Geology and Archaeology of Meadowcroft Rockshelter and the Multiple Ice Ages of Southwestern Pennsylvania

Total Page:16

File Type:pdf, Size:1020Kb

Geology and Archaeology of Meadowcroft Rockshelter and the Multiple Ice Ages of Southwestern Pennsylvania GEOLOGY AND ARCHAEOLOGY OF MEADOWCROFT ROCKSHELTER Meadowcroft Rockshelter (photo from Anonymous, 2018b). AND THE MULTIPLE ICE AGES OF SOUTHWESTERN PENNSYLVANIA Pittsburgh Geological Society Field Trip September 7, 2019 Guidebook PGS Spring Field Trip September 7, 2019 Geology and Archaeology of Meadowcroft Rockshelter and the Multiple Ice Ages of Southwestern Pennsylvania Trip Leaders: Mary Ann Gross, Range Resources—Appalachia John A. Harper, Carnegie Museum of Natural History Albert D. Kollar, Carnegie Museum of Natural History i TABLE OF CONTENTS Page Introduction ................................................................................................................... 1 The Pleistocene in southwestern Pennsylvania ................................................................. 2 Pennsylvanian climate-driven sedimentary cycles with emphasis on the Monongahela Formation ...................................................................................... 12 Road log ........................................................................................................................ 20 Stop 1. Meadowcroft Historic Village and Visitor Center ......................................... 23 Stop 2. Meadowcroft Rockshelter ......................................................................... 25 Stop 3. Cross Creek County Park – lunch .............................................................. 36 Stop 4. Tour of MarkWest Houston, PA plant ......................................................... 38 Stop 5. Former Pleistocene bog site ...................................................................... 44 Stop 6. Pennsylvanian Ice Age stratigraphy ........................................................... 49 References ..................................................................................................................... 55 LIST OF FIGURES Figure 1. North America during the Wisconsinan glaciation .............................................. 2 2. Glacial and interglacial stages of the Pleistocene Epoch ..................................... 2 3. Glacial map of western Pennsylvania ................................................................ 2 4. Maps of western Pennsylvania before, during, and after the Pleistocene ............. 4 5. Carmichaels Formation at Carmichaels, Greene County, showing the direction of flow of the Pleistocene Pittsburgh River ........................................................ 5 6. Reconstruction of Lake Monongahela ................................................................ 5 7. Pleistocene terrace deposits in southwestern Pennsylvania ................................ 6 8. Map of eastern North America during the Wisconsinan ...................................... 7 9. Rock cities in southwestern Pennsylvania .......................................................... 7 10. Spruce Flats Bog in Laurel Summit State Park, Westmoreland and Somerset counties and sphagnum, or peat moss ............................................................... 8 11. Map of Pennsylvania peat bogs ........................................................................ 8 12. The Great Meadow at Fort Necessity in Fayette County ..................................... 9 13. Mastodon tusk found at Sharpsburg in 1909 ..................................................... 9 14. Comparisons of the fossil jaws of some now-extinct animals from Blair County ... 10 15. Some of the larger now-extinct animals that roamed the tundra of western ........ 10 Pennsylvania during the late Pleistocene and very early Holocene 16. Paleogeographic map of the Early Pennsylvanian during peak icehouse conditions in southern Gondwana ..................................................................... 12 17. Pennsylvanian stratigraphy of the central Appalachian Basin .............................. 13 18. Stratigraphic diagram of the Monongahela Formation in western Pennsylvania .... 14 19. Comparison of Monongahela strata with interpreted climatic cycles .................... 15 20. The Pittsburgh coal bed along Sygan Road in South Fayette Township, near Bridgeville ................................................................................................ 15 21. The Monongahela Formation outcrop along I-79 near the Carnegie interchange .. 16 22. Lacustrine climate cycles in the Monongahela Formation .................................... 17 23. Some of the trees characteristic of Pennsylvanian peat swamps ......................... 17 24. The skull of Fedexia, a Pennsylvanian ............................................................... 18 25. Characteristic tetrapods of the Monongahela Formation ..................................... 18 26. Vertebrate bones described and illustrated by Case from the Pittsburgh red beds at Pitcairn .......................................................................................... 19 27. Map of the field trip route and stop localities ..................................................... 20 28. An enthusiastic crowd gathers for a concert at KeyBank Pavilion ........................ 21 ii Page 29. Photograph of Burgettstown, around 1910 ........................................................ 21 30. Location of Stops 1 and 2 ................................................................................ 23 31. The visitor center at Meadowcroft Rockshelter and Historic Village ..................... 24 32. Map of Meadowcroft Rockshelter and Historic Village ......................................... 24 33. Some of the buildings in the Historic Village ...................................................... 24 34. Meadowcroft’s Indian village ............................................................................ 25 35. Dr. James M. Adovasio with David Scofield, Director of the Meadowcroft Rockshelter and Historic Village ........................................................................ 25 36. Regional structure map on the base of the Pittsburgh coal ................................. 26 37. Evolution of Cross Creek valley and the formation of Meadowcroft Rockshelter ... 27 38. Sedimentary structure and grain size of the Morgantown sandstone ................... 28 39. Honeycomb weathering of the Morgantown sandstone ...................................... 29 40. Early photographs of Meadowcroft Rockshelter .................................................. 30 41. Inside Meadowcroft Rockshelter ....................................................................... 30 42. The Miller Lanceolate ....................................................................................... 31 43. Assorted Miller Complex artifacts from Stratum IIa ............................................ 32 44. Meadowcroft basketry ..................................................................................... 32 45. Assortment of bone objects at Meadowcroft ...................................................... 32 46. Evidence of ancient campfires built at the site ................................................... 33 47. Plot of radiocarbon dates from Meadowcroft Rockshelter showing one standard Deviation ......................................................................................................... 33 48. Eastern half of the United States showing the locations of pre-Clovis sites .......... 34 49. Location of Stop 3 ........................................................................................... 36 50. Pavilion #3 at Cross Creek County Park ............................................................ 37 51. Cross Creek Lake and some of its ..................................................................... 37 52. Some of the fish available in Cross Creek County Park ....................................... 37 53. Local farm modified by the effects of a Marcellus shale gas lease ....................... 38 54. Location of Stop 4 ........................................................................................... 38 55. The MarkWest Houston Complex in Houston, PA ............................................... 39 56. Overviews of MPLX gathering, processing, natural gas supply, and northeast operations ....................................................................................................... 42 57. Location of Stop 5 ........................................................................................... 45 58. Former strip mining operation and Pleistocene terraces ..................................... 45 59. The geologic section exposed at the Hussey Strip Operation near ...................... 46 60. The cleaned face of the peat deposit showing test tubes in place for sampling .... 46 61. Diagram of the Wisconsinan Stage ................................................................... 47 62. Some of the mastodon bones found in the Bridgeville peat bog .......................... 48 63. Diagram showing the transition from a pond or lake to a peat bog ..................... 48 64. Location of Stop 6 ........................................................................................... 49 65. The Benwood Limestone along PA 50 west of Bridgeville ................................... 50 66. Stratigraphic diagram of the Monongahela and Waynesburg formations ............. 50 67. Callipteris conferta, once thought to be a Permian index fossil ............................ 51 68. The upper Monongahela Formation and lower Waynesburg Formation ............... 52 69. Some of the sedimentary features that can be seen at Stop 6 ..........................
Recommended publications
  • Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution
    Graduate Theses, Dissertations, and Problem Reports 2020 Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution Mark D. Swift West Virginia University, [email protected] Follow this and additional works at: https://researchrepository.wvu.edu/etd Part of the Geomorphology Commons Recommended Citation Swift, Mark D., "Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution" (2020). Graduate Theses, Dissertations, and Problem Reports. 7542. https://researchrepository.wvu.edu/etd/7542 This Thesis is protected by copyright and/or related rights. It has been brought to you by the The Research Repository @ WVU with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you must obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in WVU Graduate Theses, Dissertations, and Problem Reports collection by an authorized administrator of The Research Repository @ WVU. For more information, please contact [email protected]. Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution Mark D. Swift Thesis Submitted to the Eberly College of Arts and Sciences at West Virginia University in partial fulfillment of the requirements for the degree of Master of Arts in Geography Jamison Conley, Ph.D., Co-Chair J. Steven Kite, Ph.D., Co-Chair Nicolas Zegre, Ph.D. Department of Geology and Geography Morgantown, West Virginia 2020 Keywords: landscape evolution, knickzone, southwest Pennsylvania Copyright 2020 Mark D.
    [Show full text]
  • Washington County Watershed Roadmap
    e ounty Lin Clinto C t C n Frankfort lint for P on Frank Clinton Fra ort urd y nkf r e o l g l DILLOE RUN i g i D B S u n n Kings Creek y B H IG w Gi do K Ell a V Me I R N e R G M U Contact Information y r K ille N e d S -d rr - r l K A u s C i Van t r If you are interested in joining an active watershed association or starting a new one or just C R po G R E r B t H o N enne E U a tt a R AK c r N obtaining more information, contact the Alliance at: ls res u d AI t l e L on K r ER l E B a b e E M B R P ON CREEK) A k C urd (INTO RASCCO CH ree S y USH RUN haron s BR ts C g n G in n Washington County Watershed Alliance IN o n i e M P o K N K U D e o c iv c R s c lton Hill c 100 West Beau Street, Suite 105 l F Know Ra S i ra R K v c o C e b I k in R Washington, PA 15301 C D e r s T n C e o A l gs e P y in k K n H E T d K H A N O V E R Phone: 724-228-6774 E C S i r R e S e C C R s ll le n h l h m N u a a u i i r d v o a O D m r Fax: 724-223-4682 v r O c g n K C p olm r e e C h e ill e l b v e h b A n R e be E-Mail: [email protected] f k u teu c e l Old S o t l T S r L k ille u L u ta ake benv r e N eu k S t e T S e d y U Ol r R H 22 ce S o ru C K l p C Prepared By: Washington County Watershed Associations P lo L S I w a R Legend h p u T i S r A m e P Washington County Planning Commission GIS as a Public Service For the Washington County Watershed Alliance There are many active watershed associations in Washington County.
    [Show full text]
  • University of Michigan Radiocarbon Dates Xii H
    [Ru)Ioc!RBo1, Vol.. 10, 1968, P. 61-114] UNIVERSITY OF MICHIGAN RADIOCARBON DATES XII H. R. CRANE and JAMES B. GRIFFIN The University of Michigan, Ann Arbor, Michigan The following is a list of dates obtained since the compilation of List XI in December 1965. The method is essentially the same as de- scribed in that list. Two C02-CS2 Geiger counter systems were used. Equipment and counting techniques have been described elsewhere (Crane, 1961). Dates and estimates of error in this list follow the practice recommended by the International Radiocarbon Dating Conferences of 1962 and 1965, in that (a) dates are computed on the basis of the Libby half-life, 5570 yr, (b) A.D. 1950 is used as the zero of the age scale, and (c) the errors quoted are the standard deviations obtained from the numbers of counts only. In previous Michigan date lists up to and in- cluding VII, we have quoted errors at least twice as great as the statisti- cal errors of counting, to take account of other errors in the over-all process. If the reader wishes to obtain a standard deviation figure which will allow ample room for the many sources of error in the dating process, we suggest doubling the figures that are given in this list. We wish to acknowledge the help of Patricia Dahlstrom in pre- paring chemical samples and David M. Griffin and Linda B. Halsey in preparing the descriptions. I. GEOLOGIC SAMPLES 9240 ± 1000 M-1291. Hosterman's Pit, Pennsylvania 7290 B.C. Charcoal from Hosterman's Pit (40° 53' 34" N Lat, 77° 26' 22" W Long), Centre Co., Pennsylvania.
    [Show full text]
  • 9 !(1 !(1 !(2 !(3 !(4 !(5 !(6 !(7 !(2 !(3 !(6 !(7 !(5 !(5 !(3 !(4 !(4 !(6 !(7 !(2 !(7
    Primary Greenways Secondary Greenways Recreation Greenways Natural Areas WASHINGTON COUNTY (!1 Monongahela River Water Corridor (!1 Raccoon Creek Natural Area GREENWAYS PLAN !2 National Road Heritage Corridor (!2 Cross Creek Natural Area Raccoon Creek Valley ( 3 3 Buffalo Creek Natural Area Natural Area (! Montour Trail Corridor (! 23 HANOVER 15 4 Enlow Fork Natural Area (! 1 Hillman (! 4 Panhandle Trail Corridor (! (!?é Stat e Park (! 5 Chartiers Creek Water Corridor 5 Little Chartiers Creek Natural Area 22 Starpointe (! (! (! I¨ I¨ (!6 BicyclePA Route A Corridor (!6 Mingo Creek Natural Area Map 10: Primary and ROBINSON 7 BicyclePA Route S Corridor SGL 117 (! 7 Franklin Natural Area (!3 (! Secondary Greenways ?À (!8 Ringlands Natural Area SMITH 4 BURGETTSTOWN (! Recreation Greenways (!4 MCDONALD MIDWAY (!9 Mingo Creek Trail Corridor JEFFERSON (!10 Bethel Spur Trail Corridor (!15 !3 6 ?é 31 ( (! 11 National Pike Trail Corridor (! ?c (! 12 Montour Trail to Westland Trail Corridor CECIL (! CROSS CREEK ?À12 (!5 (!10 Meadowcroft SGL 303 (! 13 Buffalo Creek Water Corridor Museum M 24 !"c$ (! ?c MOUNT CANO(!NSBURG I¥ 14 Rea Block 14 Cross Creek Water Corridor 1" = 4 miles (! FCielrd oss Creek PLEASANT (!3 (! ?c Canonsburg Lake PETERS ?¢ Natural Area ?³ !15 Raccoon Creek Water Corridor SGL 303 ?ü ( Cross Creek Lake2 (! FINLEYVILLE 16 Ten Mile Creek Water Corridor ?é HOUSTON (!20 UNION (! WESCTross Creek County Park 19 14 CHARTIERS (! 26 INDEPENDENCE MIDDLETOWN ! (! Conservation Greenways ( (!7 NORTH (!6 HOPEWELL I-79 E xit 41 6 STRABANE ?b (! Mingo Creek (!25 17 Dutch Fork Greenway NOTTINGHAM (! Data Source: PennDot road files; National Heritage Inventory Little Chartiers Creek NEW EAGLE ?Ê CANTON !"c$ Natural Area (!5 Natural Area 18 Enlow Fork Greenway ecological data; Audubon Society Important Bird Areas; ?Ê SGL 432 I-79 E xit 40 21 MON ONG AHELA (! All other data obtained from the Southwestern Pennsylvania BLAINE I¥ 9 ! EAST ( Mingo Cree(!k Commission.
    [Show full text]
  • November-December Newsletter
    The Offi cial Publication of the Montour Trail Council MONTOUR TRAIL-LETTER Volume 18 Issue 6 November/December 2007 Another MTC Groundbreaking It was another momentous day in the history of the Montour Trail when the ground was broken, or should I say, For your consideration a bridge tie was lifted, to mark the onset of construction for Phase 16. Participants in the event gathered at the east end Every mile is two in winter. of Valleybrook #3, that will be the trail-bridget that crosses Valleybrook Road just south of Chartiers Creek and Buckeye George Herbert Lane in Peters Township. Thanks go out to Tom Robinson, owner of TAR Outside Storage for allowing us to use his property for automobile parking and easy access to the site of Photo by Dennis Sims the ceremony. From Left to Right, Mark and Kinga Blum, Mingo Creek Const.; Patricia Moore, Peters Words were said by several area community Twp.; Scott Fergus, Washington County. leaders, including Congressman Tim Murphy, Matt Campion Matt Campion aide to Sen. John Pippy.; representing state Senator John Pippy of the 37th district which Rep. Tim Murphy, Mark Imgrund, Ed Taylor, and Ned Williams of the Montour Trail. Inside this issue: includes Peters Twp., Peters Twp. Councilwoman Patricia Moore and others. The owners of Mingo Creek Construction, Kinga and Mark Blum, the winning bidder Grounbreaking 1 for the project were introduced. Following the speeches, everyone gathered at the bridge for the “tie Tour the Montour lifting”. The dignitaries took turns cranking the come-along lifting the tie from its place.
    [Show full text]
  • Canonsburg, Pennsylvania, Disposal Site Fact Sheet
    Fact Sheet UMTRCA Title I Canonsburg, Pennsylvania, Disposal Site This fact sheet provides information about the Uranium Mill Tailings Radiation Control Act of 1978 Title I disposal site located at Canonsburg, Pennsylvania. The site is managed by the U.S. Department of Energy Office of Legacy Management. Site Description and History The Canonsburg disposal site is a former uranium ore processing site located in the Borough of Canonsburg, Washington County, in southwestern Pennsylvania, approximately 20 miles southwest of downtown Pittsburgh. The site lies between Chartiers Creek and the Pittsburgh and Ohio Central Railroad tracks. The surrounding land is primarily residential and commercial. The former mill processed uranium and other ores at the site between 1911 and 1957 and provided uranium for the U.S. government national defense programs. Standard Chemical operated the site as a radium extraction plant from 1911 to 1922. Later, Vitro Corporation of America acquired the property and processed ore to extract radium and uranium salts. From 1942 until 1957, Vitro was under contract to the federal government to recover uranium from ore and scrap. Processing operations at the site ceased in 1957. For the next 9 years, the site was used only for storage under a U.S. Atomic Energy Commission contract. In 1967, the property was purchased by the Canon Development Company and was leased to tenant companies for light industrial use. Location of the Canonsburg, Pennsylvania, Disposal Site Historical milling operations at the site generated radioactive mill tailings, a predominantly sandy material. Some of the Regulatory Setting tailings were shipped to Burrell Township 50 miles away to be used as additional fill in a railroad landfill.
    [Show full text]
  • Application of Duquesne Light Company Filed Pursuant to 52 Pa
    BEFORE THE PENNSYLVANIA PUBLIC UTILITY COMMISSION Application of Duquesne Light Company filed Pursuant to 52 Pa. Code Chapter 57, Subchapter G, for Approval of the Siting and : Docket No. A-20 19 - Construction of the 138 kV Transmission Lines Associated with the Brunot Island - Crescent Project in the City of Pittsburgh, McKees Rocks Borough, Kennedy Township,RobinsonTownship,Moon Township, and Crescent Township, Allegheny County, Pennsylvania APPLICATION OF DUQUESNE LIGHT COMPANY TO THE PENNSYLVANIA PUBLIC UTILITY COMMISSION: Duquesne Light Company ("Duquesne Light" or the "Company") hereby files, pursuant to 52 Pa. Code § 57.72, this Application requesting Pennsylvania Public Utility Commission ("Commission") approval to site and construct approximately 14.5 miles of overhead double - circuit 138 kV transmission lines in the City of Pittsburgh, McKees Rocks Borough, Kennedy Township, Robinson Township, Moon Township, and Crescent Township, Allegheny County, Pennsylvania (Hereinafter called the " Brunot Island - Crescent Project" or "BI -Crescent Project"). The proposed Project is required to replace aging transmission system infrastructure. The BI - Crescent corridor has some of Duquesne Light's oldest in-service steel lattice towers. Structural evaluations have determined that the structures are approaching end of useful life. Based on current condition, structure deterioration, and Power Line Systems - Computer Aided Design and Drafting ("PLS-CADD")' modeling at current design codes, all results indicate these 'PLS-CADD is an industry
    [Show full text]
  • 12.9 Kya • Pleistocene Overkill Hypothesis=Overexploitation / Overhun
    Review of Last Class Materials (collapses): -Clovis: 12.9 kya Pleistocene Overkill Hypothesis=overexploitation / overhunting of resources by humans Younger Dryas Hypothesis=big game species died due to dropping temperatures so humans changed from clovis tech to more effective tools for their new food sources Was the change human induced or a gradual change via natural causes? -Skara Brae: 2500BC Huge Storm=excellent preservation of artifacts and engulfed in sand Conditions got worse (colder/wetter)=humans forced to migrate slowly to new areas because they couldn’t keep their crops and animals alive/sufficient for their people Was the change gradual or acute/abrupt? -Mohenjo-Daro: No evidence found of defensive/military tools or efforts=easily invaded and taken over Over-exploited resources=upwards of hundreds of city-centers along Indus river that were all trying to grow food for thousands of people which robbed the soil of its nutrients and they could no longer produce food in the quantity needed to keep their populations running Indus river’s tributaries shifted due to massive earthquakes, so the original river dried up and a new one formed east of the old one, so the city-centers had to move too -Ur: Euphrates dried up around 1000BC during the long-term desertification=urban and rural centers both suffered from lack of food, so many small rural populations are thought to have flocked to urban centers for free meals, whether through peaceful trades or harsher means (burning/sacking) -Poverty Point: Climate change=resources
    [Show full text]
  • (WRAS) State Water Plan Subbasin 20F Chartiers Creek Watershed (Ohio River) Washington and Allegheny Counties
    Updated 9/2003 Watershed Restoration Action Strategy (WRAS) State Water Plan Subbasin 20F Chartiers Creek Watershed (Ohio River) Washington and Allegheny Counties Introduction Subbasin 20F includes the 296-square mile Chartiers Creek watershed located in southwestern Allegheny and northern Washington Counties and the 19.4 square mile watershed of Sawmill Run, the upstream most named tributary flowing directly into the Ohio River. A total of 408 streams flow for 567 miles through the subbasin. Most of the tributary watersheds are small; only Little Chartiers Creek and Robinson Run have drainage areas greater than 30 square miles. Chartiers Creek starts in a rural section of northern Washington County and flows north through Allegheny County and the western Pittsburgh suburbs and through the Pittsburgh City limits to its confluence with the Ohio River near McKees Rocks. The subbasin is part of HUC Area 5030001, Upper Ohio River, a Category I, FY99/2000 Priority watershed in the Unified Watershed Assessment. Geology/Soils: The entire subbasin is in the Western Allegheny Plateau Ecoregion. The upper third of the subbasin is in the Permian Hills (70a) subsection and the lower portion is in the Monongahela Transition Zone (70b) subsection. Strata are composed of sequences of sandstone, shale, limestone, and coal. The commercially valuable Pittsburgh coal underlies the entire subbasin. The upper basin was extensively deep mined starting in the late 1800’s, by the room and pillar method, with coal left in place to support the overlying rock and surface. The region supplied coal and coke for the numerous steel plants in the Pittsburgh region.
    [Show full text]
  • The Zoogeography of the Fishes of the Youghiogheny River System
    The Zoogeographyof the Fishes of the Youghiogheny River System,Pennsylvania, Maryland and West Virginia MICHAEL L. HENDRICKS RMC-MuddyRun EcologicalLaboratory, P. 0. Box 10, Drumore,Pennsylvania 17518 JAY R. STAUFFER, JR. Universityof Maryland,Center for Environmentaland EstuarineStudies, Appalachian Environmental Laboratory,Frostburg 21532 CHARLES H. HOCUTT Universityof Maryland,Center for Environmentaland EstuarineStudies, Horn PointEnvironmental Laboratories,Cambridge 21613; andDepartment ofIchthyology and FisheriesScience, Rhodes University, Grahamstown,South Africa 6140 ABSTRACT: A total of 266 fish collectionswere made at 172 stationsin the YoughioghenyRiver drainage, the largest tributary to theMonongahela River. Collec- tionswere made usingseines, electrofishing gear, gillnets and trapnets. A comprehensiveliterature review yielded 99 speciesof fishesreported from the YoughioghenyRiver system.Six species collectedduring this survey(Amia calva, Carassiusauratus, Ericymba buccata, Notropis rubellus, Ictalurus catus and Fundulusdiaphanus) establishednew distributional records for the system, increasing the total to 105 species. Of thistotal, 78 specieswere verified either by our collections(57 species),museum records(10) or stockingrecords (11), whereas27 could not be verified.Of the 27 unverifiedspecies, 21 are expectedto occurand six are consideredmisidentifications or erroneousrecords. An additional24 speciesare expectedto have occurredhistorically in the Youghioghenyor have the potentialto do so based on theirdistribution in the
    [Show full text]
  • New Record of Terminal Pleistocene Elk/Wapiti (Cervus Canadensis) from Ohio, USA
    2 TERMINAL PLEISTOCENE ELK FROM OHIO VOL. 121(2) New Record of Terminal Pleistocene Elk/Wapiti (Cervus canadensis) from Ohio, USA BRIAN G. REDMOND1, Department of Archaeology, Cleveland Museum of Natural History, Cleveland, OH, USA; DAVID L. DYER, Ohio History Connection, Columbus, OH, USA; and CHARLES STEPHENS, Sugar Creek Chapter, Archaeological Society of Ohio, Massillon, OH, USA. ABSTRACT. The earliest appearance of elk/wapiti (Cervus canadensis) in eastern North America is not thoroughly documented due to the small number of directly dated remains. Until recently, no absolute dates on elk bone older than 10,000 14C yr BP (11,621 to 11,306 calibrated years (cal yr) BP) were known from this region. The partial skeleton of the Tope Elk was discovered in 2017 during commercial excavation of peat deposits from a small bog in southeastern Medina County, Ohio, United States. Subsequent examination of the remains revealed the individual to be a robust male approximately 8.5 years old at death. The large size of this individual is compared with late Holocene specimens and suggests diminution of elk since the late Pleistocene. Two accelerator mass spectrometry (AMS) radiocarbon assays on bone collagen samples taken from the scapula and metacarpal of this individual returned ages of 10,270 ± 30 14C yr BP (Beta-477478) (12,154 to 11,835 cal yr BP) and 10,260 ± 30 14C yr BP (Beta-521748) (12,144 to 11,830 cal yr BP), respectively. These results place Cervus canadensis in the terminal Pleistocene of the eastern woodlands and near the establishment of the mixed deciduous forest biome over much of the region.
    [Show full text]
  • July-August Newsletter
    The Official Publication of the Montour Trail Council MONTOUR TRAIL-LETTER Celebrating 32 Years Volume 32 Issue 4 July-August 2021 Always B Smiling (copied from their web page) Loving came naturally to “B” and he learned from the very best. Kristin Heine Huibregtse and Dean Huibregtse are the epitome of loving parents and they made sure that Bennett’s life was lived joyfully and to the fullest every day. Just 18, Bennett loved being at the front of his Duet Bike with mom or dad at the helm, and we are thrilled to share this simple joy with other families. Always B Smiling has teamed up with the Tandem Connection on the Montour Trail in Canonsburg, PA to offer FREE adaptive bike rides for children and young adults with disabilities and their families. It’s a great way for people with disabilities that include limited mobility to enjoy recreation and fun outdoors! When: Saturday Afternoons May 15 thru October 30 - 2pm-4pm or 4pm-6pm Where: Tandem Connection -Hendersonville, PA Riders heading out on their inaugural ride. Photo courtesy of Harry Funk O-R. Powered by trained volunteers, the Duet Bike provides a comfortable wheelchair seat at the front of the electronic-assisted bicycle. This provides riders the pleasure of riding a bike with the breeze in your hair and the sun on your face. On every outing, there will be two trained volunteers joining you and your family and friends on your outing – one to power the bike and the other to ride along as a backup. * Note that at least one parent or adult must be present with the rider.
    [Show full text]