Achieving Niagara Fa L Ls' Fu T U Re
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4 Removal of Niagara Scenic Parkway
OFFICE OF THE MAYOR Telephone: (716) 286-4310 June 26, 2018 The Niagara Falls City Council Niagara Falls, New York RE: Removal of the Niagara Scenic Parkway —from Main Street to Findlay Drive Council Members: An agreement has been reached between the Power Authority of the State of New York ("NYPA"), the New York State Office of Parks, Recreation & Historic Preservation ("State Parks"), the New York State Department of Transportation ("NYSDOT"), the USA Niagara Development Corporation ("USAN"), and the City of Niagara Falls (the "City"), which is the next step in the ROBERT MOSES PARKWAY NORTH SEGMENT REMOVAL PROJECT (Project). This construction project is estimated to cost $38,500,000. It is largely funded through NYPA ($36,500,000), with the balance being paid for by New York State Office of Parks Recreation and Historic Preservation ($2,000,000). No municipal capital funds are required for this Agreement to take effect. Since constructed in 1962, the former Robert Moses Parkway has not just been the subject of severe criticism but a malignancy that has decimated our community by having cut off both residents and visitors from the Niagara River, Niagara River Gorge, and the public lands connected thereto. The Parkway, rather than being the transportation link in service of economic development and city-building, instead only served to create an effective by-pass around the City and its Main Street, Pine Avenue, and other traditional business corridors. This Project, more than any before marks the largest removal, reconfiguration and regeneration of urban land since a portion of the Parkway passing through Niagara Falls State Park and Prospect Park was removed in the late 1970s. -
The Red Book of Niagara
\V Ki> SpCl 127 N836 p' THE RED BOOK OF NIAGARA A COMPREHENSIVE GUIDE TO THE Scientific, Historical and Scenic Aspects of Niagara FOR THE USE OF TRAVELLERS BY IRVING P. BISHOP, S. M., F, G. S. A, With Many Illustrations, Index and Maps BUFFALO, N. Y. THE WENBORNE-SUMNER CO. I 90 I ^S6696 coptright 1901 bt The Wenborne-Su>iner Co. Press of The Wenborne-Sumner Co. Buffalo, n. Y. Preface. For more than two hundred years the Niagara region has been the most celebrated part of America. In the earlier period of our history it was the doorway to the upper lake region and the Mississippi Valley, for the possession of which French and English and English and Colonists struggled in turn. From a scientific point of view it has presented problems which have interested almost every geol- ogist of distinction, both in America and Europe. As a scenic wonder the Cataract has probably attracted more visitors than any other single natural object in the world. It is the purpose of this handbook to enable the visitor, whether his tastes be for the scenic, the scientific or the historical, to see Niagara from his own point of view, with the minimum outlay of time and money. The book is based upon the author's personal acquaintance with this region, which for thirteen years has been his field for study and recreation. It is issued solely in the interest of travellers whose needs have been, as far as possible, anticipated and provided for. Advertisements of all kind are strictly excluded from its pages. -
Doing Niagara Falls If You're Stuck on the American Side
Meiqianbao/ Shutterstock Doing Niagara Falls If You're Stuck on the American Side By Jason Cochran The legendary Niagara Falls, one of the greatest natural attractions in North America, straddles the border between Ontario, Canada, and New York State. In an ideal tourism situation, you'd be able to drive or stroll across the Rainbow International Bridge to enjoy the view from both banks of the Niagara River. But sometimes you just can't get over the border. Maybe you don't have enough time. Maybe your legal status won't allow it. Or maybe you happen to be living through a once-in-a-lifetime global pandemic that has sealed national borders. It's all good! If you're restricted to the U.S. side, you won't find yourself over a barrel. There's plenty to do. In fact, some of the best activities in the Niagara Falls area are on the American side. Pictured above: Terrapin Point, at right, juts into the eastern side of the Falls from Niagara Falls State Park in New York State. Niagara Falls State Park Niagara Falls State Park If we're being honest, the Canadian side has richer options for quality lodging and tourist amenities, although the stuff on that riverbank tends toward cheesy honky-tonk. New York's territory beside the Falls, on the other hand, has been preserved from development since the 1880s. In fact, the area is now the oldest state park in the United States. The more-than-400-acre Niagara Falls State Park, which is separated from the core of town by a breakaway river, is speckled with whitewater-spanning bridges, river islands, curving walkways, and native animals. -
Imagine Niagara
This page has been intentionally left blank. Chapter 1 1 - 2 1. Imagine Niagara Physical and Economic Background The Regional Municipality of Niagara is located in Southern Ontario between Lake Erie and Lake Ontario. It corresponds approximately to the area commonly referred to as the "Niagara Peninsula" and will be referred to here as simply "the Region". It is bounded on the east by the Niagara River and the State of New York, and on the west by the City of Hamilton and Haldimand County. The Region is at one end of the band of urban development around the western end of Lake Ontario. Chapter 1 1 - 3 The Region was formed in 1970 and includes all of the areas within the boundaries of the former Counties of Lincoln and Welland. There are twelve local municipalities within the Region; these were formed by the rearrangement and amalgamation of the twenty-six municipalities which existed before 1970. The Queen Elizabeth Way and other provincial highways place most of the Region within ninety minutes' travel time of Toronto. Hamilton-Wentworth, with a population of over 400,000, is about thirty minutes away from the centre of the Region. Four road and two rail bridges connect the Region to the western part of New York State. About 2,500,000 people live along the United States' side of the Niagara River. The developing industrial complex at Nanticoke, on the shore of Lake Erie to the southwest, is about an hour's travel time from the centre of the Region. Physical Characteristics The "Niagara Peninsula" area is not a true peninsula but is a narrow neck of land stretching between Lakes Erie and Ontario. -
Downtown Neighborhood City of Niagara Falls: Phase I
Intensive Level Survey Historic Resources – Downtown Neighborhood City of Niagara Falls: Phase I 3.0 Historical Overview This section provides a narrative history of the City of Niagara Falls with specific emphasis on the Downtown neighborhood. The overview addresses significant trends and themes associated with the city’s historic context. The Downtown neighborhood’s period of significance is identified and examined in this chapter. Martin Wachadlo, architectural historian, conducted the background historic research. 3.1 Niagara County: Physiology and Geology Figure 3-1. Niagara Falls, Niagara Falls, New York Niagara County borders the southern shore of Lake Ontario in the extreme northwestern corner of New York State, and occupies part of the Huron and Ontario Plains. The Ontario Plain comprises part of Lake Ontario to the foot of the Niagara Escarpment1, and the Huron plain extends from the crest of the escarpment southward beyond the county line. The Niagara Escarpment begins in Watertown, New York, USA and extends westerly along the Manitoulin Island in the Province of Ontario, Canada. The escarpment continues through Wisconsin and Illinois. With geological material measuring 64-ft thick, the stratigraphy at Niagara Falls provides a glimpse into the overall rock types comprising the Niagara Escarpment (Figure 3-1). The top layer is Lockport Dolomite, a hard rock referred to as the "Lower Silurian Group." Below the top layer is Rochester Shale, which is much softer and wears away easily with the effects of erosion. Under the shale are harder strata of limestone and dolostone known as the "Clinton Group." Below the harder strata is Grimsby sandstone. -
Niagara National Heritage Area Study
National Park Service U.S. Department of the Interior Niagara National Heritage Area Study Study Report 2005 Contents Executive Summaryr .................................................................................................. Introduction ..........................................................................................................................5 Part 1: Study Purpose and Backgroundr Project History ....................................................................................................................11 Legislation ..........................................................................................................................11 Study Process ......................................................................................................................12 Planning Context ................................................................................................................15 The Potential for Heritage Tourism ..................................................................................20 Part 2: Affected Environmentr .............................................................................. Description of the Study Area ..........................................................................................23 Natural Resources ..............................................................................................................24 Cultural Resources ..............................................................................................................26 -
NIAGARA ROCKS, BUILDING STONE, HISTORY and WINE
NIAGARA ROCKS, BUILDING STONE, HISTORY and WINE Gerard V. Middleton, Nick Eyles, Nina Chapple, and Robert Watson American Geophysical Union and Geological Association of Canada Field Trip A3: Guidebook May 23, 2009 Cover: The Battle of Queenston Heights, 13 October, 1812 (Library and Archives Canada, C-000276). The cover engraving made in 1836, is based on a sketch by James Dennis (1796-1855) who was the senior British officer of the small force at Queenston when the Americans first landed. The war of 1812 between Great Britain and the United States offers several examples of the effects of geology and landscape on military strategy in Southern Ontario. In short, Canada’s survival hinged on keeping high ground in the face of invading American forces. The mouth of the Niagara Gorge was of strategic value during the war to both the British and Americans as it was the start of overland portages from the Niagara River southwards around Niagara Falls to Lake Erie. Whoever controlled this part of the Niagara River could dictate events along the entire Niagara Peninsula. With Britain distracted by the war against Napoleon in Europe, the Americans thought they could take Canada by a series of cross-border strikes aimed at Montreal, Kingston and the Niagara River. At Queenston Heights, the Niagara Escarpment is about 100 m high and looks north over the flat floor of glacial Lake Iroquois. To the east it commands a fine view over the Niagara Gorge and river. Queenston is a small community perched just below the crest of the escarpment on a small bench created by the outcrop of the Whirlpool Sandstone. -
Niagara Gorge – Whirlpool, Smeaton, Queenston Sites - Lower Niagara River, Ontario
1.1.1 Important Amphibian and Reptile Areas Nomination Form NIAGARA GORGE – WHIRLPOOL, SMEATON, QUEENSTON SITES - LOWER NIAGARA RIVER, ONTARIO PART 1: Nomination Eligibility Criteria Nominations for an Important Amphibian and Reptile Areas Program (IMPARA) site must be made on this Nomination Form. Please read through the IMPARA site eligibility criteria below to ensure that your nomination complies. These criteria are intended to be the first step in a dialogue between the nominator and Canadian Herpetological Society (CHS). Your nomination may not be considered if you fail to comply with this checklist. IMPARA eligibility criteria: a. Site has species of conservation concern. b. Site has a high diversity of species. c. Site fulfills important life history function for gatherings of individuals or aggregations of species. 1.1 Species of Conservation Concern A site that that is nominated under this criterion must contain a significant number of individuals of a species that is of conservation concern. CHS uses the broad definition of a species used by COSEWIC, which defines species as, "Any indigenous species, subspecies, variety or geographically defined population of wild fauna and flora." Species of conservation concern are any species with the following designations: Globally designated as Critically Endangered, Endangered or Vulnerable by the International Union for the Conservation of Nature (IUCN). See (http://www.iucnredlist.org/search) and enter species name. 1 Nationally designated as at-risk (Endangered, Threatened, and Species of Special Concern) by the Committee on the Status of Endangered Wildlife in Canada (COSEWIC) or the federal Species at Risk Public Registry (SARA). Provincially/territorially designated as at-risk by the provincial or territorial government or other designated group that assesses the status of species within a province, or a provincial/regional Conservation Data Centre. -
Niagara-On-The-Lake Wine Routes
NIAGARA-ON-THE-LAKE Niagara-on-the-Lake HORE R LAKES D 32 33 34 MARY STKING ST JOHN ST 35 38 EAST & WEST LINE 36 PENNER ST 37 39 31 R RD LINE 1 LINE 1 E IRVINE V I LINE 2 40 LINE 2 R 30 A 41 R A LINE 3 LINE 3 G AKESHORE RD CHURCH RD A CON. 3 RD I L CON. 4 RD 42 N WN LINE RD 43 TO 44 Y STEWART RD STEWART W ARA STONE RD K (HWY 55) P A NIAG R A NIAGARA ST G A I CONCESSION 1 RD CONCESSION N CONCESSION 2 RD CONCESSION GRANTHAM AVE GRANTHAM OUR MILE CREEK rd CREEK MILE OUR BUNTING RD F Lewiston AIRPORT RD AIRPORT 28 CONCESSION 6 RD CONCESSION VE QUEENSTON RD RD LINE N D A LAN WEL TOW YORK RD YORK RD QUEENSTON RD 29 LEWISTON RD BRIDGE St. Catharines GE TA 27 OR P Queenston Y W GLENDALE AVE INRD K OR RD TA P TAIN RD OUN A UN M R MO A TAYL NIAG WELLAND CANAL ST PAUL AVE ST PAUL THOROLD STONE RD AVE STANLEY WHIRLPOOL Niagara BRIDGE Falls United DORCHESTER RD RAINBOW States BRIDGE 27. NIAGARA COLLEGE TEACHING WINERY Hours: May-Oct., Mon.-Sat. winning VQA wines, featuring great 10 a.m-5 p.m. Welcome to Canada's only teaching Sundays 11 a.m.-5 p.m. Bordeaux reds and luscious Rieslings. winery, located on the Glendale cam- Nov.-April, Mon.-Fri. 12 a.m.-5 p.m. pus at the base of the Niagara Location: 450 Queenston Road, Tour Hours: Year round, on request Niagara-on-the-Lake Escarpment. -
Physical Geology Laboratory Streams, Water, and Surfaces
StreaiTI Processes, Landscapes, Mass Wastage, and Flood Hazards CONTRIBUTING AUTHORS Pamela] .W Gore • Georgia Perimeter College Richard W Macomber • Long Island University-Brooklyn Cherukupalli E. Nehru • Brooklyn College (CUNY) OBJECTIVES AND ACTIVITIES INTRODUCTION A. Be able to use topographic maps and stereo It all starts with a single raindrop, then another and an grams to describe and interpret stream valley other. As water drenches the landscape, some soaks into shapes, channel configurations, drainage the ground and becomes groundwater. Some flows patterns, depositional features, and the evolu over the ground and into streams and ponds of swface tion of meanders. water. The streams will continue to flow for as long as ACTIVITY 1: Introduction to Stream they receive a water supply from additional rain, Processes and Landscapes melting snow, or base flow (groundwater that seeps ACTIVITY 2: Meander Evolution on the into a stream via porous rocks, fractures, and springs). Rio Grande Perennial streams flow continuously throughout the year and are represented on topographic maps as blue B. Understand erosional and mass wastage lines. Intermittent streams flow only at certain times of processes that occur at Niagara Falls, and be the year, such as rainy seasons or when snow melts in able to evaluate rates at which the falls is retreat the spring. They are represented on topographic maps ing upstream. as blue line segments separated by blue dots (three blue ACTIVITY 3: Mass Wastage at Niagara Falls dots between each line segment). All streams, perennial C. Be able to construct a flood magnitude/frequency and intermittent, have the potential to flood (overflow graph, map floods and flood hazard zones, and their banks). -
Description of the Niagara Quadrangle
DESCRIPTION OF THE NIAGARA QUADRANGLE. By E. M. Kindle and F. B. Taylor.a INTRODUCTION. different altitudes, but as a whole it is distinctly higher than by broad valleys opening northwestward. Across northwestern GENERAL RELATIONS. the surrounding areas and is in general bounded by well-marked Pennsylvania and southwestern New York it is abrupt and escarpments. i nearly straight and its crest is about 1000 feet higher than, and The Niagara quadrangle lies between parallels 43° and 43° In the region of the lower Great Lakes the Glaciated Plains 4 or 5 miles back from the narrow plain bordering Lake Erie. 30' and meridians 78° 30' and 79° and includes the Wilson, province is divided into the Erie, Huron, and Ontario plains From Cattaraugus Creek eastward the scarp is rather less Olcott, Tonawanda, and Lockport 15-minute quadrangles. It and the Laurentian Plateau. (See fig. 2.) The Erie plain abrupt, though higher, and is broken by deep, narrow valleys thus covers one-fourth of a square degree of the earth's sur extending well back into the plateau, so that it appears as a line face, an area, in that latitude, of 870.9 square miles, of which of northward-facing steep-sided promontories jutting out into approximately the northern third, or about 293 square miles, the Erie plain. East of Auburn it merges into the Onondaga lies in Lake Ontario. The map of the Niagara quadrangle shows escarpment. also along its west side a strip from 3 to 6 miles wide comprising The Erie plain extends along the base of the Portage escarp Niagara River and a small area in Canada. -
National Register of Historic Places Received Inventory—Nomination
NPS Form 10-900 OMB No. 1024-0018 (3-82) Exp. 10-31-84 United States Department of the Interior National Park Service For NPS use only National Register of Historic Places received Inventory—Nomination Form date entered See instructions in How to Complete National Register Forms Type all entries—complete applicable sections________________ ________ 1. Name historic FORT NIAGARA and or common OLD FORT NIAGARA 2. Location street & number N.Y.S. Route 18F not for publication Youngstoiun city, town v,cin,tyof New York 36 Niagara 63 state code county code 3. Classification Category Ownership Status Present Use district x public x occupied agriculture X museum x building(s) private unoccupied commercial X park structure both work in progress educational private residence X site Public Acquisition Accessible entertainment religious object in process X yes: restricted government scientific being considered Jt yes: unrestricted industrial transportation no _X_ military other: 4. Owner of Property name (See continuation sheet 4-1) street & number city, town vicinity of state 5. Location of Legal Description courthouse, registry of deeds, etc. Niagara County Courthouse street & number city, town Lockport state York 6. Representation in Existing Surveys 'yes* L tltle N.Y.S. Historic Resource Sur Wthjs property been determined eligjble? no date December 1982 federal state county local New York State Historic Preservation Office depository for survey records Albany New York city, town state 7. Description Condition Check one Check one _X_ excellent _ _ deteriorated unaltered X original site __ good __ ruins X altered moved date _____._... , fair unexposed Describe the present and original (if known) physical appearance Old Fort Niagara National Historic Landmark is located at the northwest corner of the Town of Porter in Niagara County, New York.