails are available for park, and a safe connection into downtown Huntingdon and Rothrock hikers, bicyclists, and equestrians. Outfitters. Miles 126-107, Lower Trail- This multi-use rail-trail runs 17 miles Mile 94-93.5, Huntingdon Historic District- National Register Water Trail between Flowing Spring and Alfarata. For more information, contact Rails- buildings dating from the 18th century include the Huntingdon County to-Trails of Central PA., Inc. at www.rttcpa.org Jail, the Huntingdon County Courthouse, and the J.C. Blair Building, Mile 123.5-123, Point View Gap- 900-foot-deep water gap in Lock which at one time was the tallest building between Philadelphia and Upper Section Mountain. Pittsburgh. A walking tour brochure is available from the historical Mile 123, Former Three-Mile Dam- A cut stone masonry vestige of society. Three-Mile Dam is located along the south side of SR 866 at Ganister. This Mile 93, Smithfield Riverside Park Access- Features pavilions, abutment, on the north side of the Juniata River, measures about 50 feet tables, grills, restroom, playground, grass area, horseshoe pits, and a long. -
Bedford County
ON THE ROAD Highways and History in Bedford County For thousands of years the Snake Spring Valley of Bedford County Pennsylvania Department has been a vital transportation corridor through the mountains of of Transportation south-central Pennsylvania. The Snake Spring Valley contains a series of important historic trails and roads, each built on the remains of those that came before. From early native trails to the modern Pennsylvania Turnpike, each resulted from steady improvements in technology and the public’s desire for increased mobility, speed, and convenience. Although many of the early routes were obliterated by later development, traces still survive in the landscape. Recent historical and archaeological studies completed in connection with improvements to US Route 30 provided an opportunity to rediscover the area’s fascinating transportation history. ® ISBN 0-89271-119-5 Scott D. Heberling and William M. Hunter ON THE ROAD Highways and History in Bedford County Scott D. Heberling and William M. Hunter Heberling Associates, Inc. Commonwealth of Pennsylvania Pennsylvania Historical and Museum Commission for the Pennsylvania Department of Transportation 2006 Commonwealth of Pennsylvania Edward G. Rendell, Governor Federal Highway Administration-Pennsylvania Division James A. Cheatham, Division Administrator Pennsylvania Department of Transportation Allen D. Biehler, Secretary Pennsylvania Historical and Museum Commission Wayne S. Spilove, Chair Barbara Franco, Executive Director Joe Baker, Series Editor Photographs courtesy of -
Ski Well, Be Well
SKI WELL, BE WELL SKI AREA OPERATING BEST PRACTICES WINTER 2020-21 FOUNDED IN 1962, THE NATIONAL SKI AREAS ASSOCIATION serves as the trade association for over 320 alpine resorts that account for more than 90 percent of skier/ snowboarder visits nationwide. NSAA is responsible for promoting foundational best practices for the ski industry, including the nationally-accepted Your Responsibility Code, which defines the basic tenets of slope safety. The ski industry’s stable of experts develops best practices for ski, snowboard, and lift safety. OUR COMMITMENT “The ski industry led the business community last spring with our The ski and snowboard industry values and prioritizes responses to the Covid outbreak the health and safety of its guests, staff and local and intends to lead again with communities. We demonstrate this commitment to our providing responsible and safe stakeholders by implementing the following operating outdoor winter recreation for best practices for the 2020-21 winter season, or for as millions of people this next winter.” long as needed, scaled appropriately in response to the Stephen Kircher, CEO/President, COVID-19 pandemic. Boyne Resorts Ski industry leaders from across the country established these foundational best practices according to scientific guidelines put forth by infectious disease experts, including the CDC and WHO. Ski areas will comply with additional federal, state and local regulations as they are implemented. Ski areas are committed to Snowsports are a way for people to play in wide-open supporting healthy and thriving spaces, and to take advantage of the mental and physical local communities. We will continue health benefits of outdoor recreation.