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Intense rain that fell April 3-5, 1987, in southeastern New York State caused widespread flooding. As much as 9 inches of rain fell in watersheds of the Catskill Mountains, where the soils were already saturated, stream discharges were high, and some reservoirs were at or near capacity from snowmelt and previous rainfall. The flood along Schoharie Creek was the third largest since records began in the early 1900's and was exceeded only by the floods of October 1955 and March 1980. Peak discharge of many streams in the study area exceeded the 25-year recurrence interval. A New York State Thruway bridge collapsed into Schoharie Creek, killing 10 motorists. Flood damage to homes, businesses, crops, roadways, and bridges exceeded $65 million. Five counties were declared as major disaster areas and eligible for Federal disaster assistance. This report presents a summary of peak stages and discharges at sites in the affected area, precipitation maps, floodflow hydrographs of seven streams, inflow hydrographs of six reservoirs, and flood profiles along 83 miles of Schoharie Creek from its mouth on the Mohawk River to its headwaters in the Catskill Mountains. INTRODUCTION An intense coastal storm that moved slowly over southeastern New York State on April 3-6, 1987, brought drenching rain that caused widespread flooding of streams draining the Catskill Mountains (fig. 1). In most areas, the flooding rivaled records set in March 1980, October 1955, and March 1951; in a few basins the floods were the most severe recorded in this century. The rain began late on April 3. By April 6, when the storm ended, more than 9 in. (inches) of rain had fallen over the headwaters of the Schoharie, Esopus, Catskill, Rondout, Neversink, and East Branch Delaware basins. Streams that were already high from rainfall and snowmelt from a week before rose quickly in response to the heavy rain. By late evening on April 4, when the rain began to slacken, the discharge of most rivers in the mountains had peaked, having reached flows near and above the 25-year recurrence interval. State and local emergency services evacuated more than 2,400 persons from their inundated homes. Rising water destroyed more than 50 homes and damaged almost 1,000 more. Many major and secondary highways and bridges were closed when floodwaters topped and washed out road surfaces or scoured and weakened highway embankments and bridge substructures. Floodwaters spread over thousands of acres of farmland, reportedly damaging more than 3,000 acres Upper Hudson Mohawk. Schoharie Susquehanna MONTGOMERY ?/IJreakabeen Franklinton Basin boundary Study area " * * SchoharieRGilboa \ Reservoir' ^ Cannonsville Reservoir c Resecyoir & 42° Base from U.S. Geological Survey State base map. 1974 Figure 1. Major geographic features of Southeastern New York State, through erosion of topsoil and deposition of gravel and debris (figs. 2A-2G). In all, homes, farms, businesses, roads, and bridges sustained direct damages in excess of $65 million (A. Germane, New York State Emergency Management Office, written commun., 1987). The Governor declared five counties (Delaware, Greene, Montgomery, Schoharie, and Ulster) major disaster areas, and, on May 15, the President declared them eligible for Federal disaster assistance (New York State Disaster Preparedness Comm. written commun., 1987). The devastation to mountain and valley communities was extensive, but the flood will be remembered most as the one that claimed 10 lives when the New York State Thruway (Interstate 90) bridge collapsed into Schoharie Creek (fig. 2G). During late morning on April 5, the 120-foot-long center span of the bridge fell into the flood-swollen creek. Five vehicles plummetted 80 ft (feet) into the stream below. Search and rescue efforts were thwarted by deep water and swift currents. Investigators later blamed the failure on scour around one of the four piers that supported the bridge (National Transportation Safety Board, 1988). Purpose and Scope As part of a continuing program with the New York State Department of Transportation to document major floods in New York, the U.S. Geological Survey compiled and analyzed hydrologic data on the flood of April 4-5, 1987, in the Catskill Mountain region. This report documents the storm and flood in three tables and several graphs that present precipitation, discharge, and river-stage and reservoir level information. Water-surface profiles of Schoharie Creek that show water levels of the 1987 flood and the flood of record (October 1955) along 83 mi (miles) above the mouth, are included. Acknowledgments Precipitation data were provided by the New York State Department of Environmental Conservation, Division of Air Resources, and the National Weather Service. Data relating to flood damage were provided by the New York State Emergency Management Office. Benchmark information for the flood profiles was tabulated by the New York State Department of Transportation. The New York Power Authority provided water-level and discharge data on Schoharie Creek. The New York City Department of Environmental Protection provided water-level, diversion, and discharge data on the reservoirs in the New York City water-supply system. Photographs were provided by Sidney Brown of the Schenectady Gazette, Schenectady; Fred McKinney of the Times Union, Albany; and Lee Ferris of the Mountain Eagle, Hunter, N.Y. The authors acknowledge the efforts of the hydrologists and hydrologic technicians who collected the data for this report during and after the flood: P. M. Burke H. G. Lent C. O. Szabo G. D. Casey R. Lumia F. S. Tooher F. N. Dalton R. J. Martin R. A. Trudell D. D. Deloff P. S. Murdoch L. A. Wagner G. D. Firda J. A. Robideau J. F. Wilson J. A. Gardner R. F. Snow G. J. Hebert D. A. Stedfast , Figure 2A.--Lost Clove Road Bridge collapse over Esopus Creek in Shandaken, N. Y. (Courtesy of The Mountain Eagle) Figure 2B.--Undermined Catskill Mountain Railroad track along Esopus Creek in Phoenicia, N.Y. (Cour esy of the Mountain Eagle) Figure 2C.--Eroded County Route 22 along Catskill Creek in Oak Hill, N.Y. (Courtesy of The Mountain Eagle) Figure 2D. East Branch Delaware River overflow near Main Street in Margaretville, N.Y. (Courtesy of The Mountain Eagle) Figure 2E. Inundated Route 30 along Schoharie Creek near Middleburg, N.Y. (Courtesy of the Mountain Eagle) Figure 2F.--Collapsed Mill Point Bridge (Route 161) over Schoharie Creek, (Courtesy of the Times Union) Figure 2G. Collapsed New York State Thruway Bridge over Schoharie Creek, (Courtesy of Schenectady Gazette) Above: as viewed from downstream. Below: aerial view. PHYSIOGRAPHY The Catskill Mountains, in southeastern New York, consist primarily of Devonian-age sandstones and shales in massive beds underlain by Silurian shale, sandstone, and limestone. The area contains rugged mountains with narrow, steep-sided, V-shaped valleys. The mountain peaks range in elevation from 500 to 4,200 ft above sea level. Bedrock is exposed in many places, and elsewhere, the glacially derived soil is shallow and has little water-storage capacity but does support forest growth. South of the Catskills, the Shawangunk Mountains (fig. 1) are Silurian conglomerates overlain by soft Ordovician shale. The Mohawk River valley to the north is a broad flood plain of Ordovician shale and limestone overlain by rich alluvial soil on the flats and sandy, gravelly loam on the higher areas Agency Committee, 1954). (New England-New York InterDrainage Basins The Catskill Mountains separate three major drainage basins: the Hudson, the Delaware, and the Susquehanna (fig. 1). The Hudson River originates in the Adirondack Mountains of New York and flows south for about 240 mi or 315 river mi to the Atlantic Ocean at New York City. The upper Hudson basin drains 4,627 mi2 (square miles) from its headwaters to the confluence with the Mohawk River. The Mohawk River basin drains 3,462 mi2 , and the lower Hudson River basin drains 4,561 mi from the mouth of the Mohawk River to the Atlantic Ocean. The Delaware River basin has its headwaters in the Catskill Mountains. i 2 2 The basin is 260 mi long and drains a 12,765-;mi area, 2,362 mi of which are in New York State. This basin consists of the Upland, the Piedmont, and the Coastal Plain sections, which drain 46, 31, and 23 percent of the basin, respectively. The upland section includes the New York part of the watershed and is characterized by a hilly, mountainous terrain with long, steep slopes (New England-New York Inter-Agency Committee, 1954). The study area consists of the Schoharie basin, the southeastern part of the Mohawk basin, and the western half of the lower Hudson basin, all of which are within the Hudson River basin. It also includes the upland section of the Delaware River basin. Principal Streams Schoharie Creek is a major tributary to 'the Mohawk River, which is the largest tributary to the Hudson River. Catskill, Esopus, and Rondout Creeks drain directly into the Hudson River from the eastern slopes of the Catskills. The Neversink River drains into the Delaware River. I Schoharie Creek Schoharie Creek has cut a deep valley from its headwaters high in the Catskills and drains part of the northern slopes of the mountains. It flows north for 83 mi through wooded, mostly undeveloped land to become a major tributary (923-mi2 drainage area) to the Mohawk River. The Creek passes through Schoharie Reservoir and Blenheim-Gilboa Reservoir. Schoharie Reservoir, built in 1926, has a maximum capacity of 21,551 Mgal (million gallons). Schoharie Creek water is diverted out of the basin through Shandaken tunnel upstream from Gilboa Dam to Esopus Creek, where it is further routed to Ashokan Reservoir for New York City's water supply. Downstream from Schoharie Reservoir is Blenheim-Gilboa Reservoir, a pumped-storage hydroelectric project. Water is pumped from this lower reservoir to the upper reservoir, from which it is released to generate powe

Flood of April 4-5, 1987, in southeastern New York State, with flood profiles of Schoharie Creek