Seneca Indian Tribe History
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Historic Aspects of the Phelps and Gorham Treaty of July 4-8, 1788
Edited by DEXTER PERKINS, City Historian and BLAKE MCKELVEY, Assistant City Historian VOL. 1 JANUARY, 1939 No. 1 Historic Aspects of the Phelps and Gorham Treaty of July 4-8, 1788 By BLAKE MCKELVEY The commemoration of the 150th anniversary of the Phelps and Gorham treaty with the Indians presents a challenge to the imagination. The years that have passed since that July council on Buffalo Creek have seen great changes come over this beautiful country. We think first of the marvellous material changes that have taken place, for they are obvious on all sides. We might with much profit consider the institu- tional and cultural developments that make those events of 150 years ago appear like the fanciful episodes of some romantic tale. But it is not the contrast or the changes that we wish to com- memorate. That council on Buffalo Creek was a very real, a very significant occasion. The chain of events of which it was a part, and the setting in which it occurred, were vital aspects of the history of Western New York, and influenced developments throughout the country. Therefore, the recollection of this historic occasion merits our close attention, even though we shall have to turn over many of history’s musty pages in the process. A brief study of the documents is enough to reveal that the men who took part in the treaty at Buffalo Creek, and in the far-flung intrigues that followed it, were sons of Adam as we know them today- some crafty and some straightforward, some simple and some endowed with foresight, some mean and selfish, and some honestly concerned ROCHESTER HISTORY, published quarterly by the Rochester Public Library, dis- tributed free at the Library, by mail 25 cents per year. -
Tackling Pinot Noir in the Finger Lakes at Forge Cellars, Partners from the Rhône Valley and New York Meet the Challenge
Search Site Sign In | Create Account August 2017 Issue of Wines & Vines SUBSCRIBE » Tackling Pinot Noir in the Finger Lakes At Forge Cellars, partners from the Rhône Valley and New York meet the challenge by Ray Pompilio Pinot Noir is a difficult cultivar to grow successfully. Named “the heartbreak grape” by Marq De Villiers in his 1994 book about winemaker Josh Jensen at the Calera Wine Co., it continues to challenge growers and winemakers throughout numerous grapegrowing regions, especially in New York’s cool- climate Finger Lakes. This challenge is being met head-on by a partnership stretching from Gigondas, France, to Hector, N.Y., with its center at Forge Cellars on the east shore of Seneca Lake. The three partners include Louis Barruol, winegrower and winemaker for Chateau de Saint Cosme, owned by his family since 1570 (Barruol is the 42nd family member to serve as winemaker), and two wine professionals in the Finger Lakes: winemaker Justin Boyette and general manager/vineyard manager, Rick Rainey. Forge Cellars’ 2011 vintage, its first, was produced at the Hector Wine Co., where Boyette is winemaker. Each vintage through 2016 was produced there, but Forge now has a brand-new standalone facility built nearby. The winery produces wines only from Riesling and Pinot Noir. The 2015 and 2016 vintages are currently aging at the new winery, and 2017 will be the first vintage produced there. The new, energy-efficient winery facility is a 6,500-square-foot building designed and built under the direction of Rick Rainey. It was constructed of structural insulated panels (SIP) built by Energy Panel Structures Inc. -
Notable Local Floods of 1942-43
Notable Local Floods of 1942-43 GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1134 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1952 CONTENTS The letters in parenthesis preceding the titles are those used to designate the separate chapters] Page (A) Flood of August 4-5, 1943, in central West Virginia, by H. M. Erskine. 1 (B) Floods of July 18, 1942, in north-central Pennsylvania, by William S. Eisenlohr, Jr________________________________________________ 59 ILLUSTRATIONS PLATE 1. Map of West Virginia showing location of points where flood determinations were made__________--_-_--__-_-_-_--__-_ 48 2. Map of flood area showing locations of stream-gaging stations, rainfall-measurement points, and isohyetal lines for July 17-18, 1942-____-___________________-___-______--_-_-____- In pocket FIGURE 1. Map of West Virginia showing location of Little Kanawha River basin_________________________-__-__--_-_---_-_ 2 2. Residence of Yeager family, which was flooded. ____________ 5 3. Residence, near Heaters, which was washed dowiistream_____ 6 4. Washed-out railroad bridge on Copen Run _________________ 6 5. Washed-out fill on State Route 5 at Jobs Run______________ 7 6. Rock and mud deposit from a hillside wash________________ 7 7. Typical sand and gravel deposits__________________________ 8 8. Typical hillside erosion_____________________-_____-__--__ 8 9. Cornfield destroyed by flood. _--_____________-__-__-_-__- 9 10. Isohyetal map of Little Kanawha River basin showing total rainfall July 26-30, 1943__________________--_-____--- 10 11. Isohyetal map of Little Kanawha River basin showing total rainfall August 4-5, 1943__ ______________-___-_--__--__ 13 12. -
2014 Update on the Chloride Hydrogeochemistry in Seneca Lake, New York
A 2014 UPDATE ON THE CHLORIDE HYDROGEOCHEMISTRY IN SENECA LAKE, NEW YORK. John Halfman Department of Geoscience, Environmental Studies Program, Finger Lakes Institute Hobart & William Smith Colleges Geneva, NY 14456 [email protected] 12/10/2014 Introduction: Seneca Lake is the largest of the 11, elongated, north-south trending, Finger Lakes in central and western New York State (Fig. 1). It has a volume, surface area, watershed area, and maximum depth of 15.5 km3, 175 km2, 1,621 km2 (including Keuka watershed), and 188 m, respectively (Mullins et al., 1996). The lake basins were formed by glacial meltwaters eroding and deepening former stream valleys underneath the retreating Pleistocene Ice Sheet cutting into the Paleozoic sedimentary rocks approximately 10,000 years ago. Each basin was subsequently filled with a thick deposit of glacial tills and a thin veneer of pro-glacial lake clays. Basins not completely filled with sediment (e.g., Tully Valley), were subsequently filled with water and slowly accumulating postglacial muds. Seneca Lake is classified as a Class AA water resource by the New York State Department of Environmental Conservation (NYS DEC), except for a few locations along the shore (http://www.dec.ny.gov/regs/4592.html, Halfman et al., 2012). It supplies drinking water to approximately 100,000 people in the surrounding communities. Berg (1963) and Schaffner and Oglesby (1978) noted that chloride concentrations were significantly larger in Seneca Lake, and to a lesser extent in Cayuga Lake, than the other Finger Lakes. Wing et al. (1995) argued that the elevated chloride concentrations required an extra source of chloride beyond the measured fluvial fluxes to the lake. -
TRAVELTIME and DISPERSION DATA for the KANAWHA RIVER, WEST VIRGINIA, 1989 by D.H. Appel U.S. GEOLOGICAL SURVEY Open-File Report
TRAVELTIME AND DISPERSION DATA FOR THE KANAWHA RIVER, WEST VIRGINIA, 1989 By D.H. Appel U.S. GEOLOGICAL SURVEY Open-File Report 91-57 Prepared in cooperation with the MARSHALL UNIVERSITY RESEARCH CORPORATION and the VIRGINIA ENVIRONMENTAL ENDOWMENT Charleston, West Virginia 1991 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Dire ptor For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Books a.nd Open-File Reports Section Water Resources Division Box 25425 603 Morris Street Denver Federal Center Charleston, WV 24301 Denver, CO 80225 CONTENTS Page Abstract .......................................................... 1 Introduction ...................................................... 2 Purpose and scope ............................................. 2 Acknowledgments ............................................... 5 Field procedures .................................................. 5 Traveltime and dispersion data .................................... 7 August 1989 ................................................... 7 October 1989 .................................................. 7 References cited .................................................. 16 ILLUSTRATIONS Page Figure 1. Map showing the Kanawha River study area ............... 3 2. Graph showing Kanawha River profile, navigable section .................................... 4 TABLES Page Table 1. Distance, in river miles, to selected sites -
Frozen Cayuga & Seneca Lakes Article with Picture
When Cayuga Lake and Seneca Lake Have Frozen Over by Walt Gable, Seneca County Historian, Feb. 2009 Whenever we have a good “old-fashioned” winter, it is easy for Seneca County residents to begin to speculate if ‘the lake might soon freeze over.” The odds, while not great, are better that it could happen to Cayuga Lake than Seneca Lake. This is because Cayuga Lake has frozen over several more times in recorded history than has Seneca Lake. Cayuga Lake also froze over more recently (1979) than Seneca Lake (1912). This 1927 picture shows a frozen Cayuga Lake near the village of Cayuga. The infrequent freezing of Seneca Lake has led to a joke that people should put Seneca Lake water in their car’s radiator because this water never freezes. Apparently this comment was frequently mentioned to the trainees at Sampson Naval Station during World War II.1 Arch Merrill in his 1951 book Slim Finger Beckon makes reference to this “modern legend.” Some Basic Information Before going any further in this discussion, there needs to be clarification as to just what constitutes a “frozen over lake.” For our purposes in this article, “frozen over lake” will mean a lake whose surface is virtually entirely frozen over—allowing for some isolated “air holes” and/or areas nearer to shore where there is some “open water,” perhaps because of warm water being discharged. In other words, we will use “frozen over” to mean the same as “virtually completely frozen over.” If a portion of either Cayuga or Seneca Lake has ice extending from some place on the eastern shoreline to the western shoreline, when other parts of the lake are not frozen from shore to shore, this will not be considered as completely frozen over. -
Lower Buffalo Bridge Buffalo, West Virginia
Merit Award: Long Span Lower Buffalo Bridge Buffalo, West Virginia This $21.8 million project con- nects US 35 to WV62 over the Kanawha River near Buffalo, West Virginia. The bridge site is in the Kanawha Valley of Putnam County, West Virginia, halfway between Charleston, the state’s capital and largest city, and Huntington, the sec- ond largest city in the state. The broad Kanawha Valley is surrounded by rolling hills and dotted with farm- ing communities and newer subur- ban areas. Although Putnam County is one of the fastest growing counties in the state of West Virginia, there was no bridge crossing the Kanawha River within miles of Buffalo. The new Lower Buffalo Bridge opens up some of the best land in the state to economic development and provides a direct connection to a new US 35 upgrade under construction and I- 64. The bridge had to be completed and open to traffic by mid-1998 to allow for the new Toyota manufacturing facility in Buffalo to ship state-of-the-art engines. The bridge also had to span the naviga- ble Kanawha River with minimal false- work and span over areas on both banks with known archeological deposits. Environmental Concerns The flood plain area at the Lower Buffalo Bridge site is an established archeological dig site with numerous Native American campsites and artifacts. An environmental consultant for the West Virginia Department of Transportation (WVDOT) performed both phase one and phase two archeo- logical surveys at the proposed bridge site and identified archeologically sensitive areas on both riverbanks. Construction activity for a new bridge over these sensi- tive areas was limited to the depth of cul- tivation (about 30”). -
The Emergence and Decline of the Delaware Indian Nation in Western Pennsylvania and the Ohio Country, 1730--1795
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by The Research Repository @ WVU (West Virginia University) Graduate Theses, Dissertations, and Problem Reports 2005 The emergence and decline of the Delaware Indian nation in western Pennsylvania and the Ohio country, 1730--1795 Richard S. Grimes West Virginia University Follow this and additional works at: https://researchrepository.wvu.edu/etd Recommended Citation Grimes, Richard S., "The emergence and decline of the Delaware Indian nation in western Pennsylvania and the Ohio country, 1730--1795" (2005). Graduate Theses, Dissertations, and Problem Reports. 4150. https://researchrepository.wvu.edu/etd/4150 This Dissertation is protected by copyright and/or related rights. It has been brought to you by the The Research Repository @ WVU with permission from the rights-holder(s). You are free to use this Dissertation in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you must obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Dissertation has been accepted for inclusion in WVU Graduate Theses, Dissertations, and Problem Reports collection by an authorized administrator of The Research Repository @ WVU. For more information, please contact [email protected]. The Emergence and Decline of the Delaware Indian Nation in Western Pennsylvania and the Ohio Country, 1730-1795 Richard S. Grimes Dissertation submitted to the Eberly College of Arts and Sciences at West Virginia University in partial fulfillment of the requirements for the degree of Doctor of Philosophy in History Mary Lou Lustig, Ph.D., Chair Kenneth A. -
Seneca County Report.Indd
A Greenprint for Seneca County Prepared by Kristine West for the Finger Lakes Land Trust A Greenprint for Seneca County Prepared by Kristine West for the Finger Lakes Land Trust Contents Executive Summary 3 The Planning Process 5 Introduction 6 Greenprint Components 9 Agriculture 9 Tourism 12 Surface Water Resources 14 Natural Resource Focus Areas 18 Scenic Lakeshore Areas 18 Shoreline Properties 20 Montezuma Wetlands Complex 21 Finger Lakes National Forest 23 Junius Ponds 25 Former Seneca Army Depot 26 Grassland Bird Habitat 27 Canoga Marsh 28 Conservation Toolbox 29 Conservation Easements 29 Technical Assistance and Incentive Programs 31 Planning and Land Use Regulation 31 Resource Contacts 33 Acknowledgements 34 End Notes 35 Publication date: March 2010 2 Executive Summary The Seneca County Greenprint is a plan that identifi es links between the county’s natural resources, its economic development and its overall quality of life. Its purpose is to promote the conservation of environmental assets which underpin Seneca County’s economic, cultural and environmental vitality. The key components of this greenprint are lands vital to water quality, agriculture, compatible tourism, and the health of eight natural resource focus areas. Descriptions of each component include an assessment of the resource and potential threats to its long term viability. Recommendations are made for each resource to promote conservation through collaborative and community based efforts. Sprawling development patterns threaten the Finger Lakes Region, degrading agricultural viability, environmental quality and the rural lifestyle held dear to area residents. Given its distance from major urban centers, Seneca County has been spared intense development pressures thus far. -
GROWN HERE. MADE HERE. Vescelius New York Wine & Plants Frst N.Y
grown here. made here. Seneca Lake Winery Association, Inc. Association, Seneca Lake Winery 320 Suite Street, Franklin 2 North 14891 York Glen, New Watkins (877) 536-2717 (607) 535-8080 or [email protected] senecalakewine.com Here’s to the farmers, Situated around the deep, blue waters of Seneca Lake, our unique, glacially-formed And their vision. landscape and sloping shorelines create an To the growers, ideal cool-climate growing region that allows And their bounty. our members to grow a number of delicate vinifera grapes like Riesling, Chardonnay, and To the makers. other aromatic whites. Red varieties such as To the artists. Cabernet Franc and Pinot Noir also thrive here, resulting in an array of diferent varieties and To their craft. styles, most made from grapes harvested within Here’s to the tasters, federally recognized Seneca Lake American Viticultural Area (AVA). We guarantee that you’ll And the diners. find a wine perfect for you! To the lovers, And friends. Our member wineries promote a spirit of cooperation to develop an outstanding and To the locals, comprehensive wine tourism region and are And the wanderers. dedicated to creating premium, award-winning wines suitable for every palate. Furthermore, To the Finger Lakes. Seneca Lake Wine Trail member wineries To this lake. are committed to enhancing the region’s economy and quality of life through a variety To these hills. of innovative and cooperative events and These waters. programs year-round. These vines. Since our organizations founding in 1986, These grapes. we have become a popular wine and grape Here’s to our passion. -
Seneca Lake Guardian
GOVERNMENT OPERATIONS COMMITTEE April 2, 2018 at 1:30 pm Location: Legislative Chambers Committee members: Tim Dennis Chair, Jim Multer, Vice Chair, Carlie Chilson, Tim Cutler, Earle Gleason, Bonnie Percy Tim and Tim Cutler will sign the audit this month Approve minutes of the March meeting Public Comment o Joseph Campbell, President Seneca Lake Guardian Legislative Operations Tim Dennis – Resolution Opposing Waste-To-Energy Plant Proposed Fro Former Seneca Lake Army Depot Site. Elections – Robert Brechko/Amy Daines State Legislative update March Accomplishments April Objectives Soil & Water –Colby Petersen Program updates Cornell Cooperative Extension – Arlene Wilson Program updates IT – Tim Groth Help Desk calls Program updates County Clerk – Lois Hall Statistical summary DMV updates Clerk updates Clerk of the Legislature – Connie Hayes Nothing to report this month Personnel – Kerry Brennan Various Department updates Policy Discussions Continuing Education Resolution – Amending Resolution No. 129-18 Adopt 2018 Non-Union Salary Schedule County Administrator – Robert Lawton Recruit new Historian Various other activity updates EXECUTIVE SESSION – If needed SENECA LAKE GUARDIAN senecalakeguardian.org PO Box 333 Watkins Glen, NY 14891 [email protected] Know the Facts about the Trash Incinerator Plant Proposed for the Seneca Army Depot in Romulus NY. Sponsor: Circular enerG, Rochester company with no experience handling garbage or energy production, has proposed building a giant waste incinerator. Circular enerG was incorporated in January of 2017 and the names of the investors and officers are a secret. Property owner: The land is owned by Seneca Depot LLC, a subsidiary of Flaum Management. Seneca Depot LLC is promoting the project. Seneca Depot LLC shares a Rochester address with Circular enerG, Rochester developer David M. -
The Lake Reportersummer 2017 the Lake Reportersummer 2017
THE LAKE REPORTERSUMMER 2017 THE LAKE REPORTERSUMMER 2017 The Annual Meeting is a great place to hear more about current initiatives and watershed topics. 2017 ANNUAL Join us for a business meeting with officer elections, reports from the Chair and Treasurer, and award recognitions. Stay for two great presentations that are sure to MEETING be of interest to all watershed residents. Mission of the Finger Lakes Water Hub Anthony Prestigiacomo, Research Scientist with the Finger Lakes Water Hub, will THURSDAY AUGUST 17 introduce us to the group’s mission of addressing water quality issues across the FLCC STAGE 14 AT 6 PM Finger Lakes region. “State of the Lake” Presentation Kevin Olvany, Watershed Program Manager (Canandaigua Lake Watershed Council) will deliver the evening’s keynote presentation on the current water quality status of Light refreshments will be provided. the Canandaigua Lake watershed. Kevin will share water quality data looking at long A donation of $5 is suggested. RSVP to -term trends from the last 20 years of monitoring, and will identify potential threats [email protected] to the health and overall environment of the lake. Impacts of the area’s recent storm or 394-5030. events will also be discussed. We hope you will join us on August 17th to learn more about what your membership dollars help support. CITIZEN SCIENCE IN ACTION! By Nadia Harvieux, CLWA Community Outreach Committee The Community Outreach Committee has launched three citizen and NYSFOLA science initiatives for the 2017 summer lake sampling season. With will report the the goal of understanding our lake ecosystem better, CLWA is results of the partnering with local, regional and state water quality experts to train sampling in early volunteers in collecting a wide range of data about Canandaigua 2018.