Niagara Escarpment
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
When the Mountain Became the Escarpment.FH11
Looking back... with Alun Hughes WHEN THE MOUNTAIN BECAME THE ESCARPMENT The Niagara Escarpment hasnt always been But Coronelli was not the first to put Niagara known by that name. Early in the 19th century it on the map. That distinction belongs to Father Louis was often referred to as the Mountain, and of course Hennepin, the Recollect priest who was the first it is still called that in Hamilton and Grimsby today. European to describe Niagara Falls from personal We in eastern Niagara have largely forgotten the observation. In his Description de la Louisiane, name, though it survives in the City of Thorolds published in 1683, five years after his visit, he speaks motto Where the Ships Climb the Mountain. of le grand Sault de Niagara, and labels it thus on the accompanying map. This is the form that So when did the name Niagara Escarpment first prevails thereafter, and it is the spelling used for Fort come into use? And what about the areas other de Niagara, established by the French at the mouth Niagara names, like Niagara Falls, Niagara River of the river in 1726. The English followed suit, and Niagara Peninsula? When did these first appear? though on many early maps (e.g. Moll 1715, I dont pretend to have definitive answers there Mitchell 1782) they use the name Great Fall of are too many sources I have not seen but I can Niagara rather than Niagara Falls. suggest some preliminary conclusions. In his Description Hennepin also refers to la The name Niagara is definitely of native origin, belle Riviere de Niagara, so the name Niagara though there is no agreement about its meaning. -
Rideau Canal National Historic Site of Canada
Rideau Canal national historic site of canada Management Plan Copyright Her Majesty the Queen in Right of Canada, as represented by the Chief Executive Officer of Parks Canada, 2005 Government of Canada Catalogue No. R64-257/2005E ISBN: 0-662-33356-X Aussi disponible en français Rideau Canal national historic site of canada Management Plan May 2005 Lt. Col. John By, Royal Engineers; Royal Engineers Museum of Military Engineering Gillingham, U.K. If ever a man deserved to be immortalized in this utilitarian age, it was Lieutenant Colonel By. In an unexplored part of the country, where the only mode of progress was the frail Indian canoe, with a department to be organized, workmen to be instructed and many difficulties to overcome, he constructed a truly remarkable work. (Captain Richard Bonnycastle of the Royal Engineers, London, 1842) RIDEAU CANAL NATIONAL HISTORIC SITE OF CANADA Management Plan Foreword Canada’s national historic sites, national parks and national marine conservation areas represent the soul of our country. They are a central part of who we are and what we are. They are places of beauty and wonder and heritage. Each tells its own story. Together, they connect Canadians to our roots, to our future and to each other. We see a future in which each of the national historic sites of Canada, whether federally owned or not, enjoys sound commemorative health, and in which our system of sites evolves as our country evolves. Our national historic sites will be places for all Canadians to experience and learn from. They will help our communities to be vibrant and creative, and contribute to our efforts to revitalize Canada’s cities. -
Cambrian Ordovician
Open File Report LXXVI the shale is also variously colored. Glauconite is generally abundant in the formation. The Eau Claire A Summary of the Stratigraphy of the increases in thickness southward in the Southern Peninsula of Michigan where it becomes much more Southern Peninsula of Michigan * dolomitic. by: The Dresbach sandstone is a fine to medium grained E. J. Baltrusaites, C. K. Clark, G. V. Cohee, R. P. Grant sandstone with well rounded and angular quartz grains. W. A. Kelly, K. K. Landes, G. D. Lindberg and R. B. Thin beds of argillaceous dolomite may occur locally in Newcombe of the Michigan Geological Society * the sandstone. It is about 100 feet thick in the Southern Peninsula of Michigan but is absent in Northern Indiana. The Franconia sandstone is a fine to medium grained Cambrian glauconitic and dolomitic sandstone. It is from 10 to 20 Cambrian rocks in the Southern Peninsula of Michigan feet thick where present in the Southern Peninsula. consist of sandstone, dolomite, and some shale. These * See last page rocks, Lake Superior sandstone, which are of Upper Cambrian age overlie pre-Cambrian rocks and are The Trempealeau is predominantly a buff to light brown divided into the Jacobsville sandstone overlain by the dolomite with a minor amount of sandy, glauconitic Munising. The Munising sandstone at the north is dolomite and dolomitic shale in the basal part. Zones of divided southward into the following formations in sandy dolomite are in the Trempealeau in addition to the ascending order: Mount Simon, Eau Claire, Dresbach basal part. A small amount of chert may be found in and Franconia sandstones overlain by the Trampealeau various places in the formation. -
Orchids Orchids Are the Lady’S Slippers, So Named and Lake Huron
By Tom Shields Photos by Kevin Tipson and Henry Glowka unless otherwise indicated jewels of the Biosphere res The Niagara Escarpment is justly famous as a uNESCo World Biosphere Reserve, one of Canada’s first. In Southern ontario, its tower - ing dolostone cliffs, formed in ancient seas more than 420 million years ago, rise dramatically along a jagged line that stretches 725 kilo - metres from the Niagara River to the tip of Tobermory. From these heights the Escarpment tilts down gently to the west. Rainfall and ground water seep gradually through its porous rocks, creating swamps, fens, bogs, marshes, valleys, caves, and microcli - mates across the meandering band that follows its length. 28 BRuCE TRAIL MAGAzINE SPRING 201 4 erve d n a l c A e c n e r u a L : o t o h P WWW.BRuCETRAIL.oRG BRuCE TRAIL MAGAzINE 29 Nowhere are these features more promi - LADY’S SLIPPERS (CYPRIPEDIUM) nent than in the Bruce Peninsula, Easiest to find and most familiar of our enrobed on either side by Georgian Bay distinguishing orchids orchids are the lady’s slippers, so named and Lake Huron. Here, jewel-like mem - All orchids have a highly modified, due to the fancied resemblance of their bers of one of the Escarpment’s other pouched lip to an old-fashioned slipper lavish petal called the lip. usually it claims to fame grow with an abundance or moccasin. The flowers are often large is held at the bottom of the flower, and diversity thought unequalled else - and showy. Four of the nine species but sometimes at the top. -
It's Happeninghere
HAMILTON IT’S HAPPENING HERE Hamilton’s own Arkells perform at the 2014 James Street Supercrawl – photo credit: Colette Schotsman www.tourismhamilton.com HAMILTON: A SNAPSHOT Rich in culture and history and surrounded by spectacular nature, Hamilton is a city like no other. Unique for its ideal blend of urban and natural offerings, this post-industrial, ambitious city is in the midst of a fascinating transformation and brimming with story ideas. Ideally located in the heart of southern Ontario, midway between Toronto and Niagara Falls, Hamilton provides an ideal destination or detour. From its vibrant arts scene, to its rich heritage and history, to its incredible natural beauty, it’s happening here. Where Where Where THE ARTS NATURE HISTORY thrive surrounds is revealed Hamilton continues to make Bounded by the picturesque shores One of the oldest and most headlines for its explosive arts scene of Lake Ontario and the lush historically fascinating cities in the – including a unique grassroots landscape of the Niagara region outside of Toronto, Hamilton movement evolving alongside the Escarpment, Hamilton offers a is home to heritage-rich architecture, city’s long-established arts natural playground for outdoor lovers world-class museums and 15 institutions. Inspiring, fun and – all within minutes of the city’s core. National Historic Sites. accessible, the arts in Hamilton are yours to explore. • More than 100 waterfalls can be • Dundurn Castle brings Hamilton’s found just off the Bruce Trail along Victorian era to life in a beautifully • Monthly James Street North the Niagara Escarpment, a restored property overlooking the Art Crawls and the annual James UNESCO World Biosphere Reserve harbour while Hamilton Museum of Street Supercrawl draw hundreds of that cuts across the city. -
Occasional Papers of the Museum of Zoology
OCCASIONAL PAPERS OF THE MUSEUM OF ZOOLOGY UNIVERSITY OF MICHIGAN I. ON AN INCREASE IN THE NAIAD FAUNA OF SAGINAW BAY, MICHIGAN 11. THE NAIAD SPECIES OF THE GREAT LAI(ES BY CALVINGOODRICH AND HENRYVANDER SCHALIE 1. NINE species of Naiades were found by Dr. H. B. Baker to inhabit Saginaw Bay in the vicinity of Sand Point, Huron County, Michigan, when he made his study of the molluscan fauna of the region in 1908. The survey was a very thorough one and several weelis mere devoted to the work. Twenty-three years later, a much more perfunctory survey was made by the writers of this paper in the same locality, their visits to Sand Point being more in the nature of holidays than for collecting purposes. Yet their findings amounted to thirteen species in contrast to Baker's nine. Moreover, they are enabled to report that five of the nine species of the Baker list proved to be more abundant in 1931 than they were in 1908. Such an increase in ~nollnsca appears to be unusual in American species. The writers are unable to find in the litera- ture of the subject any inention of anything quite like it. In- stances have occurred where an introduced species, Bytlzinia tentaculata (Linnaeus), for example, has developed such a fecundity as to be a pest (F. C. Balier, 1902 ; Sterlqi, 1910). A circnmboreal land snail, Vallonia ~~z~l~lzella(Miiller) , is kno~\~nto have developed exceedingly large colonies that prob- ably were larger than those wliich existed before the trans- plantation of European agriculture on this continent (G. -
(Medina, Clinton, and Lockport Groups) in the Type Area of Western New York
Revised Stratigraphy and Correlations of the Niagaran Provincial Series (Medina, Clinton, and Lockport Groups) in the Type Area of Western New York By Carlton E. Brett, Dorothy H. Tepper, William M. Goodman, Steven T. LoDuca, and Bea-Yeh Eckert U.S. GEOLOGICAL SURVEY BULLETIN 2086 Prepared in cooperation with the U.S. Environmental Protection Agency and the Department of Earth and Environmental Sciences of the University of Rochester UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1995 10 REVISED STRATIGRAPHY AND CORRELATIONS OF THE NIAGARAN PROVINCIAL SERIES been made in accordance with the NASC. Because the The history of nomenclature of what is now termed the NASC does not allow use of the "submember" category, Medina Group, beginning with Conrad ( 1837) and ending units that would be of this rank are treated as informal units with Bolton (1953), is presented in Fisher (1954); Bolton and have been given alphanumeric designations. Informal (1957, table 2) presents a detailed summary of this nomen- units are discussed under the appropriate "member" clature for 1910-53. A historical summary of nomenclature categories. of the Medina Group in the Niagara region is shown in fig- The use of quotes for stratigraphic nomenclature in this ure 7. Early investigators of the Medina include Conrad report is restricted to units that have been misidentified or (1837); Vanuxem (1840, first usage of Medina; 1842); Hall abandoned. If stratigraphic nomenclature for a unit has (1840, 1843); Gilbert (1899); Luther (1899); Fairchild changed over time, the term for the unit is shown, with cap- (1901); Grabau (1901, 1905, 1908, 1909, 1913); Kindle and italization, as given in whatever reference is cited rather Taylor (1913); Kindle (1914); Schuchert (1914); Chadwick than according to the most recent nomenclature. -
Glen Haffy Conservation Area Welcome
www.trca.on.ca Glen Haffy Conservation Area Welcome to Glen Haffy Conservation Area, a beautiful natural area located within the Humber River Watershed, Humber River Watershed Fishing at Glen Haffy at the junction of Ontario’s two most dominant The Humber River watershed covers an area of 903 square Each year, Glen Haffy raises 60,000 rainbow trout at its on-site geological features - The Niagara Escarpment and kilometres, from the headwaters on the Niagara Escarpment fish hatchery, and these fish are released into the fishing the Oak Ridges Moraine. and Oak Ridges Moraine down to Lake Ontario. The watershed ponds at Glen Haffy Conservation Area, the Glen Haffy Fly provides many benefits to the people who live within it including Fishing Club and Heart Lake Conservation Area. The proceeds Glen Haffy Conservation Area is a 189 hectare Toronto drinking water, solace, renewal and contact with nature. generated by angling fees help fund the fish rearing program. and Region Conservation Authority (TRCA) property with great hiking trails you can escape into. Oak Ridges Moraine Glen Haffy Fly Fishing Club The Oak Ridges Moraine stretches as a ridge of hilly terrain for Join the Glen Haffy Fly Fishing Club, escape into 160 kilometres from the Niagara Escarpment in the west to the tranquility and enjoy: headwaters of the Trent River in the east. Rain that is collected and stored in the moraine’s vast underground layers of sand and • Access to private gated Headwaters Ponds located on 600 gravel, which are known as aquifers, eventually resurfaces as acres of prestine conservation lands Become a healthy, clean water that feeds the majority of river systems in • Use of Row Boats, Docks and Log Cabin Conservation the Greater Toronto Area. -
Stratigraphic Succession in Lower Peninsula of Michigan
STRATIGRAPHIC DOMINANT LITHOLOGY ERA PERIOD EPOCHNORTHSTAGES AMERICANBasin Margin Basin Center MEMBER FORMATIONGROUP SUCCESSION IN LOWER Quaternary Pleistocene Glacial Drift PENINSULA Cenozoic Pleistocene OF MICHIGAN Mesozoic Jurassic ?Kimmeridgian? Ionia Sandstone Late Michigan Dept. of Environmental Quality Conemaugh Grand River Formation Geological Survey Division Late Harold Fitch, State Geologist Pennsylvanian and Saginaw Formation ?Pottsville? Michigan Basin Geological Society Early GEOL IN OG S IC A A B L N Parma Sandstone S A O G C I I H E C T I Y Bayport Limestone M Meramecian Grand Rapids Group 1936 Late Michigan Formation Stratigraphic Nomenclature Project Committee: Mississippian Dr. Paul A. Catacosinos, Co-chairman Mark S. Wollensak, Co-chairman Osagian Marshall Sandstone Principal Authors: Dr. Paul A. Catacosinos Early Kinderhookian Coldwater Shale Dr. William Harrison III Robert Reynolds Sunbury Shale Dr. Dave B.Westjohn Mark S. Wollensak Berea Sandstone Chautauquan Bedford Shale 2000 Late Antrim Shale Senecan Traverse Formation Traverse Limestone Traverse Group Erian Devonian Bell Shale Dundee Limestone Middle Lucas Formation Detroit River Group Amherstburg Form. Ulsterian Sylvania Sandstone Bois Blanc Formation Garden Island Formation Early Bass Islands Dolomite Sand Salina G Unit Paleozoic Glacial Clay or Silt Late Cayugan Salina F Unit Till/Gravel Salina E Unit Salina D Unit Limestone Salina C Shale Salina Group Salina B Unit Sandy Limestone Salina A-2 Carbonate Silurian Salina A-2 Evaporite Shaley Limestone Ruff Formation -
Strategic Plan
STRATEGIC PLAN Municipality of Northern Bruce Peninsula June 2008 Revised July 2015 Municipality of Northern Bruce Peninsula Page 1 of 11 Strategic Plan Revised July 2015 MUNICIPALITY OF NORTHERN BRUCE PENINSULA STRATEGIC PLAN Northern Bruce Peninsula is a municipal corporation that commenced operations on January 1, 1999. It encompasses the former Townships of Eastnor, Lindsay and St. Edmunds and the Village of Lion’s Head. Many other hamlets within NBP are Tobermory, Stokes Bay, Pike Bay, Miller Lake, Barrow Bay, Ferndale, Dyers Bay and the Lindsay 20 communities. The Municipality of Northern Bruce Peninsula is the northerly neighbouring community to South Bruce Peninsula, Highway 6 traverses northerly through NBP. The peninsula itself is surrounded on the east by Georgian Bay and on the west by Lake Huron. We are home to Fathom Five National Marine Park, Bruce Peninsula National Park, the Bruce Trail, Niagara Escarpment, UNESCO World Biosphere, Cabot Head and Lion’s Head Nature Reserves, two First Nations Hunting Reserves and a large Bruce County Forest Tract. NBP covers an area of 781.51 square kilometers boasting a permanent population of 3,900 year round residents and just over 5000 households. The Public Works Department maintains 475 kilometres of roads and streets, some of which are paved, some gravelled. Some roads provide year round access while others enjoy only summer accessibility. In 2004, NBP was proclaimed as a “dark sky community” in the hope of preserving and protecting the night time environment and our heritage of dark skies through the use of quality outdoor lighting and goals established which are intended to stop the adverse effects of light pollution. -
Quaternary Geology of the Long Point-Port Burwell Area; Ontario Geological Survey, Open File Report 5873, 212P
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the "Content") is governed by the terms set out on this page ("Terms of Use"). By downloading this Content, you (the "User") have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario's Ministry of Northern Development and Mines (MNDM) as a public service, on an "as-is" basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the "Owner"). -
Effectiveness of COVID-19 Vaccines Against Variants of Concern, Canada
medRxiv preprint doi: https://doi.org/10.1101/2021.06.28.21259420; this version posted July 3, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted medRxiv a license to display the preprint in perpetuity. It is made available under a CC-BY-NC-ND 4.0 International license . Effectiveness of COVID-19 vaccines against variants of concern, Canada Authors: Sharifa Nasreen PhD1, Siyi He MSc1, Hannah Chung MPH1, Kevin A. Brown PhD1,2,3, Jonathan B. Gubbay MD MSc3, Sarah A. Buchan PhD1,2,3,4, Sarah E. Wilson MD MSc1,2,3,4, Maria E. Sundaram PhD1,2, Deshayne B. Fell PhD1,5,6, Branson Chen MSc1, Andrew Calzavara MSc1, Peter C. Austin PhD1,7, Kevin L. Schwartz MD MSc1,2,3, Mina Tadrous PharmD PhD1,8, Kumanan Wilson MD MSc9, and Jeffrey C. Kwong MD MSc1,2,3,4,10,11 on behalf of the Canadian Immunization Research Network (CIRN) Provincial Collaborative Network (PCN) Investigators Affiliations: 1 ICES, Toronto, ON 2 Dalla Lana School of Public Health, University of Toronto, Toronto, ON 3 Public Health Ontario, ON 4 Centre for Vaccine Preventable Diseases, University of Toronto, Toronto, ON 5 School of Epidemiology and Public Health, University of Ottawa, ON 6 Children’s Hospital of Eastern Ontario Research Institute, Ottawa, ON 7 Institute of Health Policy, Management and Evaluation, University of Toronto, Toronto, ON 8 Women’s College Hospital, Toronto, ON 9 Department of Medicine, University of Ottawa, Ottawa and Bruyere Hospital Research Institutes, Ottawa, ON 10 Department of Family and Community Medicine, University of Toronto, Toronto, ON 11 University Health Network, Toronto, ON Corresponding author: 1 NOTE: This preprint reports new research that has not been certified by peer review and should not be used to guide clinical practice.