Modeling of the Genesee River Watershed Using Swat 2000
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Schedule of Events
Spring 2020 FLTC Weekend & Annual Membership Meeting June 12th, 13th, 14th 2020 Jointly hosted by Foothills Trail Club & Genesee Valley Hiking Club Houghton College Houghton, N.Y. 14744 Join us for a weekend of all things Finger Lakes Trail! Connect with fellow members, hear from exciting and interesting speakers, share in our annual Awards Presentation and attend the Annual Meeting, and of course GO FOR A COUPLE OF HIKES! This year’s Spring Weekend and Annual Membership Meeting will be help at Houghton College. Houghton College was established in 1776 as a seminary to provide leaders for the Wesleyan Church. It is a nationally ranked Christian liberal arts college located in the scenic Genesee Valley of western New York State. It is built on the steeper shores of the Genesee River with stones brought up from the river bed by the grandfathers of some of the present staff. It is a beautiful setting with buildings of soft gray exhibiting classic Greek architecture. It is a church oriented campus, so alcohol is prohibited. The campus is on 1300 acres and has over 4 miles of hiking trails in the Houghton Forest and a creek that runs through the campus. Bring your kayak or canoe to paddle on the Genesee River. The campus is located 15 miles south of Letchworth State Park, “The Grand Canyon of the East,” with gorgeous waterfalls and hiking trails. Schedule of Events Friday, June 12 11 AM – 5 PM Registration opens, first floor of Reinhold Campus Center 12 – 2 PM Hikes, events depart, from Gillette Hall parking lot - see MAP 4:30 – 5:30 Social hour at StillWaters Inn, 7 miles South on Rt. -
Frasnian (Upper Devonian) Strata of the Genesee River Valley, Western New York State
FRASNIAN (UPPER DEVONIAN) STRATA OF THE GENESEE RIVER VALLEY, WESTERN NEW YORK STATE WILLIAM T. KIRCHGASSER D. JEFFREY OVER Deprtment of Geology Department of Geological Sciences SUNY-Potsdam SUNY-Geneseo Potsdam, New York 13676 Geneseo, New York 14454 DONALD L. WOODROW Department of Geoscience Hobart and William Smith Colleges Geneva, New York 14456 INTRODUCTION History of Investigation The Frasnian section in the Genesee Valley is located in the western part of the central Devonian outcrop belt of New York State that stretches 'from the Catskill Mountains to Lake Erie. The Genesee Valley was close to the center of the Fourth Geologic District of the first state survey, the district between Cayuga Lake and Lake Erie, covered by James Hall. Hall's final report, the monumental Part IV of the Geology of New York (Hall, 1843), is the starting point for Devonian studies in the region (Figure 1). The rocks of the classical Genesee, Portage and Chemung divisions consist of a succession of marine siliciclastics beginning with dark basinal shales (Genesee) that contain a pelagic molluscan fauna, which are overlain by lighter colored shales and siltstones that contain a pelagic and benthic fauna (Portage and Naples to the east) that were deposited in basin-and-slope environments. These strata are overlain by siltstones and sandstones bearing a benthic brachiopod fauna (Chemung) that were deposited on the slope and outer shelf. Most of the fossils in these units were described in monographs by Hall (1879) and Clarke (1899, 1904). The excellent exposures in the Genesee Valley made this section a center for geological studies of the distal rocks of the Catskill Delta, which record stages in the filling of the Appalachian Foreland Basin. -
Phase 1A Historic Resources Survey Morris Ridge Solar Energy Center Town of Mount Morris, Livingston County, New York
Phase 1A Historic Resources Survey Morris Ridge Solar Energy Center Town of Mount Morris, Livingston County, New York Prepared for: EDF Renewables Development, Inc. A subsidiary of EDF Renewables, Inc. 15445 Innovation Dr. San Diego, California 92128 Prepared by: Environmental Design & Research, Landscape Architecture, Engineering & Environmental Services, D.P.C. 217 Montgomery Street, Suite 1000 Syracuse, New York 13202 P: 315.471.0688 F: 315.471.1061 www.edrdpc.com May 2019 Phase IA Historic Resources Survey Morris Ridge Solar Energy Center (Case 18-F-0440) Town of Mount Morris, Livingston County, New York Prepared for: Morris Ridge Solar Energy Center, LLC An indirect subsidiary of EDF Renewables, Inc. 15445 Innovation Dr. San Diego, California 92128 Contact: Kevin Campbell Phone: (844) 553-3336 Project Email: [email protected] Prepared by: Environmental Design & Research, Landscape Architecture, Engineering, & Environmental Services, D.P.C. 217 Montgomery Street, Suite 1000 Syracuse, New York 13202 www.edrdpc.com May 2019 MANAGEMENT SUMMARY SHPO Project Review Number: 19PR01246 Involved State/Federal Agencies: New York State Office of Parks Recreation and Historic Preservation (Section 14.09); New York State Department of Public Service (Article 10) Phase of Survey: Phase IA Historic Resources Survey Location Information: Town of Mount Morris, Livingston County Survey Area: Project Description: 177-megawatt utility-scale solar facility consisting of ground-mounted photovoltaic arrays and associated infrastructure. Project Area: -
Hydrologic Evidence of Climate Change in Monroe County, New York
OF M TY ON N R U O O E C S T K A T R E YO OF NEW Maggie Brooks County Executive Prepared in cooperation with the Monroe County Department of Health Hydrologic Evidence of Climate Change in Monroe County, New York ncreasing evidence of climate change has raised concerns that the predicted increases in air temperature and attendant changes in precipitation patterns will affect water resources around the world. An analysis of long-term meteorological and streamflow records can be used to identify trends that might be indicative of climate change, especially with respect to the magnitude and Ifrequency of floods and droughts in western New York, including Monroe County. IN BRIEF . Long-term annual mean air temperatures have been increasing over the past 40 years, but not beyond the historical range as defined by temperatures that have been recorded since 1890. Annual precipitation totals in the Great Lakes Basin within the United States have increased by an average of 4.5 inches since 1915. The chance that daily precipitation will exceed 2.0 inches has increased from once in 5 years prior to 1963 to nearly once every year since 1992, and the chance that daily precipitation will exceed 2.5 inches has increased from once every 20 years to almost once every 4 years. In urban streams, 7-day high flows and the Streams under drought (above) and flood (below) conditions. frequency of peak flows are increasing, whereas base flows are decreasing. In rural streams, base flows and 7-day low flows are increasing, whereas 7-day high flows show no discernible trend. -
The Genesee River Basin
Bureau of Watershed Assessment and Research Division of Water NYS Department of Environmental Conservation The 2001 Genesee River Basin Waterbody Inventory and Priority Waterbodies List Encompassing all or portions of Allegany, Cattaraugus, Genesee, Livingston, Monroe, Ontario, Orleans, Steuben and Wyoming Counties March 2003 Table of Contents The Waterbody Inventory and Priority Waterbodies List. 1 Comprehensive Assessment Strategy. ...............................................1 Statewide Waters Monitoring Program.........................................2 Water Quality Assessments: Updating the WI/PWL . 2 An Expanded Waterbody Inventory ...........................................2 The Genesee River Basin ...............................................................5 Basin Description ...............................................................5 Water Quality Issues/Problems .....................................................5 Genesee River Basin Water Quality Assessment . 7 Basin Water Quality Summary .....................................................8 The 2001 Genesee River Basin Waterbody Inventory/Priority Waterbodies List. 9 Waterbody Inventory Data Sheets Lower Genesee River Watershed ............................................1 1 Lower Genesee River, Main Stem . ....................................1 3 Tribs to Lower Genesee River, Rochester to Rush .. 2 2 Black Creek Watershed ........................................2 6 Oatka Creek Watershed . ......................................3 5 Tribs to Lower Genesee River, Rush -
Letchworth State Park
2020 Wyoming County Adventure Guide Home of the Grand Canyon of the East Letchworth State Park ”OUR HOME, YOUR ADVENTURE” GOWYOMINGCOUNTYNY.COM | 1-800-839-3919 WELCOME TO WYOMING COUNTY Montreal Ottawa Yours to Explore 401 VT 81 87 GREAT BEND AT LETCHWORTH STATE PARK, PHOTO CREDIT DARREN FOX Toronto NY NH Lake Ontario QEW Syracuse Niagara Rochester Falls 90 90 Buffalo Boston 81 Albany Lake Erie 88 MA Welcome and thank you! 90 86 Thank you for picking up the 2020 Wyoming County, NY, Visitor Guide. We invite 17 87 Erie 17 you to visit our home, and have your next family adventure in our beautiful 90 CT RI Scranton outdoor landscape. 79 PA New York City We are very proud to be the home of Letchworth State Park, and invite you to 81 NJ Harrisburg experience its majestic beauty. Come and see why it was voted #1 State Park in Pittsburgh Newark the US, and #1 attraction in New York State. Philadelphia • Albany, NY – 3.75 hours After your visit to Letchworth State Park, there are plenty more attractions waiting just a short drive away. Enjoy a historic train excursion aboard the Arcade & Attica • Cleveland, OH – 3.25 hours Railroad, get up-close with exotic animals at Hidden Valley Animal Adventure, and • New York City, NY – 5 hours enjoy delicious food while watching a drive-in movie at the one-of-a-kind Charcoal • Pittsburgh, PA – 3.75 hours Corral and Silver Lake Twin Drive-in. These are just a few of the fun and exciting • Boston, MA - 7 hours experiences that await you here in Wyoming County, NY. -
14 Section 5.4.4
Section 5.4.4: Risk Assessment – Flood 5.4.4 Flood This section provides a profile and vulnerability assessment of the flood hazard. 5.4.4.1 Hazard Profile This section provides profile information including description, location, extent, previous occurrences and losses, probability of future occurrences, and climate change impacts, as well as the vulnerability assessment for the flood hazard in Monroe County. Description Floods are one of the most common natural hazards in the United States. They can develop slowly over a period of days or develop quickly, with disastrous effects that can be local (impacting a neighborhood or community) or regional (affecting entire river basins, coastlines, and multiple counties or states) (Federal Emergency Management Agency [FEMA] 2008). Most communities in the United States have experienced some kind of flooding after spring rains, heavy thunderstorms, coastal storms, or winter snow thaws (George Washington University 2001). Floods are the most frequent and costly natural hazards in New York State (NYS) in terms of human hardship and economic loss, particularly in communities that lie within flood-prone areas or flood plains of a major water source. As defined in the NYS Hazard Mitigation Plan (HMP), flooding is a general and temporary condition of partial or complete inundation on normally dry land deriving from any of the following: • Riverine flooding, including overflow from a river channel, flash floods, alluvial fan floods, dam-break floods, and ice jam floods • Local drainage or high groundwater levels • Fluctuating lake levels • Coastal flooding • Coastal erosion (NYS Division of Homeland Security and Emergency Services [DHSES] 2014) • Unusual and rapid accumulation or runoff of surface waters from any source • Mudflows (or mudslides) • Collapse or subsidence of land along the shore of a lake or similar body of water caused by erosion, waves, or currents of water exceeding anticipated cyclical levels (FEMA 2014) • Sea Level Rise • Climate Change (U.S.