Modeling Raptor Migration Pathways Using A
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Simple Maps of the Pennsylvania Turnpike System
The Pennsylvania Turnpike Website: www.paturnpike.com Customer Service: 800.331.3414 (Outside U.S., call 717.831.7601) Travel Information: Dial 511 within PA Emergency Assistance or 1-877-511-PENN(7366) (877.736 .6727) when calling from outside of PA, Customer Service *11on the Pennsylvania Turnpike or visit www.511pa.com (Outside U.S., call 717-561-1522) *Gateway Toll Plaza (#2) near Ohio is a one-way toll facility. No toll is charged for westbound travel into Ohio, but there is an eastbound toll to enter Delmont Greensburg Pennsylvania via Gateway. The one-way tolling Bypass conversion was required to ease congestion and 66 allow installation of Express E-ZPass lanes. 14 Murrysville 22 Blairsville Sheffield D r. 66 12 BUS Sharon, Beaver Valley 66 Youngstown Expressway Harrison City 993 9 BUS Greensburg 376 15 66 422 Butler 8 Jeannette 130 Greensburg 376 6 Irwin 30 Greensburg 17 Mt. Jackson 108 New Castle Mainline Toll Zone 4 Mainline Toll Zone West Newton 136 Greensburg 20 New Galilee 168 Moravia 1 Erie Arona Rd. 351 Butler Ligonier Murrysville New Kensington Johnstown Greensburg 119 19 0 26 Elwood City ALLEGHENY 28 PITTSBURGH IRWIN DONEGAL 711 SOMERSET VALLEY 22 57 30 NEW STANTON 601 48 67 New Stanton Service Plaza 91 110 N.Somerset Service Plaza Allegheny Tunnel Warrendale Toll Plaza Allegheny River Allegheny Gateway Toll Plaza (Eastbound Only)* 75 Beaver River Beaver 49 To Central Section 76 70 76 Ohio 2 30 78 NEW BEAVER CRANBERRY BUTLER 112 of the map CASTLE 18 VALLEY 28 VALLEY 70 119 31 10 13 8 39 29 79 376 Darlington 551 Beaver -
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. -
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 -
Sideling Hill Creek Preserve Visitors Guide
Maryland Preserve Guide Sideling Hill Creek, Allegany County Sideling Hill Creek originates from the southwestern mountains of Pennsylvania, winding its way among the steep, forested shale cliffs of western Maryland before finally spilling into the Potomac River. It is one of the most pristine streams in Maryland, and helps support the Nature Conservancy Nature state’s healthiest population of the globally-rare The The aquatic wildflower Harperella. The rare shale barren communities are another unique feature of this preserve. There are twelve rare, endemic Sideling Hill Creek is one of the most (occurring in the shale barrens and nowhere else) pristine aquatic communities in its region. plants here including the nationally-endangered evening primrose, shale ragwort, and Kate’s mountain clover. The preserve also has many different animals, such as the Olympian marble butterfly, green Key Elements floater mussel, and tiger beetle. Other animals include wild turkey, hawks, and bobcat. Harperella Rare shale barren communities Fun Facts About Sideling Hill Evening primrose The Sideling Hill watershed is about 80% forest cover, Olympian marble butterfly and is incredibly intact because there are no urban centers or industry, and the area is sparsely populated. This isolation has allowed Sideling Hill Creek to have supremely high water quality and healthy aquatic communities. Due to the hydrology of the shale barrens, the water level in this clean creek is highly variable. This variability is common for water bodies near shale barrens, but Sideling Hill Creek is exceptionally variable. It has seven species of freshwater mussels and 40 species of fish. Throughout the preserve, there are also a number of ephemeral streams. -
Pennsylvania
Elton 243 13A Road Ithaca Harford 36 54A 226 220 Dayton 390 14 79 11 41 80° 30’ 80° 15’ 80° 00’ 79° 45’ 79° 30’ Toll 79° 15’ 79° 00’ 78° 45’ 78° 30’Machias 78° 15’ 78° 00’ 77° 45’ 77° 30’ 77° 15’ 77° 00’ 76° 45’ 76° 30’ 76° 15’ 76° 00’ 75° 45’ 75° 30’ 75° 15’ 75° 00’ 74° 45’ 74° 30’ Houghton 53 414 5 38 21 Haskinville 327 26 A B C D E F G H J K 3 L M N 1 O P Q R S T U V W X Y Z To Buffalo East Otto Rushford Arkport Avoca 36 2 54 Hammondsport Caroline 219 Caneadea 3 96B Whitney 60 83 Hamlet South 62 243 Watkins 10 20 Cassadaga 240 98 Birdsall 10 415 37 13 79 Point 7 90 Dayton 16 2 86 35 7 Glen 3 Montour 228 THESE Bloomville Bear 322 5 Wesley Lake 41 12 TOURISM AND TRANSPORTATION28 MAP Lakes 353 242 17 79 Barcelona Lake Belfast 3 Falls Danby Center Lisle Triangle 206 Unadilla Franklin Cassadaga 6 34 329 Newfield Lisle 60 Howard Richford 11 357 Tom Wolf, Governor 1 1 2 19 Bath Townsend 224 QUICK RESPONSE 8 Greene CoventryPA Sidney PA 5 5 3 33 Hornell 38 Sonora 29 34 2 Whitney Point 41 10 Westfield Charlotte Cattaraugus Franklinville Odessa 206 Stockton 9 96 Yassmin Gramian, P.E., Secretary, Department of Transportation Center Cherry Ashford Almond 4 30 9 Creek Angelica 32 Speedsville Itaska visitPA.com41 Bainbridge visitPA.com STATE 17 7 226 Monterey 414 CODES N 394 Leon 8 42 39 5 8 88 9 Delhi Forsyth 21 86 Willseyville ROAD CLASSIFICATION AND ROUTE MARKERS KEY TO MAP SYMBOLS 61 6 New 36 3 Beaver Dams 7 20 PARKSAlbion 5 Nanticoke TRAFFIC INTERCHANGES 28 ? Hartfield 27 353 31 Alfred Savona 16 CAN BE USEDJenksville Glen 7 PASSENGER RAILROADS -
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. -
The RPI Website 10
10 The RPI Website Jason Sodergren Abstract.—Hawkcount.org is an online database system that provides data submission, reporting, and storage services for hawk migration watchsites. Here, I outline current features of the online database system, implementation details, and plans for future system develop- ment. Hawkcount.org is an online database system that provides count and observation data entry, storage, and reporting services for migration watchsites. This system was implemented in 1999–2000 as a single-site data reporting system for the Holiday Beach Migration Observatory watchsite near Amherstburg, Ontario, Canada. This early version pro- vided functionality related to daily reporting of observed raptor counts at the site. Results were made available immediately on the Holiday Beach web site, and automated e-mail reports were submitted daily to various mailing lists, including the BIRDHAWK list maintained by the Hawk Migration Association of North America (HMANA), regional bird-related mailing lists, and others. One of the primary goals of the original system involved the simplifi - cation of the hawk counters’ daily reporting tasks, including eliminating the need to submit hard-copy daily paper forms. Each day, the counter (or other site representative) “reported” the day’s results to several places, including a hard-copy daily report form or HMANA “greensheet” to be submitted to HMANA, various e-mail lists, and the Autumn HawkWatch system, an internet-based database system that, as the result of collabora- tion among Hawk Mountain Sanctuary, the Cornell Lab of Ornithology, and the Hawk Migration Association of North America, provided a database of Hawk Migration Association of North America, P.O. -
1 I-68/I-70: a WINDOW to the APPALACHIANS by Dr. John J
I-68/I-70: A WINDOW TO THE APPALACHIANS by Dr. John J. Renton Dept. of Geology & Geography West Virginia University Morgantown, WV Introduction The Appalachian Mountains are probably the most studied mountains on Earth. Many of our modern ideas as to the origin of major mountain systems evolved from early investigations of the Appalachian region. The Appalachians offer a unique opportunity to experience the various components of an entire mountain system within a relatively short distance and period of time. Compared to the extensive areas occupied by other mountain systems such as the Rockies and the Alps, the Appalachians are relatively narrow and can be easily crossed within a few hours driving time. Following I-68 and I-70 between Morgantown, WV, and Frederick, Maryland, for example, one can visit all of the major structural components within the Appalachians within a distance of about 160 miles. Before I continue, I would like to clarify references to the Allegheny and Appalachian mountains. The Allegheny Mountains were created about 250 million years ago when continents collided during the Alleghenian Orogeny to form the super-continent of Pangea (Figure 1). As the continents collided, a range of mountains were created in much the same fashion that the Himalaya Mountains are now being formed by the collision of India and Asia. About 50 million years after its Figure 1 1 creation, Pangea began to break up with the break occurring parallel to the axis of the original mountains. As the pieces that were to become our present continents moved away from each other, the Indian, Atlantic, and Arctic oceans were created (Figure 2). -
Wild Trout Waters (Natural Reproduction) - September 2021
Pennsylvania Wild Trout Waters (Natural Reproduction) - September 2021 Length County of Mouth Water Trib To Wild Trout Limits Lower Limit Lat Lower Limit Lon (miles) Adams Birch Run Long Pine Run Reservoir Headwaters to Mouth 39.950279 -77.444443 3.82 Adams Hayes Run East Branch Antietam Creek Headwaters to Mouth 39.815808 -77.458243 2.18 Adams Hosack Run Conococheague Creek Headwaters to Mouth 39.914780 -77.467522 2.90 Adams Knob Run Birch Run Headwaters to Mouth 39.950970 -77.444183 1.82 Adams Latimore Creek Bermudian Creek Headwaters to Mouth 40.003613 -77.061386 7.00 Adams Little Marsh Creek Marsh Creek Headwaters dnst to T-315 39.842220 -77.372780 3.80 Adams Long Pine Run Conococheague Creek Headwaters to Long Pine Run Reservoir 39.942501 -77.455559 2.13 Adams Marsh Creek Out of State Headwaters dnst to SR0030 39.853802 -77.288300 11.12 Adams McDowells Run Carbaugh Run Headwaters to Mouth 39.876610 -77.448990 1.03 Adams Opossum Creek Conewago Creek Headwaters to Mouth 39.931667 -77.185555 12.10 Adams Stillhouse Run Conococheague Creek Headwaters to Mouth 39.915470 -77.467575 1.28 Adams Toms Creek Out of State Headwaters to Miney Branch 39.736532 -77.369041 8.95 Adams UNT to Little Marsh Creek (RM 4.86) Little Marsh Creek Headwaters to Orchard Road 39.876125 -77.384117 1.31 Allegheny Allegheny River Ohio River Headwater dnst to conf Reed Run 41.751389 -78.107498 21.80 Allegheny Kilbuck Run Ohio River Headwaters to UNT at RM 1.25 40.516388 -80.131668 5.17 Allegheny Little Sewickley Creek Ohio River Headwaters to Mouth 40.554253 -80.206802 -
Summary of Sexual Abuse Claims in Chapter 11 Cases of Boy Scouts of America
Summary of Sexual Abuse Claims in Chapter 11 Cases of Boy Scouts of America There are approximately 101,135sexual abuse claims filed. Of those claims, the Tort Claimants’ Committee estimates that there are approximately 83,807 unique claims if the amended and superseded and multiple claims filed on account of the same survivor are removed. The summary of sexual abuse claims below uses the set of 83,807 of claim for purposes of claims summary below.1 The Tort Claimants’ Committee has broken down the sexual abuse claims in various categories for the purpose of disclosing where and when the sexual abuse claims arose and the identity of certain of the parties that are implicated in the alleged sexual abuse. Attached hereto as Exhibit 1 is a chart that shows the sexual abuse claims broken down by the year in which they first arose. Please note that there approximately 10,500 claims did not provide a date for when the sexual abuse occurred. As a result, those claims have not been assigned a year in which the abuse first arose. Attached hereto as Exhibit 2 is a chart that shows the claims broken down by the state or jurisdiction in which they arose. Please note there are approximately 7,186 claims that did not provide a location of abuse. Those claims are reflected by YY or ZZ in the codes used to identify the applicable state or jurisdiction. Those claims have not been assigned a state or other jurisdiction. Attached hereto as Exhibit 3 is a chart that shows the claims broken down by the Local Council implicated in the sexual abuse.