View the Plan
Total Page:16
File Type:pdf, Size:1020Kb
Load more
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. -
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. -
A STUDY of the TYRONE - MOUNT Udion LINEAMENT by REMOTE SENSING TECHNIWES and Fleld NIETHQDS
A STUDY OF THE TYRONE - MOUNT UdION LINEAMENT BY REMOTE SENSING TECHNIWES AND FlELD NIETHQDS Con- NAS 5-22822 0. P. Gold, Principal Indga@x ORSER Technical Report 12-77 Office for Ramow Sensing of Earth Resources 219 Electrical Engineering West University Park, PA 16802 Prepared for GODDARD SPACE FLIGHT CENTER Greenbelt, MD 20771 The field invesrigations and much of the analvsis descrihrd in this report were used as the basis for a payer in Crology. submtttrd by Elicharl R. Cnnich to tbe Departmc~~tof ~:t~oscic-~\c~?i, in partial iu!ffllment of the rrqufrrurznts tor tlrc Mastt-r- oi Science Dcgrre. b I r T-nd- r RoonOlk I A S~~M)YOF ms ~RONR- ~\nurWIW LIN~BY December 1977 RBWTS SMSSIUC TECHNIQUS AND FlliLD t4STHWS 6 hnwym-- - r Technical Report 12-?7 J 7. habftd a -@-mQImwwn-amL David P. Gold, Principal Inwe8tigator m , 10. WRk uau Wa e m)a~~mt-#y#mdMem Office for Remote Senaing of Earth Resources 219 Electrical Bngineerin8 West Building rt. bn~nar ~nn\ &. \ The Pennsylvania State Uniwrsi ty NA!! 5-22822 University Park, PA 16802 13 ~*oro@~.om.ndhd~CI tr sponss~lr-v-nd~ddnr Final Report 11 1176-6/30/77 Caddard Space Flight Center I Crecnbelt, ND 20771 4 m.LI Field work was combined with satellite imagery and photography to study the Tyrone - Pkrunt Union lineament in Blair and Huntingdon Counties, central Pennsylvania. This feature, expressed as the valleys containing the Little Juniata and Juniata River: . transgtesscs the nose of the southwest-plunging Nittany Anticlinorium in the western extremity of the Valley ;~ndRidge Province. -
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. -
Alkaline Addition Problems at the Skytop/Interstate-99 Site, Central Pennsylvania1
ALKALINE ADDITION PROBLEMS AT THE SKYTOP/INTERSTATE-99 SITE, CENTRAL PENNSYLVANIA1 Arthur W. Rose and Hubert L. Barnes2 Abstract. In 2002-3, approximately 8x105 m3 of pyrite-bearing Bald Eagle sandstone and Reedsville shale were removed from a large road cut through Bald Eagle Ridge near State College, PA. The rock contained an average of about 4.5% pyrite as veins and fine veinlet networks across 200 m of road cut. Smaller amounts of ZnS and other heavy metal sulfides accompany the pyrite. The rock was placed in 9 nearby locations, including large waste piles and several valley fills, two ‘buttresses” and a lane elevation along about 0.8 km of hillside that was threatening to slide into the road. During excavation of the cut, pyrite was recognized as a potential problem and considerable lime was added as layers to the various piles. Despite the lime addition, highly acidic seeps emerged from the piles and fills, with pH 2.0 to 2.7, Fe 90-1500 mg/L, and acidities as high as 18,000 mg/L (as CaCO3). These results clearly show that addition of lime and other alkaline materials as layers is not effective. In experiments to test remediation methods, Bauxsol slurry was sprayed onto part of the buttress area but failed to prevent continuing acid seepages. Inspection trenches showed little penetration of the Bauxsol, and demonstrated the presence of the added lime as impermeable lime layers within the buttress. Bucket tests of mixtures of alkaline circulating fluidized-bed ash with pyritic rocks, when well mixed, gave alkaline effluents. -
C:\Documents and Settings\David Glick\My Documents\Nitminsoc\2016-Bulletin\NL1611.Wpd
Nittany Mineralogical Society Bulletin Nittany Mineralogical Society, Inc., meeting in State College, Pennsylvania Contact information on back page Editor (see back page): November, 2016 Visit our web site: www.nittanymineral.org David C. Glick November 16th meeting: December 21st NMS Holiday Dinner & Sale The Rogue Kimberlite Dikes in Indiana County, Pennsylvania On Wednesday, Dec. 21, 6:00 p.m., rather than our usual meeting, we’ll have a Holiday Dinner at Quaker by Steak & Lube Restaurant, 501 Benner Pike (across Benner Pike from the Nittany Mall), State College PA 16801. Dr. David P. Gold and others (see page 4) NMS will pay for appetizer plates to be shared by all Our November meeting will be held Wednesday the 16th in room 118 (classroom in the left-side hallway), Earth & those present, then attendees would order and pay for their Engineering Sciences Building on the west side of the Penn own dinners. If you plan to attend, please RSVP to Bob Altamura, [email protected] or 814-234-5011. State campus in State College, PA. Maps are available on our web site. We are bringing back our tradition from a few years 6:45 to 7:45 p.m.: Social hour, refreshments in the lobby ago: members can have a table at the dinner to sell [if the lobby is available] minerals / fossils/ gems / jewelry / rock crafts. Sellers 7:45 to 8:00 p.m.: announcements, questions, answers would need to collect PA sales tax. NMS would charge a about 8:00 p.m.: featured program commission fee at 10% of the vendor's pre-tax sales. -
This Project Was Financed in Part by a Grant from the Coldwater Heritage Partnership on Behalf of the PA Department of Conservat
This project was financed in part by a grant from the Coldwater Heritage Partnership on behalf of the PA Department of Conservation and Natural Resources, the PA Fish and Boat Commission, the Western PA Watershed Program and the PA Council of Trout UnlimiUnlimitedtedtedted.... Coldwater Heritage Partners: The Clinton County Conservation District would like to thank: Lock Haven University Dr. Md. Khalequzzaman Dr. John Way John Woodward Lycoming College Clean Water Institute Lloyd Wilson Chapter of Trout UnliUnlimitedmited Allegheny Mountain Chapter of Trout Unlimited PA State Council of Trout Unlimited Clinton County Conservation District 2008 Summer Interns PA Fish & Boat Commission USDA ––– Natural Resource Conservation Service Lamar National Fish Hatchery and NortheaNortheastst Fishery Center Special thanks to Josh Furl who was one of the Conservation District’s 2007 and 2008 Interns. Josh played a major role in field work, data collection, and preparing this Conservation Plan. TABLE OF CONTENTS Summary . 6 Fishing Creek/Cedar Run Watershed Characteristics. 6 Watershed Overview . 6 Fishing Creek Watershed’s Ecoregional Framework . 8 Physiography, Topography, and Geology. 9 Hydrology. 11 Trout . 11 Land Use . .12 Pennsylvania Department of Environmental Protection Ch. 93 Designations . .16 Previous Studies/Analysis of Watershed. .18 Methods and Materials. 20 Water Chemistry . .20 Chemical Parameter Explanations . 22 Habitat Assessments . .24 Macroinvertebrates . .24 Electrofishing . .26 Fishing Creek Assessment . 28 Water Chemistry . .28 Habitat Assessments . .38 Macroinvertebrates . .40 Electrofishing . .45 Cedar Run Assessment . .47 Water Chemistry . 47 Habitat Assessments . 51 Macroinvertebrates . .54 Electrofishing . .58 Recommendations . 60 Agricultural Conservation Plans . 61 Riparian Vegetation/Canopy Cover . .61 No-Till/Conservation Tillage . .62 Fish Habitat Improvement/Bank Stabilization Structures . -
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. -
Comparing the 2017 Team to the 1994 Squad
INSIDE Getting ‘hands on’ with Editorial: Holding Volleyball focusing on Curley out of prison, now animal therapy: page 3 accountability: page 4 improving record: page 5 under house arrest: page 7 Vol. 118, No. 38 Wednesday, Oct. 11, 2017 PUMPKIN PICASSO ‘We do this because we love y’all’: PRCC closes for the week By Elizabeth Winters appreciation of the diverse per- THE DAILY COLLEGIAN spectives, experiences, and cul- tures of many under-represented The Paul Robeson Cultural communities that comprise the Center announced Monday student, faculty, staff, and commu- evening that it would be closed nity population of University Park for the remainder of the week and State College, Pennsylvania,” due to lack of support from stu- according to its site. dents. The PRCC sent out Tweets The center, located in 21 indicating its disappointment on HUB-Robeson Center, left a the turnout for events held by note on its door and tweeted the center, such as the recent about the closing. Hip-Hop Summit, for students “We have changed pro- whom they serve “day in and day grams,” the letter reads. out.” “We have added events. We Students and alumni of the Erin O’Neill/Collegian have stopped doing events that center have made their feel- 5-year-old Alan Mogilnyy paints the bottom of his pumpkin with help from his mother, Gulnara Mogilnyy, were not reaching students in ings known about the closing via of State College, outside of Weston Community Center in White Course Apartments on Oct. 10. meaningful ways. We have cre- social media sites like Twitter and ated new events. -
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.