Prime Birding Locations in the Grand Manan Area
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My New Brunswick — GRAND MANAN Island
My ew runswick GRAND MANAN Island Grand Manan’s famous Swallowtail lighthouse. Story and photos by Larry Dickinson and Steve Rogers n a small island in the Bay of Fundy When you arrive on the ferry, you pass watching or sunset cruise. Olies a mystical place called Grand the iconic Swallowtail Lighthouse that Beaches on Grand Manan come in all Manan. It is a place of legends and lore, stands guard over the island and has done so sizes and shapes. The texture of the beaches and it’s only a 90-minute ferry ride from for 160 years. It is one of New Brunswick’s also changes. Many seem to endlessly the mainland. most photographed lighthouses and even stretch along the bays, coves and harbours The island is very peaceful and appears on a Canadian stamp. of the island. Seal Cove, Deep Harbour, relaxing, with its stunning scenery and Grand Manan is on the eastern fyway and the Anchorage are popular with natural resources. It has become a laid- for migratory birds. More than 400 species locals and visitors alike. You can spend a back paradise for kayakers, hikers and have been counted on the island. Every relaxing afternoon lying on the sand in the bird-watchers. The salt air and summer September, bird watchers travel to the warm sun and listening to the waves. Or sun seems to make everyday problems island and head to the marshes to see fnd treasures such as beach glass, pottery disappear. hundreds of bird species. shards, driftwood, shells and sand dollars The island’s rocky, cliff-lined coast, Puffns are a must-see during your visit. -
Geology of the Island of Grand Manan, New Brunswick: Precambrian to Early Cambrian and Triassic Formations
GEOLOGICAL ASSOCIATION OF CANADA / MINERALOGICAL ASSOCIATION OF CANADA JOINT ANNUAL MEETING 2014 UNIVERSITY OF NEW BRUNSWICK, FREDERICTON, NEW BRUNSWICK, CANADA FIELD TRIP B3 GEOLOGY OF THE ISLAND OF GRAND MANAN, NEW BRUNSWICK: PRECAMBRIAN TO EARLY CAMBRIAN AND TRIASSIC FORMATIONS MAY 23–25, 2014 J. Gregory McHone 1 and Leslie R. Fyff e 2 1 9 Dexter Lane, Grand Manan, New Brunswick, E5G 3A6 2 Geological Surveys Branch, New Brunswick Department of Energy and Mines, PO Box 6000, Fredericton, New Brunswick, E3B 5H1 i TABLE OF CONTENTS List of Figures and Tables..............................................................................................................i Safety............................................................................................................................................ 1 Itinerary ......................................................................................................................................... 2 Part 1: Geology of the Island of Grand Manan......................................................................... 3 Introduction ................................................................................................................................... 3 Precambrian Terranes of Southern New Brunswick ..................................................................... 3 Caledonia Terrane ............................................................................................................. 7 Brookville Terrane ............................................................................................................ -
Grand Manan Channel – Southern Part NOAA Chart 13392
BookletChart™ Grand Manan Channel – Southern Part NOAA Chart 13392 A reduced-scale NOAA nautical chart for small boaters When possible, use the full-size NOAA chart for navigation. Published by the 33-foot unmarked rocky patch known as Flowers Rock, 3.9 miles west- northwestward of Machias Seal Island, the channel is free and has a National Oceanic and Atmospheric Administration good depth of water. The tidal current velocity is about 2.5 knots and National Ocean Service follows the general direction of the channel. Daily predictions are given Office of Coast Survey in the Tidal Current Tables under Bay of Fundy Entrance. Off West Quoddy Head, the currents set in and out of Quoddy Narrows, forming www.NauticalCharts.NOAA.gov strong rips. Sailing vessels should not approach West Quoddy Head too 888-990-NOAA closely with a light wind. North Atlantic Right Whales.–The Bay of Fundy is a feeding and nursery What are Nautical Charts? area for endangered North Atlantic right whales (peak season: July through October) and includes the Grand Manan Basin, a whale Nautical charts are a fundamental tool of marine navigation. They show conservation area designated by the Government of Canada. (See North water depths, obstructions, buoys, other aids to navigation, and much Atlantic Right Whales, chapter 3, for more information on right whales more. The information is shown in a way that promotes safe and and recommended measures to avoid collisions with whales.) efficient navigation. Chart carriage is mandatory on the commercial Southwest Head, the southern extremity of Grand Manan Island, is a ships that carry America’s commerce. -
MCP No 02-E.Cdr
Silica Natural Resources Lands, Minerals and Petroleum Division Mineral Commodity Profile No. 2 ilicon (Si) is the second most common element on Earth after World Production and Reserves Soxygen. Si does not occur naturally in its pure state but instead is found chiefly in mineral form as either silica (SiO2) or silicates. Silica Silica deposits occur, and are mined, in most and/or silicate minerals are a constituent of nearly every rock type in countries. Global silica output is estimated at Earth's crust. roughly 120 Mt to 150 Mt per year (Dumont 2006). The most familiar silica mineral is quartz. In commodity terms, silica About 5.9 Mt of ferrosilicon were produced also refers to geological deposits enriched in quartz and/or other silica worldwide in 2006. The major contributors were minerals. Silica resources include 1) poorly consolidated quartzose China, Russia, United States, Brazil and South sand and gravel, 2) quartz sand/pebbles in consolidated rock (e.g. Africa (U.S. Geological Survey [USGS] 2006). quartzose sandstone), 3) quartzite , and 4) quartz veins. Global production of silicon metal reportedly Uses approached 1.2 Mt in 2006, almost half of which came from China (USGS 2006). Other important Silica is hard, chemically inert, has a high melting point, and functions producers are the United States, Brazil, Norway, as a semiconductor—characteristics that give it many industrial France, Russia, South Africa and Australia. applications. Silica deposits generally must be processed to remove iron, clay and other impurities. The most valuable resources contain Silica Consumption in Canada (Total = 2.57 Mt) >98% SiO2 and can be readily crushed into different sizes for the various end products. -
Real Property Issues in the Marine Aquaculture Industry in New Brunswick
REAL PROPERTY ISSUES IN THE MARINE AQUACULTURE INDUSTRY IN NEW BRUNSWICK SUE NICHOLS IAN EDWARDS JIM DOBBIN KATALIN KOMJATHY SUE HANHAM October 2001 TECHNICAL REPORT NO. 208217 REAL PROPERTY ISSUES IN THE MARINE AQUACULTURE INDUSTRY IN NEW BRUNSWICK Sue Nichols Ian Edwards Jim Dobbin Katalin Komjathy Sue Hanham Department of Geodesy and Geomatics Engineering University ofNew Brunswick P.O. Box 4400 Fredericton, N.B. Canada E3B 5A3 October 2001 PREFACE In order to make our extensive series of technical reports more readily available, we have scanned the old master copies and produced electronic versions in Portable Document Format. The quality of the images varies depending on the quality of the originals. The images have not been converted to searchable text. PREFACE This report was prepared under contract for the New Brunswick Department of Fisheries and Aquaculture. The research was carried out in 1997 at the University of New Brunswick, Fredericton, Canada, under the leadership of Professor Sue Nichols. As with any copyrighted material, permission to reprint or quote extensively from this report must be received from the authors. The citation to this work should appear as follows: Nichols, S., I. Edwards, J. Dobbin, K. Komjathy, and S. Hanham (2001). Real Property Issues in the Marine Aquaculture Industry in New Brunswick. Final contract report for the New Brunswick Department of Fisheries and Aquaculture, by the Geographical Engineering Laboratory, Department of Geodesy and Geomatics Engineering Technical Report No. 208, University of New Brunswick, Fredericton, New Brunswick, Canada, 102 pp. Real Property Issues in the Marine Aquaculture Industry in New Brunswick Acknowledgements The authors would like to thank for the Department of Fisheries and Aquaculture for recognising the need for this research and providing the funds. -
Machias Seal Island Mowad a R I MACHIAS SEAL ISLABD
Foet patK Bltn4 Machias Seal Island Mowad A r i MACHIAS SEAL ISLABD by Paula Butler, Belmont Machias Seal Island— the Contested Island*— has served as a sentinel at the South end of the Bay of Fundy slnce the estahlishment of a lighthouse in 1832. Before that time, this rock (barren except for a highland meadow in summer) vas a marinar's nightmare of sudden fog banks, high seas and hidden rocky shoals. The Harbour Seal, for whioh this island vas probably named, occurs only at a nearby shoal, North Rock. Although today's Journey is quite safe, trips to the island are cancelled vithout notice due to unexpected vind changes or a possible dangerous landing because of ground svells, strong cur- rents and surf. The meadov area of the island contains a variety of plant life: asters, vild parsleys, docks, grasses, sedges, and many other herbs. This island, like many others in the Machias Bay area, vas used for cattle and sheep grazing as vell as Limited farming. Some of these islands vere strategic in the naval maneuvers during the American Revolution. The first naval encounter of that var vas in Machias Bay vhen the villagers of Machias beached the British cutter Margareta. Most birders and photographers are attracted to Machias Seal Island to ob serve Common Puffins (Pratercula árctica) at cióse range. Common Puffins and Razorbills (Alca torda) seem to invite us not only to vatch them but to take delight in posing. Tvo blinds eire provided overlooking the rocky nesting area. The puffins arrive in late April and remain in the vater until they receive a mysterious signal; then, in one large flock, they settle into their nesting sites. -
Hon. J.W. Pickersgill MG 32, B 34
Manuscript Division des Division manuscrits Hon. J.W. Pickersgill MG 32, B 34 Finding Aid No. 1627 / Instrument de recherche no 1627 Prepared in 1991 by Geoff Ott and revised in Archives Section 2001 by Muguette Brady of the Political -ii- Préparé en 1991 par Geoff Ott et révisé en 2001 par Muguette Brady de la Section des Archives politiques TABLE OF CONTENTS PAGE PRE-PARLIAMENTARY SERIES ............................................... 1 SECRETARY OF STATE SERIES, 1953-1954 ..................................... 3 CITIZENSHIP AND IMMIGRATION SERIES ..................................... 4 Outgoing Correspondence - Sub-Series ........................................ 4 Citizenship - Sub-Series .................................................... 5 Estimates - Sub-Series .................................................... 28 National Gallery - Sub-Series .............................................. 32 National Film Board - Sub-Series ........................................... 37 Indian Affairs Branch - Sub-Series - Indian Act ................................. 44 Indian Affairs Branch - Sub-Series - General ................................... 46 Immigration - Sub-Series .................................................. 76 Immigration Newfoundland - Sub-Series ..................................... 256 Immigration - Miscellaneous - Sub-Series .................................... 260 Public Archives of Canada - Sub-Series ...................................... 260 National Library of Canada - Sub-Series .................................... -
2 Study Area
CA PDF Page 49 of 1038 Energy East Project Part B: Deterministic Modelling of the Ecological and Volume 24: Ecological and Human Health Risk Human Health Consequences of Marine Oil Spills Assessment for Oil Spills in the Marine Environment Section 2: Study Area 2 STUDY AREA The study area for the analysis of hypothetical crude oil spills for the proposed marine terminal is described in detail in Part A, Section 2 of the EHHRA. This section provides an overview. 2.1 Overview of Canaport Energy East Marine Terminal Operations and Expanded Shipping Operations The proposed marine terminal will be located on the western shore of the Bay of Fundy, southeast of the City of Saint John and southwest of Mispec Point, New Brunswick. The marine terminal is proposed to be located adjacent to the two existing Canaport marine facilities: a single buoy mooring (SBM or mono- buoy) for offloading crude oil to the Irving Canaport facility, and the Canaport LNG terminal for import and now recently licensed for export of liquefied natural gas (Figure 1-1). The marine terminal will include pile-supported trestles and breasting/mooring dolphins for two berths that can accommodate Aframax and Suezmax tankers (Berth 2), as well as VLCC tanker types (Berth 1), with capacities of 113,300 to 348,000 m3 (710,000 to 2.2 million barrels). The two berths will be constructed simultaneously. Oil will be pumped from shore via a trestle approximately 645 m long. Berths 1 and 2 will be interconnected by a trestle approximately 380 m long. The marine terminal is expected to receive approximately 281 tanker calls per year for shipping of crude oil products originating from western Canada. -
Seeing the Light: Report on Staffed Lighthouses in Newfoundland and Labrador and British Columbia
SEEING THE LIGHT: REPORT ON STAFFED LIGHTHOUSES IN NEWFOUNDLAND AND LABRADOR AND BRITISH COLUMBIA Report of the Standing Senate Committee on Fisheries and Oceans The Honourable Fabian Manning, Chair The Honourable Elizabeth Hubley, Deputy Chair October 2011 (first published in December 2010) For more information please contact us by email: [email protected] by phone: (613) 990-0088 toll-free: 1 800 267-7362 by mail: Senate Committee on Fisheries and Oceans The Senate of Canada, Ottawa, Ontario, Canada, K1A 0A4 This report can be downloaded at: http://senate-senat.ca Ce rapport est également disponible en français. MEMBERSHIP The Honourable Fabian Manning, Chair The Honourable Elizabeth Hubley, Deputy Chair and The Honourable Senators: Ethel M. Cochrane Dennis Glen Patterson Rose-Marie Losier-Cool Rose-May Poirier Sandra M. Lovelace Nicholas Vivienne Poy Michael L. MacDonald Nancy Greene Raine Donald H. Oliver Charlie Watt Ex-officio members of the committee: The Honourable Senators James Cowan (or Claudette Tardif) Marjory LeBreton, P.C. (or Claude Carignan) Other Senators who have participated on this study: The Honourable Senators Andreychuk, Chaput, Dallaire, Downe, Marshall, Martin, Murray, P.C., Rompkey, P.C., Runciman, Nancy Ruth, Stewart Olsen and Zimmer. Parliamentary Information and Research Service, Library of Parliament: Claude Emery, Analyst Senate Committees Directorate: Danielle Labonté, Committee Clerk Louise Archambeault, Administrative Assistant ORDER OF REFERENCE Extract from the Journals of the Senate, Sunday, June -
Triassic Basin Stratigraphy at Grand Manan, New Brunswick, Canada J
Document generated on 09/27/2021 4:33 p.m. Atlantic Geology Triassic Basin Stratigraphy at Grand Manan, New Brunswick, Canada J. Gregory. McHone Volume 47, 2011 Article abstract The island of Grand Manan (Canada) in the southwestern Bay of Fundy has the URI: https://id.erudit.org/iderudit/ageo47art06 only exposed strata and basalt of the Grand Manan Basin, a mainly submerged Early Mesozoic riſt basin about 30 km wide by 70 km long. The basin is See table of contents bounded on the southeast by the west-dipping Red Point Fault, which bisects the island, and on the northwest by a submarine border fault marked by the Murr Escarpment, a bathymetric feature that parallels the coast of Maine Publisher(s) (USA). A fault-bounded horst of Ediacaran to Cambrian rocks separates the Grand Manan Basin from the much larger Fundy Basin to the east. The Atlantic Geoscience Society Ashburton Head, Seven Days Work, and Southwest Head members of the end-Triassic Dark Harbour Basalt cover most of western Grand Manan with a ISSN total thickness around 240 m. Up to 12 m of sub-horizontal grey mudstone and fine-grained red sandstone of the Dwellys Cove Formation are exposed along 0843-5561 (print) the western shoreline beneath the basalt. Coarse red arkosic sandstone a few 1718-7885 (digital) metres thick at Miller Pond Road rests on a basement of Late Ediacaran rocks east of the basin. Exposures of the Dwellys Cove and Miller Pond Road Explore this journal formations are at the top and bottom, respectively, of several km (?) of sub-horizontal Late Triassic clastic basin strata, juxtaposed by the eastern border fault. -
New Brunswick Eastern Habitat Joint Venture Five Year Implementation Plan for the North American Waterfowl Management Plan
New Brunswick Eastern Habitat Joint Venture Five Year Implementation Plan for the North American Waterfowl Management Plan New Brunswick Eastern Habitat Joint Venture December 14 2007 Executive Summary The New Brunswick Eastern Habitat Joint Venture (NB-EHJV) was established in 1989 to implement the North American Waterfowl Management Plan (NAWMP) in New Brunswick through a partnership of federal, provincial and regional conservation organizations. The NB-EHJV Five Year Implementation Plan to be known as the Plan is an update of the 1989 – 2004 NB Eastern Habitat Joint Venture Implementation Plan. The Plan outlines the current status of wetland habitats and waterfowl populations in New Brunswick and presents waterfowl population goals and habitat conservation targets for the next five years. The Plan is a blueprint for the conservation of important breeding, staging and wintering waterfowl habitat in New Brunswick. It describes the habitat conservation program the NB- EHJV partnership will employ to achieve the waterfowl population objectives, the methods for program assessment and the resource needs. Though this Plan may benefit other bird species, it does not explicitly address the objectives for the other bird Pillars of the North American Bird Conservation Initiative (NABCI). The Plan will address 15% (1,105 IBP) of the 7,600 IBP population deficit for dabbling ducks (American black duck, Mallard, green-winged teal, ring-necked duck) in NB through the enhancement or restoration of 1,380 hectares of wetlands and the active management of 13,901 hectares of wetlands to optimum waterfowl brood rearing conditions. A nest box program will be used to increase wood duck and common goldeneye. -
Machias Seal Island Quartz Monzodiorite: the Southernmost Rocks in New Brunswick
72 AGS Abstracts – 2006 Annual General Meeting Machias Seal Island quartz monzodiorite: the southernmost rocks in New Brunswick Sandra M. Barr1, James K. Mortensen2, and Heather E. Wolczanski1, 1. Department of Geology, Acadia University, Wolfville, NS, B4P 2R6 <[email protected]> ¶ 2. Earth & Ocean Sciences, University of British Columbia, Vancouver, BC, V6T 1Z4 Machias Seal Island is located at the mouth of the Bay of Fundy, about 20 km south of Grand Manan Island and 20 km east of Machias, Maine. The island has an area of about 0.04 km2, and is barren except for a lighthouse and dwell- ings maintained by the government of Canada. It has the last manned lighthouse in the Maritime Provinces, and is well known among bird-watchers as a nesting site for puffi ns, auks, and other seabirds. Geologically, Machias Seal Island is important because of its location in an area through which it is diffi cult to trace terranes from the mainland of Nova Scotia and New Brunswick into the New England states. Studies in Grand Manan Island have not entirely resolved the problem, as rocks there most resemble those of the New River terrane of southern New Brunswick, suggesting that the Kingston, Brookville, Caldonia (Avalon), and Meguma terranes all lie outboard of Grand Manan Island. Machias Seal Island consists entirely of grey, locally pink, fi ne- to medium-grained weakly foliated quartz monzodiorite, gradational to granodiorite. Small ovoid metadioritic xeno- Atlantic Geology, 2006, Volume 42, Number 1 Copyright © 2015 Atlantic Geology Atlantic Geology 73 liths, generally less than 20 cm in maximum dimension, are abundant and consist of fi ne-grained granoblastic plagioclase, orthopyroxene, clinopyroxene, amphibole, and biotite.