Eolian Dune Field of Late Triassic Age, Fundy Basin, Nova Scotia'
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BLAZING the TRAIL in NOVA SCOTIA in Canada’S Second Ook Up, Way Up, Because Glooscap Is a Giant in Atlantic Canada’S Mi’Kmaq Culture
article and photos by Jan Napier BLAZING THE TRAIL IN NOVA SCOTIA In Canada’s second ook up, way up, because Glooscap is a giant in Atlantic Canada’s Mi’kmaq culture. This almighty being was of such gargantuan proportions that the smallest province, a province of Nova Scotia was his bed and Prince Edward Island his pillow. larger-than-life demigod, Ancient legends of the mythical creator live on, and there’s no better place Lto explore them than the spectacular Glooscap Trail in northwestern Nova Scotia. over-the-top scenery and The trail stretches 227 miles, all told, but our itinerary focuses on a 125-mile the world’s highest tides segment between Truro and Joggins. It’s a laid-back, mostly coastal drive, beloved by those in the know. set the stage for RV The Mi’kmaq (pronounced Meeg-mah), an indigenous people native to travels on a grand scale Canada’s Maritime Provinces and the Gaspé Peninsula of Quebec, once lived freely in this region. Silas Tertius Rand, a Baptist missionary who traveled among the Mi’kmaq in the mid- to late-1800s, documented their stories featuring the heroic Glooscap. He “lived like other men ... but he never died, never was sick, never grew old,” wrote Rand. “He could do anything and everything.” Traveling RVers can learn more about Mi’kmaq myths and culture, and stand — dwarfed — beneath the demigod’s towering bronze likeness, at the Glooscap Heritage Centre, less than 5 miles from Truro in Millbrook. If you’re lucky, Climb Five Islands Lighthouse Program Director Gordon Pictou or a heritage interpreter will be on hand to for panoramic views of the Bay of Fundy, Minas Basin and the share some of the Mi’kmaq creation stories, like the one about Five Islands. -
Regional Geology of the Scotian Basin
REGIONAL GEOLOGY OF THE SCOTIAN BASIN David E. Brown, CNSOPB, 2008 INTRODUCTION The Scotian Basin is a classic passive, mostly non-volcanic, conjugate margin. It represents over 250 million years of continuous sedimentation recording the region's dynamic geological history from the initial opening of the Atlantic Ocean to the recent post-glacial deposition. The basin is located on the northeastern flank of the Appalachian Orogen and covers an area of approximately 300,000 km2 with an estimated maximum sediment thickness of about 24 kilometers. The continental-size drainage system of the paleo-St. Lawrence River provided a continuous supply of sediments that accumulated in a number of complex, interconnected subbasins. The basin's stratigraphic succession contains early synrift continental, postrift carbonate margin, fluvial-deltaic-lacustrine, shallow marine and deepwater depositional systems. PRERIFT The Scotian Basin is located offshore Nova Scotia where it extends for 1200 km from the Yarmouth Arch / United States border in the southwest to the Avalon Uplift on the Grand Banks of Newfoundland in the northeast (Figure 1). With an average breadth of 250 km, the total area of the basin is approximately 300,000 km2. Half of the basin lies on the present-day continental shelf in water depths less than 200 m with the other half on the continental slope in water depths from 200 to >4000 m. The Scotian Basin formed on a passive continental margin that developed after North America rifted and separated from the African continent during the breakup of Pangea (Figure 2). Its tectonic elements consist of a series of platforms and depocentres separated by basement ridges and/or major basement faults. -
Preliminary Management Plan May 2009
NovaNova ScotiaScotia ProvincialProvincial ParksParks Preliminary Management Plan May 2009 Cape Split Provincial Park Reserve ...discover our nature 1.0 EXECUTIVE SUMMARY ..................................................1 2.0 INTRODUCTION .........................................................2 3.0 VISION ..................................................................3 Vision .................................................................3 4.0 PARK VALUES ...........................................................3 Natural Heritage .......................................................4 Geology .........................................................4 Marine Environment ..............................................4 Flora ...........................................................4 Fauna ...........................................................5 Cultural Heritage .................................................5 Outdoor Recreation .....................................................6 Outdoor Education .....................................................6 Tourism ...............................................................6 5.0 PARK OBJECTIVES ......................................................7 Protection .............................................................7 Outdoor Recreation .....................................................7 Heritage Appreciation ...................................................7 Tourism ...............................................................8 6.0 PARK CLASSIFICATION ..................................................8 -
On Cape Breton Island, Nova Scotia, Canada
Canadian Journal of Earth Sciences Remnants of Early Mesozoic basalt of the Central Atlantic Magmatic Province (CAMP) on Cape Breton Island, Nova Scotia, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2016-0181.R1 Manuscript Type: Article Date Submitted by the Author: 07-Nov-2016 Complete List of Authors: White, Chris E.; Nova Scotia Department of Natural Resources Kontak, DanielDraft J.; Department of Earth Sciences, Demont, Garth J.; Nova Scotia Department of Natural Resources Archibald, Douglas; Queens University, Department of Geological Sciences Keyword: CAMP, Mesozoic, Fundy Basin, Ashfield Formation https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 48 Canadian Journal of Earth Sciences 1 Remnants of Early Mesozoic basalt of the Central Atlantic Magmatic Province (CAMP) on Cape Breton Island, Nova Scotia, Canada Chris E. White 1, Daniel J. Kontak 2, Garth J. DeMont 1, and Douglas Archibald 3 1. Nova Scotia Department of Natural Resources, Halifax, Nova Scotia, B3J 3T9, Canada 2. Department of Earth Science, Laurentian University, Sudbury, Ontario, P3E 2C6, Canada 3. Department of Geological Sciences and Geological Engineering, Queens University, Kingston, Ontario, K7L 3N6, Canada Corrected version:Draft for re-submission to CJES November 7, 2016 ABSTRACT Amygdaloidal basaltic flows of the Ashfield Formation were encountered in two drillholes in areas of positive aeromagnetic anomalies in the Carboniferous River Denys Basin in southwestern Cape Breton Island, Nova Scotia. One sample of medium-grained basalt yielded a plateau age of 201.8 ± 2.0 Ma, similar to U-Pb and 40 Ar/ 39 Ar crystallization ages from basaltic flows and dykes in the Newark Supergroup. -
2019 Bay of Fundy Guide
VISITOR AND ACTIVITY GUIDE 2019–2020 BAYNova OF FUNDYScotia’s & ANNAPOLIS VALLEY TIDE TIMES pages 13–16 TWO STUNNING PROVINCES. ONE CONVENIENT CROSSING. Digby, NS – Saint John, NB Experience the phenomenal Bay of Fundy in comfort aboard mv Fundy Rose on a two-hour journey between Nova Scotia and New Brunswick. Ferries.ca Find Yourself on the Cliffs of Fundy TWO STUNNING PROVINCES. ONE CONVENIENT CROSSING. Digby, NS – Saint John, NB Isle Haute - Bay of Fundy Experience the phenomenal Bay of Fundy in comfort aboard mv Fundy Rose on a two-hour journey between Nova Scotia Take the scenic route and fi nd yourself surrounded by the and New Brunswick. natural beauty and rugged charm scattered along the Fundy Shore. Find yourself on the “Cliffs of Fundy” Cape D’or - Advocate Harbour Ferries.ca www.fundygeopark.ca www.facebook.com/fundygeopark Table of Contents Near Parrsboro General Information .................................. 7 Top 5 One-of-a-Kind Shopping ........... 33 Internet Access .................................... 7 Top 5 Heritage and Cultural Smoke-free Places ............................... 7 Attractions .................................34–35 Visitor Information Centres ................... 8 Tidally Awesome (Truro to Avondale) ....36–43 Important Numbers ............................. 8 Recommended Scenic Drive ............... 36 Map ............................................... 10–11 Top 5 Photo Opportunities ................. 37 Approximate Touring Distances Top Outdoor Activities ..................38–39 Along Scenic Route .........................10 -
Geological Map of the North Mountain Basalt from Cape Split to Brier Island, with Comments on Its Resource Potential
Report of Activities 2005 39 Geological Map of the North Mountain Basalt from Cape Split to Brier Island, with Comments on its Resource Potential D. J. Kontak Introduction preparation and will be published elsewhere (Kontak, in prep.), where it is demonstrated that the sequence corresponds to other continental flood The Jurassic North Mountain Basalt (NMB) forms basalt provinces (e.g. 65 Ma Deccan Traps, 17- a prominent cuesta along the southern coastline of 15 Ma Columbia River Basalt Group) that have the Bay of Fundy, and is contiguous with outliers analogues in the active flows of Hawaii. This along the northern side of the bay (Fig. 1). This correspondence provides a basis for interpreting the prominent topographic feature, roughly 200 km in volcanological features of the NMB (see Kontak, length, is the focus of this paper and the topic of 2002, for discussion). field studies over the past few years (Kontak, 2000, 2002; Kontak et al., 2005). One result of this work is the first geological map of this unit over the Geological Setting length of the North Mountain (Kontak, 2005, 2006), which provides a basis for assessment of the Numerous, early Mesozoic continental tholeiitic area’s resources. Previous work indicated that the basalt flows, dykes and sills formed along the NMB contained three distinct flow units, referred eastern margin of North America, concurrent with to as the Lower, Middle and Upper flow units the infilling of basins with non-marine sedimentary (Kontak, 2002), and the results of this work have rocks during Pangean rupture, as a prelude to the shown that this subdivision can be extended over opening of the present-day Atlantic Ocean. -
R E P O R T S 112 Structure of the Minas Passage, Bay of Fundy: A
Reports 112 Structure of the Minas Passage, Bay of Fundy: A Preliminary Report* DONALD J. P. SWIFT Duke University, Durham, N. C. FRANK L. JAGODITS Huntec Limited, Toronto, Ont. BERNARD L. MANISTRE Lockwood Survey Corporation Limited, Toronto, Ont. NORMAN R. PATERSON Huntec Limited, Toronto, Ont. Introduction From July, 1965 to March, 1966, a joint geological-geophysical study of the Minas Passage, Bay of Fundy, was undertaken by Huntec Limited of Toronto for the Atlantic Development Board of Canada. The purpose of the project was to test the feasibility of a tidal power station in the Passage. This paper presents a portion of the study, namely the structure of the geologically critical Minas Passage area and its bearing on regional structure. The Bay of Fundy is a funnel-shaped body of water lying between Nova Scotia and New Brunswick (Fig. 1). Fundy proper is 144 kilometers long, 100 kilometers wide at the base, and averages 75 meters in depth. The northeast end bifurcates into northeast-trending Chignecto Bay, and the east-trending Minas Basin. Three distinct bodies of water are included within the latter; the Minas Basin proper; the Minas Channel, separated from the basin by the great curved peninsula of Cape Blomidon-Cape Split; and the Minas Passage, connecting the Channel and the Basin (Fig. 2). ^Manuscript received 12 January, 1968. Reports 113 -V. N - ~M ' , , , - I . , I - I Figure 2 - The Minas Passage with Cape Split in the background. Stratigraphy Three well-defined bedrock sequences occur in the Minas Passage area. The Cobequid Complex is a lower Paleozoic metamorphic and igneous complex comprising the upraised Cobequid Fault Block (Fig. -
The Jurassic North Mountain Basalts, Nova Scotia: More Than Just Simple Flood Basalts1
188 Mineral Resources Branch The Jurassic North Mountain Basalts, Nova 1 Scotia: More Than Just Simple Flood Basalts D. J. Kontak The 201 Ma North Mountain Basalt (NMB) is a sequence of continental tholeiitic basalts erupted within a continental rift (Fundy Basin) that has been subdivided into lower, middle and upper flow units (LFU, MFU, UFU, respectively). Petrographically the basalts are medium- to fine-grained with ophitic textures and are variably vitrophyric (#30 %). Results of ongoing investigations of the features of the NMB are summarized below followed by inferences regarding their nature and origin. 1. The LFU (#190 to #40 m) is a medium- to coarse-grained, massive, columnar jointed basalt of dominantly holocrystalline texture with minor vitrophyre. The top few m are often amygdaloidal and mafic pegmatites local occur with felsic layers (#2-3 cm). Rarely spectacular Neptunian dykes (#20- 30 cm) are controlled by columnar jointing. Although the LFU forms a prominent valley wall along the Annapolis Valley, this topographic feature diminishes westwards. 2. The MFU contains numerous (4-16), variably thick (#1 to #25 m) flows with a laterally variable composite thickness (150 to 10 m) that decreases westwards. The basalts are fine- to medium-grained and contain abundant, variably textured mesostasis (#30-40%). The MFU is characterized by a systematic zonation of zeolites occluding primary vugs. Minor amounts of massive, fine-grained, homogeneous, red inter-flow sediment occurs as thin (cm scale) beds, and discordant vein networks or dykes; zeolites cross cut and locally replace the dyke rock. 3. The UFU (#160 m) consists of at least two or more flows and is similar to the LFU. -
Early Ornithischian Dinosaurs: the Triassic Record
Historical Biology An International Journal of Paleobiology ISSN: 0891-2963 (Print) 1029-2381 (Online) Journal homepage: https://www.tandfonline.com/loi/ghbi20 Early ornithischian dinosaurs: the Triassic record Randall B. Irmis , William G. Parker , Sterling J. Nesbitt & Jun Liu To cite this article: Randall B. Irmis , William G. Parker , Sterling J. Nesbitt & Jun Liu (2007) Early ornithischian dinosaurs: the Triassic record, Historical Biology, 19:1, 3-22, DOI: 10.1080/08912960600719988 To link to this article: https://doi.org/10.1080/08912960600719988 Published online: 10 Oct 2011. Submit your article to this journal Article views: 291 View related articles Citing articles: 70 View citing articles Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=ghbi20 Historical Biology, 2007; 19(1): 3–22 Early ornithischian dinosaurs: the Triassic record RANDALL B. IRMIS1, WILLIAM G. PARKER2, STERLING J. NESBITT3,4, & JUN LIU3,4 1Museum of Paleontology and Department of Integrative Biology, University of California, 1101 Valley Life Sciences Building, Berkeley, CA, 94720-4780, USA, 2Division of Resource Management, Petrified Forest National Park, P.O. Box 2217, Petrified Forest, AZ, 86028, USA, 3Lamont–Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades, NY, 10964, USA, and 4Division of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, NY, 10024, USA Abstract Ornithischian dinosaurs are one of the most taxonomically diverse dinosaur clades during the Mesozoic, yet their origin and early diversification remain virtually unknown. In recent years, several new Triassic ornithischian taxa have been proposed, mostly based upon isolated teeth. -
Guide to the Mesozoic Redbeds of Central Connecticut
I I I Guide to the Mesozoic Redheds I of I Central Connecticut I JOHN F. HUBERT, ALAN A. REED, I WAYNE L. DOWDALL, and J. MICHAEL GILCHRIST I I I STATE GEOLOGICAL AND NATURAL HISTORY SURVEY OF CONNECTICUT DEPARTMENT OF ENVIRONMENTAL PROTECTION 1978 GUIDEBOOK NO. 4 On the cover: In the early morning along the shore of on East Berlin Lake, the 7-m phytosour Rutiodon snatches a Semionotus from the sho I lows. The tall horsetail Equisetum and cycad Otozomiles thrive in the wet mud of the lake strand. Stands of the conifer Aroucarioxylon tower 60 m high along the distant horizon on sandy soils of the well drained uplands. The dinosaur Eubronfes passed this way the previous evening. Sketch by Amy S. Hubert STATE GEOLOGICAL AND NATURAL HISTORY SURVEY OF CONNECTICUT DEPARTMENT OF ENVIRONMENTAL PROTECTION } } ] GUIDE TO THE MESOZOIC REDBEDS OF CENTRAL CONNECTICUT JOHN F. HUBERT J University of Massachusetts ALAN A. REED ) Chevron Oil Company WAYNE L • DOWDALL Weston Geophysical Resea:t>ch J. MICHAEL GILCHRIST Texaco Oil Company ,-------,_r-- -----------, i 1 i I 1 I ~ l ; .J J 1978 J GUIDEBOOK NO. 4 J J ii STATE GEOLOGICAL AND NATURAL HISTORY SURVEY OF CONNECTICUT THE NATURAL RESOURCES CENTER DEPARTMENT OF ENVIRONMENTAL PROTECTION Honorable Ella Grasso, Governor of Connecticut Stanley J. Pac, Connnissioner of the Department of Environmental Protection STATE GEOLOGIST DIRECTOR, NATURAL RESOURCES CENTER Hugo F. Thomas, Ph.D. This guidebook is a reprint of "Guide to the Redbeds of Central Connecticut: 1978 Field Trip, Eastern Section of the Society of Economic Mineralogists and Paleontologists." It was originally published as Contribution No. -
Wolfville Historical Society and Randall House Museum
WOLFVILLE HISTORICAL SOCIETY ARCHIVAL COLLECTION STORED AT ESTHER CLARK WRIGHT ARCHIVES ACADIA UNIVERSITY FINDING AID WHS PHOTOGRAPH COLLECTION updated to May 1, 2016 Researchers wishing to access photographs or other boxes should contact the Curator at 542-9775 from June to September, or the WHS Archivist at 542-5061. The photograph boxes are still being actively worked on and photographs are sometimes difficult to access. Note: the data base back-up disk is in box 6a Note: A large photograph collection relating to the W.H. Chase family is part of the Chase fonds, 06.01. See finding aid for the historical collection for description. Boxes 6a through to 6x Photographs & Postcards Box 6a CC 373 to CC 430 [entered & scanned. Worksheets and discs for 6a plus the backup Passage d.b. and images folder, created March 10, 2008 are stored separately] CC 373 post card, Presbyterian Church on fire, August 14, 1913 CC 374 arrival of J.W. Regan party (tentative id) at Railway Station, 1900 CC 375 Wolfville Cadets marching on Main Street outside MT&T, ca 1940s CC 376 Wolfville Harbour with Skoda building, boy fishing from log raft CC 377 original sepia print, very clear,Wolfville Harbour at low tide CC 378 sepia post card, Gaspereau Valley from the Stile CC 379 interior of a church, decorated with flags and flowers (see also 03.12.1 for a similar church interior which may identify this as the 2nd Baptist Church) CC 380 snapshot, Godfrey House on Main Street, ca 1920 CC 381 studio portrait of two women, taken in Kamloops, B.C. -
Fundy Tidal Energy Demonstration Project Volume I: Environmental Assessment
Fundy Ocean Research Centre for Energy (Minas Basin Pulp and Power Co. Ltd.) Environmental Assessment Registration Document – Fundy Tidal Energy Demonstration Project Volume I: Environmental Assessment Project Number 107405 June 2009 Minas Basin Pulp and Power Volume 1: Environmental Assessment Fundy Tidal Energy Demonstration Facility Final for submission Prepared by: AECOM Canada Ltd. 1701 Hollis Street, SH400 (PO Box 576 CRO), Halifax, NS, Canada B3J 3M8 T 902.428.2021 F 902.428.2031 www.aecom.com Project Number: 107405 Date: June 10, 2009 Minas Basin Pulp and Power Volume 1: Environmental Assessment Fundy Tidal Energy Demonstration Facility Statement of Qualifications and Limitations © 2009 AECOM CANADA LTD. ALL RIGHTS RESERVED. THIS DOCUMENT IS PROTECTED BY COPYRIGHT AND TRADE SECRET LAW AND MAY NOT BE REPRODUCED IN ANY MANNER, EXCEPT BY CLIENT FOR ITS OWN USE, OR WITH THE WRITTEN PERMISSION OF AECOM CANADA LTD. The attached Report (the “Report”) has been prepared by AECOM Canada Ltd. (“Consultant”) for the benefit of the client (“Client”) in accordance with the agreement between Consultant and Client, including the scope of work detailed therein (the “Agreement”). The information, data, recommendations and conclusions contained in the Report: • are subject to the budgetary, time, scope, and other constraints and limitations in the Agreement and the qualifications contained in the Report (the “Limitations”); • represent Consultants’ professional judgement in light of the Limitations and industry standards for the preparation of similar