Annotated Bibliography of Sources Related to the Natural Values of the Mackenzie River
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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. -
023810 Rangifer Spec Issue
The Ninth North American Caribou Workshop, S7 Kuujjuaq, Québec, Canada, 23-27 April, 2001. Status, population fluctuations and ecological relationships of Peary caribou on the Queen Elizabeth Islands: Implications for their survival Frank L. Miller1 & Anne Gunn2 1 Canadian Wildlife Service, Prairie & Northern Region, Room 200, 4999 - 98th. Avenue, Edmonton, Alberta T6B 2X3 Canada ([email protected]). 2 Department of Resources, Wildlife and Economic Development, Government of the Northwest Territories, Box 1320, Yellowknife, Northwest Territories X1A 3S8 Canada. Abstract: The Peary caribou (Rangifer tarandus pearyi) was recognized as 'Threatened' by the Committee on the Status of Endangered Wildlife in Canada in 1979 and 'Endangered' in 1991. It is the only member of the deer family (Cervidae) found on the Queen Elizabeth Islands (QEI) of the Canadian High Arctic. The Peary caribou is a significant part of the region's biodiversity and a socially important and economically valuable part of Arctic Canada's natural heritage. Recent microsatellite DNA findings indicate that Peary caribou on the QEI are distinct from caribou on the other Arctic Islands beyond the QEI, including Banks Island. This fact must be kept in mind if any translocation of caribou to the QEI is pro• posed. The subspecies is too gross a level at which to recognize the considerable diversity that exists between Peary cari¬ bou on the QEI and divergent caribou on other Canadian Arctic Islands. The Committee on the Status of Endangered Wildlife in Canada should take this considerable diversity among these caribou at below the subspecies classification to mind when assigning conservation divisions (units) to caribou on the Canadian Arctic Islands. -
Chapter 1: Sequence Stratigraphy of the Glenshaw Formation
Martino, R. L., 2004, Sequence stratigraphy of the Glenshaw Formation (middle–late Pennsylvanian) in the central Appalachian basin, in J. C. Pashin and R. A. Gastaldo, eds., Sequence stratigraphy, paleoclimate, and tectonics of coal-bearing strata: AAPG Studies 1 in Geology 51, p. 1–28. Sequence Stratigraphy of the Glenshaw Formation (Middle–Late Pennsylvanian) in the Central Appalachian Basin Ronald L. Martino Department of Geology, Marshall University, Huntington, West Virginia, U.S.A. ABSTRACT he Glenshaw Formation consists predominantly of sandstones and mud- rocks with thin limestones and coals, which are thought to have accumu- T lated in alluvial, deltaic, and shallow-marine environments. Analysis of 87 Glenshaw outcrops from southern Ohio, eastern Kentucky, and southern West Vir- ginia has revealed widespread, well-developed paleosols. These paleosols are used, along with marine units and erosional disconformities, to develop a high-resolution sequence-statigraphic framework. The tops of the paleosols constitute boundaries for nine allocycles, which are interpreted as fifth-order depositional sequences. Allocycles in this framework correlate with similar allocycles described from the northern Appalachian basin. A sequence-stratigraphic model is proposed that provides a framework for in- terpreting facies architecture in terms of base-level dynamics linked to relative sea level changes. Lowered base level caused valley incision along drainage lines and sediment bypassing of interfluves, which led to development of well-drained paleo- sols. Rising base level produced valley filling by fluvioestuarine systems (lowstand systems tract/transgressive systems tract), whereas pedogenesis continued on inter- fluves. As drainage systems aggraded, the coastal plain water table rose, and in- terfluvial paleosols were onlapped by paludal and lacustrine deposits. -
CZN Comments on Final Arguments
September 16, 2011 Chuck Hubert Environmental Assessment Officer Mackenzie Valley Review Board Suite 200, 5102 50th Avenue, Yellowknife, NT X1A 2N7 Dear Mr. Hubert RE: Environmental Assessment EA0809-002, Prairie Creek Mine Comments on Final Arguments Canadian Zinc Corporation (CZN) is pleased to provide the attached comments on the Final Arguments submitted by parties at the conclusion of environmental assessment EA0809-002. Technical replies are provided, where necessary, by stating CZN’s position with respect to recommendations made. Where recommendations are unchanged from Technical Reports, the Review Board is directed to CZN’s comments on Technical Reports in Attachment 1. The contents of Attachment 1 should be read first since context is provided for some of our responses to the Final Arguments. Please note that our comments on Technical Reports contain no new information, and no timeline was provided by the Review Board for their submission. Also attached is a final commitments table (Table 1), and the curricula vitae of the main individual consultants who provided deliverables for the environmental assessment process. Yours truly, CANADIAN ZINC CORPORATION David P. Harpley, P. Geo. VP, Environment and Permitting Affairs Suite 1710-650 West Georgia Street Vancouver, BC V6B 4N9 Tel: (604) 688-2001 Fax: (604) 688-2043 E-mail: [email protected], Website: www.canadianzinc.com COMMENTS ON PARTY FINAL ARGUMENTS Aboriginal Affairs and Northern Development Canada (AANDC) Water Management and Storage Recommendation 2: Final selection of an additional water storage option must be done in conjunction with the determination of Site Specific Water Quality Objectives for Prairie Creek. If increased capacity associated with construction of an additional pond provides for the ability to meet Reference Condition Approach benchmarks as defined within the derivation process, that option must be selected and implemented. -
NWT Transportation Report Card 2015 Is Intended to Provide a Statistical Benchmark of Progress Achieved and an Evaluation Framework to Measure Future Progress
TABLED DOCUMENT 345-17(5) TABLED ON OCTOBER 7, 2015 Table of Contents Overview ....................................................................................................................................3 Strengthening Connections .....................................................................................................5 Capturing Opportunities ...........................................................................................................9 Embracing Innovation ............................................................................................................ 11 Metrics & Data .........................................................................................................................13 1.0 Financial .................................................................................................................. 13 1.1 Capital and O&M Expenditures and Revenue .............................................. 13 1.2 Analysis of Capital Needs ............................................................................ 14 1.3 Major Partnership Funding ........................................................................... 15 1.4 Airport, Road Licensing and Deh Cho Bridge Toll Revenues ....................... 16 1.5 Northern, Local, Other, contracts and Total Value of Contracts .................... 18 1.6 Community Access Program Expenditures ................................................. 18 2.0 Airports ....................................................................................................................19 -
EA1415-01 Developer's Assessment Report
DEVELOPER’S ASSESSMENT REPORT ALL SEASON ROAD PROJECT PRAIRIE CREEK MINE MAIN REPORT Volume 1 of 3 SUBMITTED IN SUPPORT OF: Environmental Assessment of Prairie Creek Mine EA 1415-01 SUBMITTED TO: Mackenzie Valley Review Board Yellowknife, NT X1A 2N7 SUBMITTED BY: Canadian Zinc Corporation Vancouver, BC V6B 4N9 April 2015 PROJECT FACT SHEET CORPORATE DATA Project Name Prairie Creek Mine Company Name and Address Canadian Zinc Corporation Suite 1710, 650 West Georgia Street Vancouver, B.C., V6B 4N9 Telephone: (604) 688-2001 Fax: (604) 688-2043 Canadian Zinc Corporation 9926-101st Avenue PO Box 500 Fort Simpson, NT X0E 0N0 Telephone: (867) 695-3963 Fax: (867) 695-3964 Contacts Alan Taylor, Chief Operating Officer and VP Exploration David Harpley, VP Environment & Permitting Affairs Wilbert Antoine, Manager of Northern Development COMMUNITY DATA First Nation Territory Nahanni Butte Dene Band, Dehcho Nearest Community Nahanni Butte, 95 km south-east Other Communities Fort Liard, 165 km south-east Fort Simpson, 185 km east Land Claims Status In negotiation, Dehcho Process PROJECT DETAILS Location 550 km west of Yellowknife, NWT 61°33’ N latitude, 124°48’ W longitude Undertaking ~185 km all season road to the Liard Highway essentially using the existing, permitted winter road alignment Prairie Creek All Season Road Project – April 2015 1 GONDI AEK’ÉHZE ADLÁ Gondi Éhgonñæá Dii Prairie Creek Mine góhts’edi tå’a Góhdli Ndehé k’eh yunahnee tå’uh nît’i ii gots’ç xôh shíhtah á goæô. Káa azhô t’áh Canadian Zinc Corporation (CZN) gots’êh á agøht’e. K’õô 1980 kéhonñdhe ekúh á ndéh gozhíhe gots’êh satsõ kázhe gha seegúdlá agøht’e t’áh t’ahsíi met’áh alaeda thela á agøht’e. -
Final Complete Dissertation Kua 1
Trends and Ontology of Artistic Practices of the Dorset Culture 800 BC - 1300 AD Hardenberg, Mari Publication date: 2013 Document version Early version, also known as pre-print Citation for published version (APA): Hardenberg, M. (2013). Trends and Ontology of Artistic Practices of the Dorset Culture 800 BC - 1300 AD. København: Det Humanistiske Fakultet, Københavns Universitet. Download date: 08. Apr. 2020 Trends and Ontology of Artistic Practices of the Dorset Culture 800 BC – 1300 AD Volume 1 By © Mari Hardenberg A Dissertation Submitted to the Ph.d.- School In Partial fulfillment of the Requirements for the Degree of Doctor of Philosophy SAXO-Institute, Department of Prehistoric Archaeology, Faculty of Humanities University of Copenhagen August 2013 Copenhagen Denmark ABSTRACT This dissertation examines the various artistic carvings produced by the hunter-gatherer Dorset people who occupied the eastern Arctic and temperate regions of Canada and Greenland between circa BC 800 – AD 1300. It includes considerations on how the carved objects affected and played a role in Dorset social life. To consider the role of people, things and other beings that may be said to play as actors in interdependent entanglements of actions, the agency/actor- network theory is employed. From this theoretical review an interpretation of social life as created by the ways people interact with the material world is presented. This framework is employed as a lens into the social role and meaning the carvings played in the Dorset society. The examined assemblages were recovered from a series of Dorset settlement sites, mainly in house, midden, and burial contexts, providing a substantive case study through which variations and themes of carvings are studied. -
Infonorth Five Hundred Meetings of the Arctic Circle
ARCTIC VOL. 67, NO. 2 (JUNE 2014) P. 1 – 12 InfoNorth Five Hundred Meetings of the Arctic Circle by C.R. Burn SUPPLEMENTARY TABLES 1 AND 2 TABLE 1. List of meetings of the Arctic Circle.1 Special Meetings are in bold. Year Meeting Date Speaker2 Topic3 1947 1 12 December Flt. Lt. A.H. Tinker Establishment of weather stations at Eureka and Resolute Bay 1948 2 15 January Sgt. F.S. Farrar, RCMP Film: St Roch 3 16 February R.G. Madill, Flt. Lt. J.F. Drake North magnetic pole 4 18 March Lt. Col. A. Croft Operation Musk-ox 5 13 April H.M. Raup Botany, geology, and archaeology, Alaska Highway 6 25 May J.G. Wright Film: RMS Nascopie 7 20 August Picnic at the Jenness’s cottage 8 4 November C.S. Lord Mining in NWT 9 9 December P. Serson Operation Magnetic 1949 10 13 January B.J. Woodruff Geodetic Survey of Canada 11 10 February P.D. Baird Project Snow Cornice 12 10 March Cdr. D.C. Nutt, USNR Antarctica 13 14 April J.C. Wyatt Construction in the Arctic 14 12 May Mrs. T.H. Manning Travels in Hudson Bay and Foxe Basin 15 10 November Dr. J.C. Callaghan Experiences of a medical officer in the Arctic 16 8 December M.J. Dunbar Marine resources of the eastern Arctic 1950 17 12 January Flt. Lt. B. Hartman Search and rescue in the eastern Arctic 18 9 February A.E. Porsild Plant life 19 9 March D. Wilkinson NFB in the North 20 13 April T.H. -
Northwest Territories Transportation Strategy, 2015-2040
TABLED DOCUMENT 267-17(5) TABLED ON JUNE 3, 2015 NING CON THE NEC NG TI E ON R S ST S E E M Connecting I T B I R N A Us U C T I N R G O P I N P N O O G V A IN T R IO U N PT CA 2015-2040 Northwest Territories Transportation Strategy Minister’s Message The road, air, rail and marine transportation system has played a key role in the history and development of the Northwest Territories, and will continue to support sustainable communities and a growing economy into the future. Over the past year, the Department of Transportation engaged a broad base of stakeholders to discuss the challenges and opportunities facing our northern transportation system. These engagements helped identify the vision and strategic priorities for enhancing our transportation system to meet the future needs of residents, communities, businesses and industry. As we mark the 25th anniversary of the Department of Transportation, established in 1989, and reflect on the great accomplishments achieved to date, it is the perfect time to redefine the path forward over the next 25 years. This strategy, Connecting Us, presents a vision for the transportation system and the strategic long-term priorities that will guide future actions of the Department of Transportation. It also outlines a framework for measuring and reporting on our success into the future. Northerners are strong, resilient people and we must continue working together to strengthen connections, capture opportunities and embrace innovation. Doing so will improve and enhance our transportation infrastructure, services, programs and policies, which will, in turn, lead to a sustainable economy, vibrant communities and self-reliant people. -
Movements and Habitat Use of Muskoxen on Bathurst, Cornwallis
MOVEMENTS AND HABITAT USE OF MUSKOXEN (Ovibos moschatus) ON BATHURST, CORNWALLIS, AND DEVON ISLANDS, 2003-2006 Morgan Anderson1 and Michael A. D. Ferguson Version: 23 December 2016 1Department of Environment, Government of Nunavut, Box 209 Igloolik NU X0A 0L0 STATUS REPORT 2016-08 NUNAVUT DEPARTMENT OF ENVIRONMENT WILDLIFE RESEARCH SECTION IGLOOLIK, NU i Summary Eleven muskoxen (Ovibos moschatus) were fitted with satellite collars in summer 2003 to investigate habitat preferences and movement parameters in areas where they are sympatric with Peary caribou on Bathurst, Cornwallis, and Devon islands. Collars collected locations every 4 days until May 2006, with 4 muskoxen on Bathurst Island collared, 2 muskoxen collared on Cornwallis Island, and 5 muskoxen collared on western Devon Island. Only 5-29% of the satellite locations were associated with an estimated error of less than 150 m (Argos Class 3 locations). Muskoxen in this study used low-lying valleys and coastal areas with abundant vegetation on all 3 islands, in agreement with previous studies in other areas and Inuit qaujimajatuqangit. They often selected tussock graminoid tundra, moist/dry non-tussock graminoid/dwarf shrub tundra, wet sedge, and sparsely vegetated till/colluvium sites. Minimum convex polygon home ranges representing 100% of the locations with <150 m error include these movements between core areas, and ranged from 233 km2 to 2494 km2 for all collared muskoxen over the 3 years, but these home ranges include large areas of unused habitat separating discrete patches of good habitat where most locations were clustered. Several home ranges overlapped, which is not surprising, since muskoxen are not territorial. -
Potamology As a Branch of Physical Geography Author(S): Albrecht Penck Source: the Geographical Journal, Vol
Potamology as a Branch of Physical Geography Author(s): Albrecht Penck Source: The Geographical Journal, Vol. 10, No. 6 (Dec., 1897), pp. 619-623 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1774910 Accessed: 27-06-2016 09:37 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The Royal Geographical Society (with the Institute of British Geographers), Wiley are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 128.110.184.42 on Mon, 27 Jun 2016 09:37:29 UTC All use subject to http://about.jstor.org/terms ( 619 ) POTAMOLOGY AS A BRANCH OF PHYSICAL GEOGRAPHY.* By Professor ALBRECHT PENCK, Ph.D. OF the different departments of physical geography treating of the hydrosphere, none has advanced more slowly than the science of rivers. Oceanography has developed in a wonderful way. The limnology advocated by Forel at the London Congress of 1895 has become a separate flourishing branch; only the hydrology of running water is still in a very unsatisfactory state. The fact that it has not a name of its own corresponding to oceanography or to limnology, indicates its neglected position, but there can be no doubt that it must gain equal rank and follow the same evolution as the two other above-named branches of hydrology. -
Carboniferous Coal-Bed Gas Total Petroleum System
U.S. Geological Survey Open-File Report 2004-1272 Assessment of Appalachian Basin Oil and Gas Resources: Carboniferous Coal-bed Gas Total Petroleum System Robert C. Milici U.S. Geological Survey 956 National Center Reston, VA 20192 1 Table of Contents Abstract Introduction East Dunkard and West Dunkard Assessment units Introduction: Stratigraphy: Pottsville Formation Allegheny Group Conemaugh Group Monongahela Group Geologic Structure: Coalbed Methane Fields and Pools: Assessment Data: Coal as a source rock for CBM: Gas-In-Place Data Thermal Maturity Generation and Migration Coal as a reservoir for CBM: Porosity and Permeability Coal Bed Distribution Cumulative Coal Thickness Seals: Depth of Burial Water Production Cumulative Production Data: Pocahontas basin and Central Appalachian Shelf Assessment Units Introduction: Stratigraphy: Pocahontas Formation New River Formation Kanawha Formation 2 Lee Formation Norton Formation Gladeville Sandstone Wise Formation Harlan Formation Breathitt Formation Geologic Structure: Coalbed Methane Fields: Coal as a Source Rock for CBM Gas-in-Place Data Thermal Maturity Generation and Migration Coal as a Reservoir for CBM: Porosity and Permeability Coal Bed Distribution Cumulative Coal Thickness Seals: Depth of Burial Water Production Cumulative Production Data: Assessment Results: Appalachian Anthracite and Semi-Anthracite Assessment Unit: Pennsylvania Anthracite Introduction: Stratigraphy: Pottsville Formation Llewellyn Formation Geologic Structure: Coal as a Source Rock for CBM: Gas-In-Place-Data Thermal