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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 -
In the Matter of an Arbitration Under Chapter Eleven of the North American Free Trade Agreement and the Uncitral Arbitration Rules
Bilcon v. The Government of Canada Amended Statement of Defence December 18th, 2009 IN THE MATTER OF AN ARBITRATION UNDER CHAPTER ELEVEN OF THE NORTH AMERICAN FREE TRADE AGREEMENT AND THE UNCITRAL ARBITRATION RULES BETWEEN: WILLIAM RALPH CLAYTON, WILLIAM RICHARD CLAYTON, DOUGLAS CLAYTON, DANIEL CLAYTON, AND BILCON OF DELAWARE, INC. Claimants and GOVERNMENT OF CANADA Respondent AMENDED STATEMENT OF DEFENCE OF THE GOVERNMENT OF CANADA STATEMENT OF DEFENCE: May 4, 2009 AMENDED STATEMENT OF DEFENCE: DECEMBER 18, 2009 Departments of Justice and of Foreign Affairs and International Trade Trade Law Bureau Lester B. Pearson Building 125 Sussex Drive Ottawa, Ontario K1A 0G2 CANADA TABLE OF CONTENTS I. PRELIMINARY STATEMENT ..................................................................................... 1 II. FACTUAL BACKGROUND........................................................................................... 2 A. Digby Neck, Nova Scotia and the Claimants’ Proposal for a 152 Hectare Quarry and Marine Terminal............................................................................................... 2 1. Digby Neck – Environment, Community and Economy............................ 2 2. The Claimants’ Proposal for a 152 Hectare Quarry and Marine Terminal. 4 B. Environmental Assessment in Canada.................................................................... 4 1. The Canadian Environmental Assessment Act........................................... 5 2. The Nova Scotia Environment Act............................................................ -
Hurricane & Tropical Storm
5.8 HURRICANE & TROPICAL STORM SECTION 5.8 HURRICANE AND TROPICAL STORM 5.8.1 HAZARD DESCRIPTION A tropical cyclone is a rotating, organized system of clouds and thunderstorms that originates over tropical or sub-tropical waters and has a closed low-level circulation. Tropical depressions, tropical storms, and hurricanes are all considered tropical cyclones. These storms rotate counterclockwise in the northern hemisphere around the center and are accompanied by heavy rain and strong winds (NOAA, 2013). Almost all tropical storms and hurricanes in the Atlantic basin (which includes the Gulf of Mexico and Caribbean Sea) form between June 1 and November 30 (hurricane season). August and September are peak months for hurricane development. The average wind speeds for tropical storms and hurricanes are listed below: . A tropical depression has a maximum sustained wind speeds of 38 miles per hour (mph) or less . A tropical storm has maximum sustained wind speeds of 39 to 73 mph . A hurricane has maximum sustained wind speeds of 74 mph or higher. In the western North Pacific, hurricanes are called typhoons; similar storms in the Indian Ocean and South Pacific Ocean are called cyclones. A major hurricane has maximum sustained wind speeds of 111 mph or higher (NOAA, 2013). Over a two-year period, the United States coastline is struck by an average of three hurricanes, one of which is classified as a major hurricane. Hurricanes, tropical storms, and tropical depressions may pose a threat to life and property. These storms bring heavy rain, storm surge and flooding (NOAA, 2013). The cooler waters off the coast of New Jersey can serve to diminish the energy of storms that have traveled up the eastern seaboard. -
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. -
Hurricanes: a Century of Scientific Progress
Hurricanes: A Century of Scientific Progress Kerry Emanuel Program in Atmospheres, Oceans, and Climate Massachusetts Institute of Technology 1. Introduction In the early 20th century, at the same time that the theories of relativity and quantum mechanics were being developed, there was essentially no basic understanding of the physics of hurricanes. The energy cycle that sustains such storms was not known, nor were the factors that controlled their movement. What was known about the structure and behavior of hurricanes was inferred largely from visual observations of clouds and damage patterns, and it was widely believed that the storm circulation extended upward only a few kilometers. By the end of the century, the structure and behavior of hurricanes had been thoroughly quantified, thanks to rapid technological progress that brought about such wonders as aircraft, radar and satellites, and the basic physics of the storms themselves as well as their intricate substructure had come to be well understood. This new understanding, coupled with the invention and rapid development of the computer, made it possible to forecast the motion of hurricanes with such accuracy that, given modern communications and transportation, loss of life from hurricanes has been virtually eliminated in the developed world. This chapter chronicles the extraordinary progress in the scientific understanding of hurricanes through the 20th century. We begin with a brief review of progress through World War II, which marked an important turning point in the science of meteorology, and continue with an account of the rapid progress made in the first two decades after the war. Section 4 discusses the very influential CISK theory that was developed in the 1960s. -
Internal Stratigraphy of the Jurassic North Mountain Basalt, Southern Nova Scotia
Report of Activities 2001 69 • Internal Stratigraphy of the Jurassic North Mountain Basalt, Southern Nova Scotia D. J. Kontak Introduction sediments are exposed, only 9 m of Scots Bay Formation remain as remnant inliers along the The Jurassic (201 Ma, Hodych and Dunning, 1992) Scots Bay coastline (De Wet and Hubert, 1989). North Mountain Basalt (NMB; also referred to as the North Mountain Fonnation) fonns a prominent The NMB outcrops along the Bay of Fundy in cuesta along the southern coastline of the Bay of southern mainland Nova Scotia and is Fundy. These continental, tholeiitic basalt flows exceptionally well exposed along the coastline and have played an important role in the geological inland along river valleys (Fig. 1). Topographic heritage of the province by: (l) hosting some ofthe relief of the area bounding the Bay of Fundy earliest mineral resources exploited (e.g. Cu, Fe), reflects the distribution of the underlying massive (2) contributing to the character of zeolite basalt flows. No more obvious is this than along mineralogy (e.g. type locality for mordenite; How, the Annapolis Valley area where the west side of 1864), (3) fonning part of the Fundy Rift Basin, an the valley is composed of massive, fresh basalt of important part of the Mesozoic evolution of eastern the lower flow unit of the NMB. The proximity of North America, and (4) filling an important niche the area on the north side of the Bay of Fundy to in the aggregate operations of the province. Despite the east-west Cobequid-Chedabucto Fault Zone has the importance of the NMB there has been resulted in structural modifications to the otherwise relatively little recent work devoted to defining and simple stratigraphy of the NMB. -
Landform Generated: Nova Scotian Example
Landform Generated: Drumlin (an oval or elongated hill) Nova Scotian Example: Halifax Military Heritage Preservation Society Kuowaqe’jk, Big Pine Hill (Citadel Hill, Halifax) MAIN CULPRIT: WATER & ICE Halifax is known for this large drumlin overlooking the city, dropped by this culprit. Made of unsorted sediment, the drumlin was soft enough to carve Citadel Hill into it. This culprit also left behind a partially submerged drumlin in the harbour. Mélanie Léger, Radio-Canada, 2019 Landform Generated: Erratic (a rock that does not match the rocks of the area) Nova Scotian Example: Kjipanu’pek, Great bay opening out to the sea (Areas along St. Margaret’s Bay) MAIN CULPRIT: WATER & ICE These large granite boulders likely came from the North Mountain batholith and were deposited and exposed by this culprit around 10,000 years ago. Striations scraped into the boulders tell us the direction of the culprit’s movement. Michael C. Rygel, Wikimedia Commons Landform Generated: Lake Basin (the indent where the water of a lake collects) Nova Scotian Example: Pitu’pok/Pitu’paq, Long dish of saltwater/To which all things flow (Bras d’Or Lakes, Cape Breton) MAIN CULPRIT: WATER & ICE This culprit carved the basins of the Bras d’Or lakes, leaving behind stratified sediment. As the lake basins formed, they filled with fresh water, but as the sea level rose, they filled with sea water and marine life. Joseph Apaloo, Research Gate, Jan 2010 Landform Generated: Roche Moutonée (a bare rock with a smooth gentle slope side and a steep, rough cliff side) Nova Scotian Example: Nukumkikewe’jk, At the soft place (Taylor Head Provincial Park) MAIN CULPRIT: WATER & ICE This culprit slowly travelled up the soft sandstone bedrock, making the gradual slope on one side. -
Whale Tails & Other Stories.Pdf
B Greg Trowse photo Thank you to the people and businesses who contributed to this guide: Photos: Brier Island Whale & Seabird Cruises Mariner Cruises June Farnsworth Robert J. Galbraith Todd Sollows Amanda Stark/Freeport Whale & Seabird Tours Amy Tudor Mi’kmaw Ecological Knowledge: Robert McEwan Sandy-Lynn Fisher Lenley Melvin Alanna Syliboy Fred Phillips Interviewees: Artwork: Frank Gillis June Farnsworth Penny Graham Gerald Gloade Shelley Lonergan Patricia Sollows Laurie and Tony Thurber cover image by June Farnsworth Amy Tudor C Greg Trowse photo Contents 1.Prologue 57. Orca 4. Mi'kmaw Ecological Knowledge 61. Sperm whale 7. Species Names in Mi'kmaw 64. Seals 10. General Species Locations 65. Harbour seal 12. Common Cetacean Behaviours 68. Grey seal 19. The Baleen Whales 71. Leatherback turtle 21. Minke whale 74. Sharks 25. Humpback whale 77. Porbeagle shark 30. Sei whale 80. Shortfin mako shark 33. North Atlantic right whale 83. Blue shark 37. Fin whale 86. Thresher shark 40. Blue whale 89. Great white shark 43. Toothed Whales & Dolphins 92. Basking shark 45. Harbour porpoise 95. Ocean sunfish 48. Atlantic white-sided dolphin 98. Other Fish of the Bay of Fundy 51. Beluga whale 102. Artist Profiles 54. Long-finned pilot whale 106. References 108. Reporting Sightings and Animals in Distress Greg Trowse photo E Prologue incredible Bay of Fundy and her thick they sounded like rainstorms creatures. Th is is meant to be a pounding the ocean and looked With this guide we are looking to living, growing document that will like a writhing silver mat moving bring together traditional knowl- evolve alongside our understand- atop the water as they attempted edge, scientifi c understanding, and ing and as contributions are made. -
P3.4 the Distribution of Precipitation Over the Northeast Accompanying Landfalling and Transitioning Tropical Cyclones
20th Conf. on Weather Analysis and Forecasting Seattle, WA, 11–15 January 2004 P3.4 The Distribution of Precipitation over the Northeast Accompanying Landfalling and Transitioning Tropical Cyclones David P. DeLuca*, Lance F. Bosart, Daniel Keyser University at Albany, State University of New York, Albany, New York and David R. Vallee National Weather Service Forecast Office, Taunton, Massachusetts 1. INTRODUCTION United States. Approximately 3500 surface stations were analyzed for each storm period (currently: 1950– Landfalling and transitioning tropical cyclones 1991) by Ron Horwood of NWS WFO Taunton, MA. pose a significant heavy precipitation forecast challenge Obvious erroneous data were removed to obtain the most over the northeastern United States. The forecast accurate analyses possible. challenge is heightened because the heavy rainfall distribution associated with these tropical cyclones can A subset of eight storms (Fig. 1) where the be modulated significantly when the poleward-moving precipitation distribution is possibly influenced by storms interact with mobile midlatitude upper-level coastal frontogenesis was chosen from well–documented troughs and coastal fronts over regions of complex or famous cases. Detailed analyses were conducted terrain. The purpose of this paper is to document the using the four times daily (0000, 0600, 1200 and 1800 large spatial and temporal variability of heavy UTC) NCEP/NCAR reanalysis dataset (Kalnay et al. precipitation that accompanies landfalling and 1996; Kistler et al. 2001) and archived DIFAX surface transitioning tropical cyclones, and to determine the charts in an attempt to elucidate both synoptic and physical basis for the observed rainfall distribution. mesoscale processes. 2. METHODOLOGY 3. RESULTS A 38-storm dataset (Fig. -
Hurricanes in Maine: Past, Present, & Future
Hurricanes in Maine: Past, Present, & Future Kerry Emanuel Massachusetts Institute of Technology Some Famous Maine Hurricanes Hurricane Carol of 1954 in Maine Three deaths in Maine; 65 deaths and 1,000 injuries in New England $10 million in damages in Maine ($250 million in 2019 dollars) $500 million in damages, New England ($12.5 billion 2019) Peak wind gusts of 78 MPH in mid-coast Maine 2.25 inches of rain in places (not that much, but played into the Edna disaster a few weeks later) Power lost in all of greater Portland Most lobster fisherman reported damage Three-quarters of the Maine apple crop destroyed Falmouth, ME Portland, ME The Blaine Mansion, Augusta A scene in Maine during Carol Looking SW from Ocean Point, Boothbay during Carol 148-year-old steeple of the Old North Church in Boston falling during Hurricane Carol, 1954 Hurricane Edna of 1954 in Maine Eight deaths in Maine $25 million damage in Maine ($240 million in 2019 dollars) Peak wind gusts of 75 MPH in Maine Rainfall totals as high as 7.5 inches The Androscoggin and Kennebec rivers both reached above- normal levels, causing flooding and washing out roads President Eisenhower declared Maine a disaster area Harvard Beal's Bait Scow and Beal's Boat Yard, Southwest Harbor, during Hurricane Edna Memorial Highway near Dunn's Corner, Yarmouth (now Rt. 9) Damage to dam in Limestone, ME Remains of the drive-in movie theater in Rockport, ME, after Edna Article by E.B. White, The New Yorker, Sept. 25th 1954 (White resided in North Brooklin, Maine) Menemsha hurricane - Thomas Hart Benton (1954). -
Bilcon of Delaware, Inc
IN THE MATTER OF AN ARBITRATION UNDER CHAPTER ELEVEN OF THE NORTH AMERICAN FREE TRADE AGREEMENT AND THE UNCITRAL RULES OF 1976 (“UNCITRAL RULES”) - between - WILLIAM RALPH CLAYTON, WILLIAM RICHARD CLAYTON, DOUGLAS CLAYTON, DANIEL CLAYTON AND BILCON OF DELAWARE, INC. (the “Investors”) - and - GOVERNMENT OF CANADA (the “Respondent” and, together with the Investors, the “Parties”) AWARD ON JURISDICTION AND LIABILITY 17 MARCH 2015 ARBITRAL TRIBUNAL: Judge Bruno Simma (President) Professor Donald McRae Professor Bryan Schwartz SECRETARY: Dr. Dirk Pulkowski Permanent Court of Arbitration (PCA) Case No. 2009-04 PCA 122204 TABLE OF CONTENTS TABLE OF CONTENTS .............................................................................................................................. I GLOSSARY OF DEFINED TERMS ......................................................................................................... VII I. INTRODUCTION ....................................................................................................................... 1 A. THE PARTIES...................................................................................................................... 1 B. THE ESSENCE OF THE INVESTORS’ CASE ........................................................................ 2 C. THE ESSENCE OF THE RESPONDENT’S CASE ................................................................... 8 II. PROCEDURAL HISTORY ..................................................................................................... 11 A. COMMENCEMENT -
Forest Ecosystem Classification for Nova Scotia Part I: Vegetation Types (2010)
Forest Ecosystem Classification for Nova Scotia Part I: Vegetation Types (2010) prepared by Nova Scotia Department of Natural Resources REPORT FOR 2011-1 Tourism, Culture and Heritage Forest Ecosystem Classification for Nova Scotia Part I: Vegetation Types (2010) prepared by Nova Scotia Department of Natural Resources Peter Neily, Sean Basquill, Eugene Quigley, Bruce Stewart, Kevin Keys Nova Scotia Department of Natural Resources Renewable Resources Branch REPORT FOR 2011-1 Tourism, Culture and Heritage © Crown Copyright, Province of Nova Scotia, 2011. Forest Ecosystem Classification for Nova Scotia, Part I: Vegetation Types (2010) Prepared by the Nova Scotia Department of Natural Resources authors: Peter Neily1, Sean Basquill2, Eugene Quigley1, Bruce Stewart1, Kevin Keys1 Nova Scotia Department of Natural Resources, Renewable Resources Branch 1Forestry Division, Truro 2Wildlife Division, Kentville ISBN 978-1-55457-411-7 Photo credits All photos used in this guide unless credited were provided by the authors. Acknowledgements The authors wish to thank Susan Corning (Susan Corning Communications & Graphic Design) for her expertise and many hours spent bringing our field work and ideas to publishable form. We are indebted to Lawrence Benjamin and Pamela Mills (NSDNR Wildlife Division) for their assistance in VT fact sheet preparation. A special thanks goes to Catherine Turner-Robert (NSDNR Forestry Division) for her preparation of the distribution maps. Finally, we thank all our forestry colleagues inside and outside of NSDNR who have contributed to field work, promotion and use of FEC throughout the province. Your enthusiasm and support is very much appreciated. REPORT FOR 2011-1 Table of Contents Photo credits . 2 Acknowledgements . 2 List of Tables & Figures .