Niagara Power Project FERC No. 2216

 

DESCRIBE THE EFFECTS OF PROJECT CONSTRUCTION ON THE SURROUNDING ENVIRONMENT

 

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Prepared for: New York Power Authority 

Prepared by: URS Corporation; Gomez and Sullivan Engineers, P.C.; and E/PRO Engineering & Environmental Consulting, LLC

 

August 2005

 

___________________________________________________

 

Copyright © 2005 New York Power Authority

 

 

EXECUTIVE SUMMARY

This report identifies and summarizes the social, regional and ecological pre-construction conditions in the Niagara region prior to construction of the Niagara Power Project (NPP).  The information regarding pre-construction conditions may be used in the cumulative effects analysis section of the Applicant Prepared Environmental Assessment.  The objectives of this report were to:

1.       describe the construction of the NPP structures and related facilities, including any relocations,

2.       describe pre-construction terrestrial and aquatic habitats in the area presently occupied by the NPP,

3.       qualitatively describe the excavation, dredging, and spoil placement or filling activities associated with the construction of the Project,

1.       describe the pre-construction cultural and social setting, and

2.       identify the source of the spoil or fill materials generated during construction of the Project.

Major components of the NPP development involved the construction of two below grade water conduits from the upper Niagara River to the forebay, construction of the forebay and Lewiston Reservoir, construction of the Lewiston Pump Generating Plant (LPGP) between the forebay and Lewiston Reservoir, and the construction of the Robert Moses Niagara Power Plant (RMNPPP).  Major construction milestones were as follows:

March 18, 1958          First  rock excavation

January 25, 1960        First scroll case completed and tested at the Robert Moses Niagara Power Plant

June 25, 1960             Conduit excavation completed

August 19, 1960         First turbine runner installed at the Robert Moses Niagara Power Plant

December 31, 1960    Conduits and canal watered

January 28, 1961        Unit 1 at the Robert Moses Niagara Power Plant put into regular commercial operation

February 10, 1961      First Power ceremonies

September 30, 1961    Adams and Schoellkopf plants cease operation

December 1, 1961      Unit 1 at LPGP put into regular commercial operation

October 11, 1962       Twelfth and final unit at LPGP put into regular commercial operation

PROJECT CONSTRUCTION ACTIVITIES

Construction activities occurred from the upper Niagara River near the southern boundary of the City of Niagara Falls along a 500-foot wide conduit right-of-way to the main Project area in Lewiston.  Construction of the Project also involved the use of spoil storage and placement areas, temporary and permanent relocation of roads, and the placement of fill along sections of the upper Niagara River shoreline (Robert Moses Parkway route).  In general, permanent fill placement occurred along the upper Niagara River shoreline (near the intake structures), conduit routes, and in Artpark.  Temporary spoil stockpiles were placed along Buffalo Avenue, adjacent to the intake construction, within the Reservoir footprint, and on property located on Porter Road in the City of Niagara Falls.  The rock material stockpiled within the reservoir footprint was used for concrete, aggregate, or as construction material for the reservoir dikes and backfill of the conduit routes.  Both topsoil and overburden were used throughout the project for finish-grade landscaping.  Clay overburden was also used to construct the reservoir dikes.  Additionally, concrete batch plants were set up near major construction areas (intakes, conduits, Robert Moses Niagara Power Plant, and Lewiston Pump Generating Plant).

 

 

Conduits

The route of the two parallel water conduits extends from the intake structures on the upper Niagara River to the Forebay.  Topsoil and overburden was stripped off and stockpiled within the future reservoir area.   Bedrock was removed from the conduit areas and placed along the upper Niagara River shoreline to develop the Robert Moses Parkway. 

In constructing the two intakes, a cofferdam was installed to create a dry work area.  Excavated material from the intake structure locations was placed in the Robert Moses Parkway right-of-way.  Additionally, an ice escape channel was blasted into the rock downstream of the intakes.  Rock removed for this channel was used in the construction of the Buckhorn Island diversion dikes, which was proceeding at approximately the same time as intake construction.

Forebay

The 71-acre Forebay, which receives the water from the conduits, serves as headwater for the Robert Moses Niagara Power Plant and tailwater from the Lewiston Pump Generating Plant.  Material removed from the Forebay excavation was stored within the reservoir boundaries for use during construction of the reservoir dike.

Robert Moses Niagara Power Plant

The Robert Moses Niagara Power Plant (RMNPP) is located at the western end of the forebay on the face of the Niagara River gorge.  To construct the RMNPP, topsoil and overburden was stripped and stored within the reservoir footprint.  The rock was removed from the gorge wall and permanently placed in the Lewiston Spoil Area, which is part of the Earl W. Brydges Artpark State Park.

 

Lewiston Pump Generating Plant

The Lewiston Pump Generating Plan (LPGP), situated between the forebay and the Lewiston Reservoir, is built on bedrock.  One end of the reservoir dike is anchored to the plant’s north end and the other to its south end.  The dike is a rockfill structure with an impervious clay core.  To reduce the permeability of the foundation, the bedrock under the central core was extensively grouted. 

NYPA-Funded Non-Project Related Construction

As part of the development of the NPP, numerous public benefit projects were undertaken.  Original efforts related to the Project included construction of an 8.5-mile section of the Robert Moses Parkway from the North Grand Island Bridges to the Upper Mountain Road interchange, enlargement of and construction of a new parking lot on Goat Island, enhancements to the Niagara Reservation State Park, including a contribution of parcels of land toward creation of a new parking lot, construction of a new American Rapids bridge connecting the mainland to Goat Island, construction of a maintenance garage at Whirlpool State Park for the Office of State Parks and Recreation, and enlargement of Hyde Park in the City of Niagara Falls.

Additionally, land was either donated by NYPA or provided as a site by NYPA to local and state agencies.  This included provision of land and the development of Reservoir State Park, provision of land for the Schoellkopf Geological Museum, provision of land for the development of Artpark, donation of land and development of DeFranco Park in the City of Niagara Falls, and donation of land and development of Veterans Park in the Town of Niagara.

Project Construction Relocations

Seven permanent relocations were required to complete the project.  Four relocations were required for construction of the Reservoir: Two relocations involved Fish and Gill creeks, respectively, which were rerouted around the Reservoir, The third relocation  involved moving a portion of Garlow Road  east  of the Reservoir.  The fourth relocation involved the existing transmission lines that crossed through the reservoir footprint, which were relocated north (just north of the reservoir) and east (approximately two miles east of the reservoir), through the Tuscarora Nation. 

The fifth relocation was the moving of 76 homes for the construction of the conduits.  The sixth relocation was the power lines crossing the Niagara River from the Sir Adam Beck Generating Station in Ontario.  These lines originally crossed in the future location of the RMNPP and forebay.  The lines were moved approximately one half mile to the south. 

The seventh relocation involved either moving homes or building new homes for Tuscarora that were impacted by construction of the Lewiston Reservoir.  Twenty-nine households were affected and eventually relocated onto other lands owned by the Tuscarora Nation.

Although not a relocation, a 630-foot section of the Gill Creek streambed was reinforced with a concrete bottom within the section that crosses over the conduits.

NYPA-Funded Non-Project Construction Relocations

To construct the Robert Moses Parkway, the section north of the Rainbow Bridge and south of Ontario Avenue required the relocation of 14 houses from Rapids Boulevard, and the relocation of Whirlpool Street.  The houses were moved to a newly constructed subdivision called College Terrace, while Whirlpool Street was moved slightly to the east of its former location.

PRE-RMNPP CONSTRUCTION AQUATIC ENVIRONMENT

Project construction took place in the following areas of the Niagara River: (1) the area around the present-day Buckhorn Marsh weirs and Buckhorn Island Diversion Dikes on the north end of Grand Island; (2) the shoreline of the upper Niagara River near the location of the present-day intakes and along the eastern end of Goat Island (Niagara Reservation State Park); (3) the area around the present-day Robert Moses Power Plant in the lower Niagara River, and (4) specific areas of Gill and Fish Creeks where the Lewiston Reservoir was created and where the conduits were placed under a section of Gill Creek. 

The area in the vicinity of the Buckhorn Island Diversion Dikes and the north end of the Buckhorn Island Dikes on the north end of Buckhorn Island likely consisted of moderately deep (approximately 10 feet.) water. Submerged aquatic vegetation (SAV) was located in water from three to five feet deep, and out to a narrow point about 1,000 feet from shore.  

Prior to the construction of the Robert Moses Parkway, as discussed above, much of the shoreline had been altered and numerous industries existed here.  Just west of the present-day intakes there were several small areas of SAV and three small islands (Conners Island and two unnamed islands).  This area was just to the south of the area where fill was placed to create the present-day shoreline.  SAV also existed in the upper Niagara River at depths of 1.5 to 5.5 feet in the mainstem, and at depths of less than 1.5 feet in sheltered bays.  Substrates in the area included soft (“mud”), sand and stony areas.  For approximately 2,000 feet to the west of Conners Island, no SAV is indicated as existing in this area. 

Along the eastern end of Goat Island (i.e., Niagara Reservation State Park) where fill was placed, the upper Niagara River has high water velocities and standing waves and unlikely to contain SAV. 

The shallow, near-shore zone in the area of the present-day RMNPP likely existed as a narrow strip and contained large-grained substrate (e.g., large cobble, boulder, and bedrock).  A 1928 survey of SAV in the lower Niagara River indicated that SAV was found downstream of Lewiston extending 10-30 feet from the shore over an area 30-60 feet wide in water 3-12 feet deep.  The survey did not indicate whether SAV was found upstream of Lewiston in the area now occupied by the RMNPP.

Portions of Gill and Fish Creeks were relocated for the construction of the Lewiston Reservoir.  In the area where the reservoir was constructed, both creeks appear to have been meandering channels, bordered largely by a thin strip of riparian vegetation, and surrounded by agricultural lands.  The creeks in this area were likely slow-moving, with little gradient.  From the existing information, it is not possible to determine the species of aquatic plants that grew in these areas.

PRE-RMNPP CONSTRUCTION TERRESTRIAL ENVIRONMENT

Construction activities took place in the following land areas:  (1) the shoreline of the upper Niagara River near the present-day location of the intakes, (2) the area around the present-day RMNPP on the lower Niagara River, (3) those locations where the forebay, Lewiston Reservoir, maintenance/equipment warehouse, switchyard, and conduits are found today, (4) along the present-day route of the Robert Moses Parkway, on the Niagara River, (5) parkland in the City of Niagara Falls, (6) present-day Earl W. Brydges Artpark, (7) Niagara Reservation State Park, (8) Whirlpool/Devil’s Hole State Parks, (9) and those areas where fill or excavated material was temporarily placed or stored.

Prior to construction, the terrestrial habitat on Buckhorn Island in the area where the Buckhorn Island Diversion Dikes are located consisted of a mixed growth of herbaceous, shrub, and tree species.  There appears to have been a mix of upland and wetland habitats.  The areas along the shoreline, especially on the northwest and north end (near the present-day site of the dikes) were herbaceous and shrub wetland.  It is likely that some coastal wetlands existed in the area where the dikes were constructed.

Before Project construction, the area adjacent to Robert Moses Parkway of the upper Niagara River was a heavily developed industrial area.  This development encompassed the entire shoreline and adjacent lands.  Because of these conditions, the shoreline had little if any riparian vegetation and lacked significant growth of emergent aquatic vegetation (EAV).

On the 1953 USACE navigation chart, Conners Island and the two unnamed islands appear to be submerged.  It is therefore likely they were not true islands, but shallow areas with EAV.  For approximately 2,000 feet to the west of Conners Island, there is no indication from existing information that EAV existed in this area.  Further west, there existed a small bay near the Niagara Falls Power Company.  This bay appears to have been shallow and contained at least some EAV. 

The conduits, from the intakes to the forebay, traverse land that was heavily developed prior to Project construction.  The forebay area, which includes a switchyard and maintenance/equipment warehouse, was a golf course and agricultural land prior to project construction.  The Lewiston Reservoir area was primarily agricultural fields with a few patches of undeveloped woodlands.  Also within the reservoir construction area were several roads, residential properties, and Gill and Fish Creeks.  The streams, from Garlow Road west, meandered through active agricultural land.  There was vegetated riparian zone along both streams that ranged from zero to several hundred feet in width.  Most of the land adjacent to the streams was actively farmed close to the stream banks.  Gill Creek passed through a golf course.  Except for one section, it was bordered by an approximately 25-foot-wide band of riparian vegetation on each side. 

Three railroads or railroad rights-of-way crossed the Project area.  These included (1) the former Great Gorge Railroad right-of-way, (2) an inoperative track owned by the New York Central Railroad that descended into the gorge and that was used as a haul road during construction, and (3) the operational New York Central Railroad on the rim of the gorge.  The portion of the RMNPP site that is upslope of the gorge had once been the location of a railroad line and a quarry.  The areas along the shoreline of the lower Niagara River that were affected by Project construction consisted of the site of the RMNPP and an associated access road, and additional shore access created for Whirlpool/Devils Hole State Park and Artpark.  There were the remains of a railroad bed (former Great Gorge Railroad) and several footpaths in the gorge prior to Project construction.  The immediate shoreline along the lower Niagara River in the Project area was primarily an undeveloped, wooded riparian zone.  Because of the steep topography, no large areas of wetland existed in this area.  Prior to Project construction, the Artpark area was utilized for commercial/industrial activities.  Just prior to Project construction, the area had several roads meandering through it and there were several areas of disturbed, bare soils and sparse vegetation.

Surface Water and Groundwater Hydraulics

As part of this study an evaluation of river and groundwater hydraulics was conducted to determine what effect the operation of the NPP has on both water regimes.  To evaluate the surface water hydraulics, data were used from a 1953 study conducted by the International Joint Commission, and 1991 to 2002 river hydraulic data collected by NYPA.  The groundwater evaluation used data from the 1964 United States Geological Survey study and an ongoing NYPA groundwater study begun in 2003.

Based on available data, current river water levels for a diversion flow of approximately 100,000 cfs are higher than pre-1950 water levels.  The magnitude of this difference is greatest in the Chippawa-Grass Island Pool and diminishes with distance upstream.  For a flow diversion of 100,000 cfs, current water levels at Material Dock are 0.85 feet higher than pre-1950 conditions. 

The primary groundwater aquifer in this region exists within layers of bedrock.  Several unique water-bearing zones are found in the bedrock, which together comprise a relatively complex groundwater flow regime.  Groundwater flow patterns and levels have changed since the construction of the Project.  This effect is most pronounced in the area of the conduits and is the result of groundwater being redirected through external drains designed to reduce hydrostatic pressure on the walls of the conduits.  In general, groundwater levels very near the conduits have been lowered by tens of feet (dewatering effects farther away from the conduits are much less), and groundwater in the vicinity of the conduits now flows towards the conduits rather than towards the south or west (ultimately heading toward a large diameter sewer tunnel or the Niagara River gorge).

As a result of filling the Lewiston Reservoir, groundwater levels near the reservoir dike generally increased.  The increased groundwater levels near the dike were generally less than ten feet.  The effect of increased water levels diminished farther away from the reservoir.

 

1.0     INTRODUCTION

This report identifies and summarizes the social, regional and ecological pre-construction conditions in the Niagara region prior to construction of the Niagara Power Project (NPP).  The information regarding pre-construction conditions may be used in the cumulative effects analysis section of the Applicant Prepared Environmental Assessment.

1.1         Objectives

The objectives of this report are as follows:

·         Describe the construction of the NPP structures and related facilities, including any relocations,

·         Describe pre-construction terrestrial and aquatic habitats in the area presently occupied by the NPP,

·         Qualitatively describe the excavation, dredging, and spoil placement or filling activities associated with the construction of the Project,

·         Describe the pre-construction cultural and social setting, and

·         Identify the source of the spoil or fill materials generated during construction of the Project.

1.2         Investigation Area

The investigation area includes areas affected by both Project-related and NYPA-funded non-Project-related construction.  These areas are described below and depicted in Figure 1.1-1.

Areas within the FERC project boundary:  These areas include the locations of Project-specific structures, namely, the water intakes, water conduits, forebay, Lewiston Reservoir, Lewiston Pump Generating Plant, Robert Moses Niagara Power Plant, the tailrace tunnels, and portions of the Robert Moses Parkway.

Lands used to store spoil and stockpile material:  These are generally adjacent or near the major construction areas and include Artpark, the reservoir basin, and several locations adjacent to the conduits.

Non-Project-related construction:  These are areas that were created or constructed with the Project- funding but are not part of the NPP.  These areas include the extension of Goat Island, portions of the Robert Moses Parkway, expansion of Hyde Park, and allocation of land for several city and the present-day state parks.

1.3         Methods

This investigation involved compiling and reviewing existing information regarding the physical condition of the investigation area before the Project was built and during its construction.  Information for the time period of interest (1951 to 1962) was reviewed.  Information from before this time period was also reviewed.  Information was found in the form of books, newspaper articles, government reports, and NYPA records, historical and current topographic and navigation maps, historical aerial and ground level photographs, and construction drawings and documentation.  In addition, NYPA staff and local historians were interviewed regarding their knowledge of the investigation area’s pre-construction conditions.

 

Figure 1.1-1

Project Location

[NIP – General Location Maps]

 

2.0     BACKGROUND AND PRE-CONSTRUCTION SETTING

The 1,880-MW (firm capacity) Niagara Power Project (NPP) is one the largest non-federal hydroelectric facilities in North America.  The Project was licensed to the Power Authority of the State of New York (now the New York Power Authority) in 1957.  Construction of the Project began in 1958, and electricity was first produced in 1961.  The Project occupies land within the following jurisdictions: City of Niagara Falls, Town of Niagara, the Village of Lewiston, and the Town of Lewiston.  This section provides a review of the Project’s regional setting, an overview of the international treaty on water use for the Niagara River, and the pre-construction cultural and social setting.

2.1         Regional Setting

The NPP is located in Niagara County adjacent to the international border with Canada.  Niagara County is divided topographically into two regions, one above the escarpment and one below the escarpment.  The region above the escarpment comprises the southern half of the county.  The NPP is located within this upper region.   Streams above the escarpment eventually flow, either directly or through larger streams, into the Niagara River.  Streams below the escarpment flow either into the Niagara River or Lake Ontario.

The Niagara River, which bounds the county to the south and west, consists of two major reaches: the upper Niagara River and the lower Niagara River.  The two reaches are separated by Niagara Falls.  The upper Niagara River extends about 22 miles from Lake Erie to the Falls, and the lower Niagara River about 15 miles from the Falls to Lake Ontario.  NPP structures are found along the shorelines of both river sections. 

At Grand Island (upper Niagara River), the river divides into the west channel, known as the Canadian or Chippawa Channel, and the east channel, known as the American or Tonawanda Channel.  At the north end of Grand Island, the channels unite to form the 3-mile-long Chippawa-Grass Island Pool (approximately 9 feet below the level of Lake Erie), at the downstream end of which is the International Niagara Control Structure.  This gated flow-control structure extends from the Canadian shoreline to the approximate midpoint of the river.  The Falls are located about 4,500 feet downstream of the control structure.  Below the International Niagara Control Structure, the river surface elevation falls 50 feet through the Cascade Rapids before being divided into two channels by Goat Island.  These channels convey the flow to the brink of Niagara Falls: the Horseshoe Falls (Canadian Falls) on the west side and the American Falls on the east.  At the Falls, the river surface drops approximately 167 feet.

Below the Falls, the river flows through the 7-mile-long Niagara gorge, which extends from the Falls to the foot of the escarpment at Lewiston.  The river emerges from the gorge at Lewiston, subsequently dropping another 5 feet to Lake Ontario.

2.2         International Treaties on Water Use

In 1909, the United States and Canada signed the Treaty Between the United States and Great Britain Relating to Boundary Waters and Questions Arising Between the United States and Canada (1909 Treaty), establishing a framework for the allocation of boundary waters between the two countries.  Among other provisions, the 1909 Treaty created the International Joint Commission (IJC), and granted it broad authority over “uses or obstructions or diversions, whether temporary or permanent, of boundary waters on either side of the line, affecting natural level or flow of boundary waters on the other side of the line.”  The 1909 Treaty provided further that “except in cases provided for by special agreement between them, [the U.S. and Canada] will not permit the construction or maintenance on the respective sides of the boundary of any remedial or protective works or any dams or other obstructions…, the effect of which is to raise the natural level of waters on the other side of the boundary unless the construction or maintenance thereof is approved by [the IJC].”  IJC authority extends to all United States-Canada boundary waters, including the Niagara River.

In addition to creating the IJC, the 1909 Treaty set diversion limits on the Niagara River, limiting the amount of water that the United States could take from above Niagara Falls for power purposes to 20,000 cfs.  In 1950, the United States and Canada renegotiated diversion limits on the Niagara River and signed the Treaty Between Canada and the United States of America Concerning the Diversion of the Niagara River (1950 Treaty).  The 1950 treaty required that a minimum of 100,000 cfs flow over the Falls during the daytime during the tourist season, and that a minimum of 50,000 cfs flow over the Falls at all other times.  The 1950 Treaty further provided that, except for certain designated portions of the outflow from Lake Erie, the remaining flow was to be divided equally between the United States and Canada and could be used for power generation purposes.  While the 1950 treaty established new baseline flows, it did not alter the jurisdictional authority granted to the IJC by the 1909 Treaty to oversee boundary waters and to ensure that minimum flows are maintained.  In response to the 1950 Treaty, the IJC created the International Niagara Board of Control, which provides routine management authority over the Niagara River

Within approximately three months after the signing of 1950 Treaty, Ontario Hydro began construction of the Sir Adam Beck 2 Generating Station, designed to use Canada’s share of the water.

In response to the June 7, 1956, collapse of the Schoellkopf power plant, Congress passed the Niagara Redevelopment Act in August 1957, directing the Federal Power Commission (today’s Federal Energy Regulatory Commission, or FERC) to issue a license to the Power Authority for the construction and operation of a power project with capacity to utilize the entire United States share of the Niagara River permitted to be used by international agreement.  President Dwight D. Eisenhower signed the legislation on August 21, 1957.  On January 30, 1958, following several months of hearings in Washington, D. C., the Federal Power Commission issued the license to the Power Authority.

The water level in the Chippawa-Grass Island Pool is regulated in accordance with a 1993 directive of the International Niagara Board of Control.  This directive requires that, to ameliorate the adverse effect of high or low water levels in the pool, the Power Entities (Ontario Power Generation, or OPG, and the Power Authority) operate the International Niagara Control Structure to ensure the maintenance of an operational long-term average pool level of 171.17 meters (El. 562.75 feet in USLSD 1935, El. 561.5 IGLD 1985).  The directive also establishes adverse high or low water levels in the pool, as well as certain tolerances for the pool’s level as measured at the Material Dock gauge.   The maximum permissible accumulated deviation is 1.5 feet per day within a 3-foot normal range.  The maximum level in the pool may be increased temporarily to assist in flushing ice over the Falls.  The Directive also provides that these tolerances may be waived in case of significant risk of severe property damage or loss of life.

2.3         Pre-Construction Cultural and Social Setting

2.3.1        Population

Niagara County is part of the Buffalo-Niagara metropolitan regional center.  Niagara County has a population of 219,846 (Census Bureau 2000).  The total population of the four Niagara County communities in which Project lands are found (City of Niagara Falls, Town of Niagara, Town of Lewiston, and Village of Lewiston) is 83,609  (Census Bureau 2000).  Niagara County’s largest city, Niagara Falls, has a current population of 55,677, down from 102,394 in 1960 (Census Bureau 2000 and Census Bureau 1960).  Land within the four host communities is used for heavy industrial, residential, and agricultural purposes, with the City of Niagara Falls being the industrial center of the area.

In the past century, the Niagara region has undergone extensive change.  An area where this change is most evident is population.  As a whole, Niagara County’s population grew steadily from 74,961 in 1900 to 242,269 in 1960.  The Towns of Niagara and Lewiston, the Village of Lewiston, and the City of Niagara Falls also exhibited this trend for the same period.  From 1930 to 1960, the City of Niagara Falls and the communities adjacent to it formed 60% of the county’s population. 

The population of the City of Niagara Falls, which was the major population center for the region before and during construction, grew from 11,700 in 1893 to 19,457 in 1900, and reached its peak of 102,394 before 1960 (Census Bureau 1962).  This last population increase paralleled the city’s transformation into the commercial and cultural center of the region.  A trend toward suburbanization would soon follow, however, with substantial population growth in surrounding towns and villages.  Urban and suburban growth proceeded concomitantly during the 1950s, but urban growth peaked around 1960, and City of Niagara Falls population began to decline.

2.3.2        Economy

Prior to Project construction, manufacturing was the largest sector of Niagara County industry.  In 1950, 37,353 people are employed in the manufacturing sector, with 18,697 of them employed in the City of Niagara Falls.  The development of industry in Niagara Falls was primarily due to the proximity of the Niagara River’s hydroelectric power.  Among the first industries to move to the Niagara region were the Carborundum Company, Pittsburgh Reduction, Union Carbide, and the International Paper Company.  As the manufacturing processes advanced, the economy of the region likewise advanced.

In 1950, retail and wholesale trade was the next largest industrial sector.  Niagara County employed over 11,294 people in this industry, of which over 6,000 were employed in the City of Niagara Falls.  The service sector was the third largest employer, with 5,363 people employed in the county and 2,563 of these in the City of Niagara Falls.  These statistics support the fact the City of Niagara Falls was the population and industrial center for the Niagara region in 1950.  Outside the City of Niagara Falls, agriculture was the dominant economic activity.

In the early 1900s, agriculture provided a strong basis for local economies.  About half of Niagara County, including the Towns of Niagara and Lewiston and the Village of Lewiston, was devoted to agriculture.  Region wide, dairying and fruit growing were the dominant forms of agriculture.

2.3.3        Parks And Transportation

From 1900 to 1950, the Niagara region was evolving from a slow paced area at the crossroads between two countries into an-industrial center, due primarily to abundant water and hydroelectric power.  The proximity of the area to a major ship and rail transshipment center, Buffalo—not to mention the attraction of the Falls itself—added greatly to the vitality of the region.  The explosive industrial growth and the rise of tourism brought about a spirited and lengthy public debate on whether this same rapid development of tourism and industry was ruining the scenic beauty of the Niagara region and particularly of Niagara Falls.

This concern for the preservation of the environment had, previous to the twentieth century, resulted in the “Free Niagara Movement,” led by Frederick Law Olmsted.  In 1885, the State of New York took control of the land bordering the American Falls, and created the 430-acre Niagara Reservation State Park, the nation’s oldest state park.  The park is made up of numerous islands, as well as the Prospect Point area (Figure 2.3-1).  Reservation State Park highlights include a visitor center, observation tower where elevators take visitors either down to the base of the gorge or 80 feet above street level to view the Falls, and guided trolley tours of the park’s most scenic vistas.  Since the creation of this first park, more land has been set aside as parkland (Whirlpool State Park, Devils Hole State Park, and Artpark), helping  the region remain a major tourist area.

In addition to Reservation State Park, other parks were found throughout the region prior to Project construction.  Three of today’s parks that existed prior to construction are:

·         Hyde Park, the largest park operated by the city (Figure 2.3-1).  Prior to the construction of the NPP, Hyde Park had an 18-hole golf course, athletic fields, and various nature trails along Gill Creek, which flowed through the park’s western portion.  A number of changes have been made to Hyde Park.  These will be detailed in Section 4.0.

·         The Whirlpool Rapids Trails, located 2 miles north of Niagara Falls.  The trail system here offers two levels of recreational opportunities.  The upper level offers views of the mile-long rapids, along with a playground and picnic area.  The river level is accessible by walking the trails and steps that descend into the Niagara gorge and that lead to Devil’s Hole State Park.  The Niagara Gorge Trail System extends through the park and parallels the Niagara gorge, which extends from Niagara Falls to Lewiston. 

·         Bond Lake County Park, a 545-acre park in the Town of Lewiston developed for multiple uses.  The lakes attract migrating waterfowl during spring and fall while the surrounding fields and brushland support a variety of birds and wildflowers.  A narrow section of the Niagara escarpment occurs along the southern edge of the park.  Here are found 13 miles of trails for hiking, horseback riding, and cross-country skiing.

Throughout the early twentieth century, the increased use of the automobile as well as the extension and improvement of roads made the Niagara region more accessible and contributed to an upswing in visitors to the region.  The transportation system of the region played an additional role in providing mobility to residents of the region.  Even though the Niagara region was not connected directly to an interstate or to the New York State Thruway, the network of town and city streets and county roads and rail lines allowed efficient vehicular movement in and around the Niagara region. 

The City of Niagara Falls was the location for the first suspension bridge across the Niagara River—the Niagara Suspension Bridge (over the Whirlpool Rapids)—and soon developed into a major international rail transshipment center.  Population was starting to locate to the city.  A streetcar service was soon set up in response to the population growth.  This streetcar provided service to Niagara Falls and Queenston, Ontario, via two international crossings, and to Lewiston.  Eventually streetcars and rail passenger service were phased out, and supplanted by automobiles.

2.3.4        Niagara University

Niagara University was founded in 1856, and in 1863 was chartered by the New York State legislature as the Seminary of Our Lady of Angels.  Following the destruction of the original building by fire in December 1864 new construction was undertaken, and by April 1865, the first buildings of the present university were built.  In 1869, the original structure was rebuilt.  The suburban campus occupies 300 acres adjacent to the Project, with institutional buildings, residences, athletic complexes and parking.

2.3.5        Tuscarora Nation

The lands of the Tuscarora Nation are bounded the Town of Lewiston.  Before project construction, they consisted of 6,249 acres or about 9.8 square miles that were composed of three contiguous parcels acquired by the Tuscaroras at different times.  The Senecas, who originally owned the land, granted the Tuscaroras 640 acres to settle sometime in the late 1700s.   They sold their interests to the Holland Land Company in 1797 who then ceded one square mile to the Tuscaroras in 1798.   The Company ceded a second parcel of 1,280 acres to the Tuscaroras in 1799.  In 1804, using funds from the sale of Tuscarora lands in North Carolina that were held in trust by the United States Secretary of War, the Tuscaroras purchased a third land parcel consisting of 4,329 acres from the Holland Land Company.  Fee title to this tract was subsequently transferred by the United States to the