The Smelt Fishery

Total Page:16

File Type:pdf, Size:1020Kb

The Smelt Fishery BAY OF FUNDY SURVEY The Smelt Fishery By G. W. Jeffers I. Name It is not at all certain why this excellent little fish came to be called "ameLt.!". At first glance the name appears to be merely a shortening of "smeLf it" from the fact that the fish has a peculiar and characteristic odor. This odor has been compared with that of cucumber or garlic, and hence the name. In Germany it is s aid to be called list inkfisc h II, and we know t hat the European smelt smells so strongly as to be objectionable. Certainly the odor given off by the American smelt is never very noticeable. It has been suggested that the word 'smelt' was first used lIin the sense of smelting metals and was derived from the trans­ parent app ear-anc e of the r i e h.." Then again, it is ¢.fttiifJ'fi claimed that the word comes from the Anglo-Saxon "ameol t " signifying smooth and shiny, in much the same manner that the young salmon ll• is termed a II s mo l t In Norway there are two varieties of smelt - the large smelt, or " s1om", and a smaller one with a more pungent, odor, called "n o r a". In Germany it is called "atan t , seestint, and grosser s t ant". In England it is known as smelt or sparling, and 2 this last name is sometimes met with in Germany also. In Holland it goes under the name %p~f spiering ar spearling. In Denmark it is called' smaelt'; in Finland 'norssi' and knore'; in France , eperlan' ; and in Russia' korjuschka' . 'Smelt' is about the only name given to it in this country, although a few older fishermen frequently refer to it as 8icefisb' or' fro s t f ishr • The name smelt is incorrectly a pplied to a lesser Whitefish, (Argyrosomus o~meriformis), on many lakes in New York state. Likewise, a small minnow (N ~ropis hudsonius) that ranges from the Great lakes to South Carolina, is sometimes called smelt. The scientific name of the common ,s mel t of our Atlantic coasts is Osmerus mordax. Our fish is regarded as a distinct species from that on the Pacmfic coasts (Osmerus ~eatex), and from the European smelt (Osmerus eperlanus) Some smelts are permanent residents of fresh water, but these probably belong to t De same species as the common marine smelt. In certain lakes, as for example, La~e Champaain a n d lake Utopia in New Br~~swick, the land-locked smelts are of two kinds, a large variety Which is very little, if any, smaller than the sea form, and a smaller Ki n d which 1s only five or six inches in length. Dr. McGonigle informs me that it has been suggested to him that the large land-locked type are native to \ to the lakes in question whereas the smaller ones have been \ J i n t r od uc e d from hatcheries. These small smelt are matu~r fish. /' In the Miramichi river small smelts are called "b.l anka!". 3 I L .P icture No good on e available See, Kendall "I'ne Smelts II Bigelow and We l ah 4 III. Economic Importance Formerly the smelt was considered of only minor importance as a food fish, and people generally used it a s a fertilizer. For example, in 1867 Knight wrote tl It seems almost an offence to claim for the smelt a relationship with the elite family of the salmonidae; nevertheless naturalists persist in calling it a salmon. II To-day we offer no a,Pology for considering the smelt as a relative of the salmon, for even if very little is ever heard of the smelt fishery this fishery has already attained considerable magnitude. The fish first assumed importc.:..nce in New Jersey and southern New England in the sixtes , but in recent years the co mmercial smelt fishery has gradualiliy receded northwards, and to-day the quantity taken south of Maine is negligible. Canada is t he most important smelt-producing country in the world; about three-fourths of the world's smelts come from Canada and the Miramichi river, in Quebec, l i s responsible for one-third of the total Canadia,n production. JJp r i o r to 1908 the markets of central Canada were supplied from New England. In that year the Department embarked on the policy . ~ of paying one-third of t he express charges on less-than-carload lot shipments from the Atlantic ports. By 1918 the quantity of fresh fish so shipped had increased 300%. About 90,000,000 ibs ' o f fresh fish are annually marketed from the Mi.ritimes. n Can.Fish. In 1914, a record year, 9,038,900 pounds of smelt, valued at $7 13 , 5 0 1 were recorded from the Dominion; in 1923 When the catch was only 5,811,800 pounds the value was considerably greater, being $78 9 , 36 1 . Whe r e a s the bay of Fundy may be considered a fair smelt area ~_ ~.~ tr~-~ I 70 (.~ H.t' f. I r: ,.. <> ~' f " . ~ ~:.--t-7 {'-. 6 IV. Methods of Capture The principal methods of taking smelt are by bag-nets, box-nets, gill-nets, hook-and-line, spearing and by weirs set for sardines. The first two methods, the bag-net and box-net, are restricted to l ar g e rivers that freeze over in the Winter and at the same time have a good run of tide, such as the Miramichi river. Because of the absence of these conditions in the Fundy area bag-nets and box nets are not used. Two or three years ago bay-nets were tried out at Drury cove on the Kennebecasis river, but it was ~ found that they did not pay and so were abandonned. Gill-nets, commonly called smelt nets, are in pretty general use in the Fundy region, particularly in Charlotte county. They are employe~ in the fall and spring When the fish are congregated , } outside the mouths of the rivers. Hook-and-line is the method used after the rivers have frozen over, by simply cutting holes in the ice and fishing through these. When smelting is indulged in for its excellent sport value this is the method par excellane~; the fish not only take bait but will rise to the fly as well. It is interesting to note that Yarmouth county has abolished all other methods of taking smelt, and relies on hook-and-line entirely. This method gives an equal opportunity to all the people, it is less harmful to the fish and less destr­ uctive ~¢/~~~ than gill nets, hence the fish are of a better and more uniform qualityhnd so 'grade' better. This is an excellent ! example of cooperation among fishermen to conserve a really good source of income. The Yarmouth smelt fishery is the most impor­ tant in the Fundy region, and Yarmouth smelt because of their 7 quality always command a good price. The best bait seems to be worms, particularly the sand worm (Nereis) which is dug from the sand flats and are sold locally or else shipped by mail in the frozen state. The price is around twenty-five cents per dozen. Another g ood bait is eel meat which has been colored red by means of a diamond dye. In other sections especially around the bead of the bay beef i6 used for bait. Formerly spearing for smelt was indulged in t u a consider­ able extent, but in general the fishermen have found out that the practice does not pay, particularly if the fish are to be offered for sale, since the appe~rance of the fish plays an important part in the eyes of the consumer. For home consumption smelt are still taken by spearing aroun~ the head of the bay. The type of spear used is shown in t he accompanying diagram. It consists of a wooden handle in one end of which is a stout needle. fWo metal springs, one opposite the other, are attached to the wood enclosing the ~¢¢ needle. These springs are made of the ribs of an umbrella and their purpose is to hold the fish that has been pierced by the neeale until it can be landed on the ice. During t he summer when the sardine weirs are being worked, fair catches of smelt are sometimes made along with the sardines. Technically this is the closed season for smelt, but smelt taken in weirs are not regarded as being captured illegally and so are subject to sale. 8 When the smelt have gathered in the rivers to spawn the dip-net is frequently used for taking them. Occasionally, too, poachers use this method for illega~ fishing in closed seasons. 9 V. Horizontal Distribution in the Fundy Area The distribution of smelt in the Fundy area is presented in figure I This distribution is based upo n the average catch for the five years 1910- 19,1 , the figures being taken from the government statistics. It will be noticed that the smelt, like most of the other commercial fishes, is more concentrated around the mouth af the bay and become scarcer towards the head of the bay. In this latter reBion the published statistics may not give an adaquate idea of the abundance of smelt due to a lack of any substantial p rov i s i on for taking them. Yarmouth county on t he Nova Scotia side of the bay is the most important smelt district, with Charlotte county in New Brunswick a close second.
Recommended publications
  • Canada 21: Shepody Bay, New Brunswick
    CANADA 21: SHEPODY BAY, NEW BRUNSWICK Information Sheet on Ramsar Wetlands Effective Date of Information: The information provided is taken from text supplied at the time of designation to the List of Wetlands of International Importance, May 1987 and updated by the Canadian Wildlife Service - Atlantic Region in October 2001. Reference: 21st Ramsar site designated in Canada. Name and Address of Compiler: Canadian Wildlife Service, Environment Canada, Box 6227, 17 Waterfowl Lane, Sackville, N.B, E4L 1G6. Date of Ramsar Designation: 27 May 1987. Geographical Coordinates: 45°47'N., 64°35'W. General Location: Shepody Bay is situated at the head of the Bay of Fundy, 50 km south of the City of Moncton, New Brunswick. Area: 12 200 ha. Wetland Type (Ramsar Classification System): Marine and coastal wetlands: Type A - marine waters; Type D - rocky marine shores and offshore islands; Type F - estuarine waters; Type G -intertidal mud, sand, and salt flats; Type H - intertidal marshes. Altitude: Range is from - 6 to 6 m. Overview (Principle Characteristics): The area consists of 7700 ha of open water, 4000 ha of mud flats, 800 ha of salt marsh and 100 ha of beach. Physical Features (Geology, Geomorphology, Hydrology, Soils, Water, Climate): The area is situated at the head of the Bay of Fundy, an area with the largest tidal range in the world (up to 14 m in Shepody Bay). Shepody Bay is a large tidal embayment surrounded by low, rolling upland. A narrow band of salt marsh occurs along the western shore, whereas the eastern side is characterised by a rocky, eroding coastline with sand- gravel beaches.
    [Show full text]
  • Tusket River & Basin
    Tusket River & Basin Introduction The Tusket River presents an area of 3000 square kilometres (1158 square miles) on the southwestern tip of Nova Scotia. The area consists of a coastal basin with an inland watershed associated with the great Tusket River. This name is derived from a Mi'kmaq word "Neketaouksit" meaning "Great Forked Tidal River". This unique and diverse environment has offered natural resources to the Mi'kmaq First Nation's people for 7000 years and to the French Acadian settlers since the early 17th century. In the context of sustainable development, the present-day Acadians can offer a bilingual ecotourism package of nature-adventure and discovery blended with local history and heritage. The following natural history of the area will be presented in two segments. The first section will describe the natural environment of the Tusket Basin and its interrelationships with the Acadian people. The second segment will describe the natural history of the Tusket River in a similar manner to present the Acadian in his natural environment. Basin description 1. Physical features The Tusket Basin has a width of 32 kilometres (20 miles) between headlands at Chebogue Point and Lower East Pubnico. The mainland coastline between these two boundaries is highly indented and irregular with a measure of 500 kilometres (310 miles). Elongated points, peninsulas, ridges, drumlins (low hills) and eskers are oriented North-South and are separated by many tidal channels, inlets, estuaries and bays. High tide in the estuary of the "great forked tidal river" (Tusket) carries salt water inland for 24 kilometres (15 miles).
    [Show full text]
  • A Review of Ice and Tide Observations in the Bay of Fundy
    A tlantic Geology 195 A review of ice and tide observations in the Bay of Fundy ConDesplanque1 and David J. Mossman2 127 Harding Avenue, Amherst, Nova Scotia B4H 2A8, Canada departm ent of Physics, Engineering and Geoscience, Mount Allison University, 67 York Street, Sackville, New Brunswick E4L 1E6, Canada Date Received April 27, 1998 Date Accepted December 15,1998 Vigorous quasi-equilibrium conditions characterize interactions between land and sea in macrotidal regions. Ephemeral on the scale of geologic time, estuaries around the Bay of Fundy progressively infill with sediments as eustatic sea level rises, forcing fringing salt marshes to form and reform at successively higher levels. Although closely linked to a regime of tides with large amplitude and strong tidal currents, salt marshes near the Bay of Fundy rarely experience overflow. Built up to a level about 1.2 m lower than the highest astronomical tide, only very large tides are able to cover the marshes with a significant depth of water. Peak tides arrive in sets at periods of 7 months, 4.53 years and 18.03 years. Consequently, for months on end, no tidal flooding of the marshes occurs. Most salt marshes are raised to the level of the average tide of the 18-year cycle. The number of tides that can exceed a certain elevation in any given year depends on whether the three main tide-generating factors peak at the same time. Marigrams constructed for the Shubenacadie and Cornwallis river estuaries, Nova Scotia, illustrate how the estuarine tidal wave is reshaped over its course, to form bores, and varies in its sediment-carrying and erosional capacity as a result of changing water-surface gradients.
    [Show full text]
  • Lady Crabs, Ovalipes Ocellatus, in the Gulf of Maine
    18_04049_CRABnotes.qxd 6/5/07 8:16 PM Page 106 Notes Lady Crabs, Ovalipes ocellatus, in the Gulf of Maine J. C. A. BURCHSTED1 and FRED BURCHSTED2 1 Department of Biology, Salem State College, Salem, Massachusetts 01970 USA 2 Research Services, Widener Library, Harvard University, Cambridge, Massachusetts 02138 USA Burchsted, J. C. A., and Fred Burchsted. 2006. Lady Crabs, Ovalipes ocellatus, in the Gulf of Maine. Canadian Field-Naturalist 120(1): 106-108. The Lady Crab (Ovalipes ocellatus), mainly found south of Cape Cod and in the southern Gulf of St. Lawrence, is reported from an ocean beach on the north shore of Massachusetts Bay (42°28'60"N, 70°46'20"W) in the Gulf of Maine. All previ- ously known Gulf of Maine populations north of Cape Cod Bay are estuarine and thought to be relicts of a continuous range during the Hypsithermal. The population reported here is likely a recent local habitat expansion. Key Words: Lady Crab, Ovalipes ocellatus, Gulf of Maine, distribution. The Lady Crab (Ovalipes ocellatus) is a common flats (Larsen and Doggett 1991). Lady Crabs were member of the sand beach fauna south of Cape Cod. not found in intensive local studies of western Cape Like many other members of the Virginian faunal Cod Bay (Davis and McGrath 1984) or Ipswich Bay province (between Cape Cod and Cape Hatteras), it (Dexter 1944). has a disjunct population in the southern Gulf of St. Berrick (1986) reports Lady Crabs as common on Lawrence (Ganong 1890). The Lady Crab is of consid- Cape Cod Bay sand flats (which commonly reach 20°C erable ecological importance as a consumer of mac- in summer).
    [Show full text]
  • Minas Basin, N.S
    An examination of the population characteristics, movement patterns, and recreational fishing of striped bass (Morone saxatilis) in Minas Basin, N.S. during summer 2008 Report prepared for Minas Basin Pulp and Power Co. Ltd. Contributors: Jeremy E. Broome, Anna M. Redden, Michael J. Dadswell, Don Stewart and Karen Vaudry Acadia Center for Estuarine Research Acadia University Wolfville, NS B4P 2R6 June 2009 2 Executive Summary This striped bass study was initiated because of the known presence of both Shubenacadie River origin and migrant USA striped bass in the Minas Basin, the “threatened” species COSEWIC designation, the existence of a strong recreational fishery, and the potential for impacts on the population due to the operation of in- stream tidal energy technology in the area. Striped bass were sampled from Minas Basin through angling creel census during summer 2008. In total, 574 striped bass were sampled for length, weight, scales, and tissue. In addition, 529 were tagged with individually numbered spaghetti tags. Striped bass ranged in length from 20.7-90.6cm FL, with a mean fork length of 40.5cm. Data from FL(cm) and Wt(Kg) measurements determined a weight-length relationship: LOG(Wt) = 3.30LOG(FL)-5.58. Age frequency showed a range from 1-11 years. The mean age was 4.3 years, with 75% of bass sampled being within the Age 2-4 year class. Total mortality (Z) was estimated to be 0.60. Angling effort totalling 1732 rod hours was recorded from June to October, 2008, with an average 7 anglers fishing per tide. Catch per unit effort (Fish/Rod Hour) was determined to be 0.35, with peak landing periods indicating a relationship with the lunar cycle.
    [Show full text]
  • 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
    [Show full text]
  • The Annapolis Basin Scallop Fishery: a Historical Perspective and 1993 Stock Assessment
    Scientific Excellence • Resource Protection & Conservation • Benefits for Canadians Excellence scientifique • Protection et conservation des ressources • Bénéfices aux Canadiens DFO Library MPO - Bbliothèque III IIIIHIIIIJIIII II I/9-- - 12022666 The Annapolis Basin Scallop Fishery: A Historical Perspective and 1993 Stock Assessment E. L. Kenchington and M. J. Lundy Benthic Fisheries and Aquaculture Division Biological Sciences Branch Department of Fisheries and Oceans P.O. Box 550 Halifax, Nova Scotia B3J 2S7 1994 Canadian Manuscript Report of Fisheries and Aquatic Sciences No. 2230 5-é-/ 23 Fisheries Pêches 1+1 and Oceans et Océans Canada. Canadian Manuscript Report of Fisheries and Aquatic Sciences Manuscript reports contain scientific and technical information that contributes to existing knowledge but which deals with national or regional problems. Distribu- tion is restricted to institutions or individuals located in particular regions of Canada. However, no restriction is placed on subject matter, and the series reflects the broad interests and policies of the Department of Fisheries and Oceans, namely, fisheries and aquatic sciences. Manuscript reports may be cited as full publications. The correct citation appears above the abstract of each report. Each report is abstracted in Aquatic Sciences and Fisherics Abstracts and indexed in the Department's annual index to scientific and technical publications. Numbers 1-900 in this series were issued as Manuscript Reports (Biological Series) of the Biological Board of Canada, and subsequent to 1937 when the name of the Board was changed by Act of Parliament, as Manuscript Reports ( Biological Series) of the Fisherics Research Board of Canada. Numbers 901-1425 were issued as Manuscript Reports of the Fisheries Research Board of Canada.
    [Show full text]
  • Annapolis Basin Bay of Fundy Estuary Profile Annapolis Basin
    Bay of Fundy Estuary Profiles Annapolis Basin Bay of Fundy Estuary Profile Annapolis Basin The Annapolis Basin is a sub-basin of the Bay of Fundy along the northwestern shore of Nova Scotia and at the western end of the Annapolis Valley. The Annapolis River is the major water source flowing into the estuary. At the NB mouth of the estuary, a narrow channel known as the Digby Gut connects the 44 NS estuary to the Bay of Fundy. Annapolis Royal and Digby are the main communities along the shore of the estuary, and Kingston-Greenwood is within the catchment area. Near Digby, there is a ferry port that connects to Saint John, New Brunswick. The estuary also hosts a tidal power generating station, which is near Annapolis Royal. The economy within the catchment area is largely driven by agriculture. However, Estuary surface area 104.07 km2 there are also several shellfish and finfish aquaculture tenures, and some Width at estuary mouth 1.85 km commercial fisheries near the mouth of the estuary that largely target Shoreline length 200.63 km invertebrates such as crab, lobster, and clams that inhabit tidal mudflats. The Catchment area 2322.05 km2 extensive tidal mudflats within the estuary are important habitat for Shorebird colonies 2 shorebirds. Within the catchment area there is freshwater habitat for wood Protected area 94.81 km2 turtles, and two protected areas that overlap with the landward boundary of Paved roads 1028 km the estuary. Although the upper valley is primarily agricultural land, much of Aquaculture leases 10 the rest of the catchment area is covered by forest.
    [Show full text]
  • Modelling the Sea Level in the Upper Bay of Fundy
    Modelling the sea level in the upper Bay of Fundy Fred´ eric´ Dupont, Charles G. Hannah, David Greenberg Fisheries and Oceans Canada, Bedford Institude of Oceanography, P.O. Box 1006, Dartmouth, N.S. Canada B2Y 4A2 December 9, 2003 Abstract A high resolution model of the upper Bay of Fundy was developed to simulate the tides and sea level. The model includes the wetting and drying (inundation) of the extensive tidal flats in Minas Basin. The model reproduces the dominant M2 tidal harmonic with an error of order 0.30 m, and the total water level in Minas Basin with an RMS error of 0.30-0.50 m. Overall the system is capable of simulation with sea level error of 8-11%. The motivation for the model development was the simulation of the land/water interface (instantaneous coastline) to aid in the validation of coastline retrieval algorithms from remotely sensed observations. Qualitative comparison of observed and simulated coastlines showed that the misfit was dominated by errors in the details of the local topography/bathymetry. For example, long narrow features such as dykes are difficult to resolve in a dynamical model but are important for inundation of low lying areas. 1 1 Introduction This paper reports on the development of a sea level prediction system for the upper Bay of Fundy (Fig. 1). The motivation is the simulation of the land-water boundary (instanta- neous coastline) in the Bay as part of the validation of the land-water boundary extracted from remotely sensed observations (e.g. RADARSAT-1, polarimetric SAR, CASI, Land- sat and Ikonos imagery) as described by Deneau (2002) and Milne (2003).
    [Show full text]
  • South Western Nova Scotia
    Netukulimk of Aquatic Natural Life “The N.C.N.S. Netukulimkewe’l Commission is the Natural Life Management Authority for the Large Community of Mi’kmaq /Aboriginal Peoples who continue to reside on Traditional Mi’Kmaq Territory in Nova Scotia undisplaced to Indian Act Reserves” P.O. Box 1320, Truro, N.S., B2N 5N2 Tel: 902-895-7050 Toll Free: 1-877-565-1752 2 Netukulimk of Aquatic Natural Life N.C.N.S. Netukulimkewe’l Commission Table of Contents: Page(s) The 1986 Proclamation by our late Mi’kmaq Grand Chief 4 The 1994 Commendation to all A.T.R.A. Netukli’tite’wk (Harvesters) 5 A Message From the N.C.N.S. Netukulimkewe’l Commission 6 Our Collective Rights Proclamation 7 A.T.R.A. Netukli’tite’wk (Harvester) Duties and Responsibilities 8-12 SCHEDULE I Responsible Netukulimkewe’l (Harvesting) Methods and Equipment 16 Dangers of Illegal Harvesting- Enjoy Safe Shellfish 17-19 Anglers Guide to Fishes Of Nova Scotia 20-21 SCHEDULE II Specific Species Exceptions 22 Mntmu’k, Saqskale’s, E’s and Nkata’laq (Oysters, Scallops, Clams and Mussels) 22 Maqtewe’kji’ka’w (Small Mouth Black Bass) 23 Elapaqnte’mat Ji’ka’w (Striped Bass) 24 Atoqwa’su (Trout), all types 25 Landlocked Plamu (Landlocked Salmon) 26 WenjiWape’k Mime’j (Atlantic Whitefish) 26 Lake Whitefish 26 Jakej (Lobster) 27 Other Species 33 Atlantic Plamu (Salmon) 34 Atlantic Plamu (Salmon) Netukulimk (Harvest) Zones, Seasons and Recommended Netukulimk (Harvest) Amounts: 55 SCHEDULE III Winter Lake Netukulimkewe’l (Harvesting) 56-62 Fishing and Water Safety 63 Protecting Our Community’s Aboriginal and Treaty Rights-Community 66-70 Dispositions and Appeals Regional Netukulimkewe’l Advisory Councils (R.N.A.C.’s) 74-75 Description of the 2018 N.C.N.S.
    [Show full text]
  • Atlantic Maritime Ecozone+: Evidence for Key Findings
    Atlantic Maritime Ecozone+ evidence for key findings summary Canadian Biodiversity: Ecosystem Status and Trends 2010 Evidence for Key Findings Summary Report No. 3 Published by the Canadian Councils of Resource Ministers Library and Archives Canada Cataloguing in Publication Atlantic Maritime Ecozone+ evidence for key findings summary. Issued also in French under title: Sommaire des éléments probants relativement aux constatations clés pour l’écozone+ maritime de l’Atlantique. Electronic monograph in PDF format. En14-43/0-3-2015E-PDF 978-1-100-23826-5 Information contained in this publication or product may be reproduced, in part or in whole, and by any means, for personal or public non-commercial purposes, without charge or further permission, unless otherwise specified. You are asked to: Exercise due diligence in ensuring the accuracy of the materials reproduced; Indicate both the complete title of the materials reproduced, as well as the author organization; and Indicate that the reproduction is a copy of an official work that is published by the Government of Canada and that the reproduction has not been produced in affiliation with or with the endorsement of the Government of Canada. Commercial reproduction and distribution is prohibited except with written permission from the author. For more information, please contact Environment Canada’s Inquiry Centre at 1- 800-668-6767 (in Canada only) or 819-997-2800 or email to [email protected]. Cover photos: Margaree Valley, Cape Breton Island, Nova Scotia, © iStock.com / cworthy; Hopewell Rocks, Bay of Fundy, New Brunswick, © iStock.com / MorganLeFaye This report should be cited as: ESTR Secretariat. 2014.
    [Show full text]
  • Geographic Names
    GEOGRAPHIC NAMES CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES ? REVISED TO JANUARY, 1911 WASHINGTON GOVERNMENT PRINTING OFFICE 1911 PREPARED FOR USE IN THE GOVERNMENT PRINTING OFFICE BY THE UNITED STATES GEOGRAPHIC BOARD WASHINGTON, D. C, JANUARY, 1911 ) CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES. The following list of geographic names includes all decisions on spelling rendered by the United States Geographic Board to and including December 7, 1910. Adopted forms are shown by bold-face type, rejected forms by italic, and revisions of previous decisions by an asterisk (*). Aalplaus ; see Alplaus. Acoma; township, McLeod County, Minn. Abagadasset; point, Kennebec River, Saga- (Not Aconia.) dahoc County, Me. (Not Abagadusset. AQores ; see Azores. Abatan; river, southwest part of Bohol, Acquasco; see Aquaseo. discharging into Maribojoc Bay. (Not Acquia; see Aquia. Abalan nor Abalon.) Acworth; railroad station and town, Cobb Aberjona; river, IVIiddlesex County, Mass. County, Ga. (Not Ackworth.) (Not Abbajona.) Adam; island, Chesapeake Bay, Dorchester Abino; point, in Canada, near east end of County, Md. (Not Adam's nor Adams.) Lake Erie. (Not Abineau nor Albino.) Adams; creek, Chatham County, Ga. (Not Aboite; railroad station, Allen County, Adams's.) Ind. (Not Aboit.) Adams; township. Warren County, Ind. AJjoo-shehr ; see Bushire. (Not J. Q. Adams.) Abookeer; AhouJcir; see Abukir. Adam's Creek; see Cunningham. Ahou Hamad; see Abu Hamed. Adams Fall; ledge in New Haven Harbor, Fall.) Abram ; creek in Grant and Mineral Coun- Conn. (Not Adam's ties, W. Va. (Not Abraham.) Adel; see Somali. Abram; see Shimmo. Adelina; town, Calvert County, Md. (Not Abruad ; see Riad. Adalina.) Absaroka; range of mountains in and near Aderhold; ferry over Chattahoochee River, Yellowstone National Park.
    [Show full text]