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Regional Rail Service the Vermont Way
DRAFT Regional Rail Service The Vermont Way Authored by Christopher Parker and Carl Fowler November 30, 2017 Contents Contents 2 Executive Summary 4 The Budd Car RDC Advantage 5 Project System Description 6 Routes 6 Schedule 7 Major Employers and Markets 8 Commuter vs. Intercity Designation 10 Project Developer 10 Stakeholders 10 Transportation organizations 10 Town and City Governments 11 Colleges and Universities 11 Resorts 11 Host Railroads 11 Vermont Rail Systems 11 New England Central Railroad 12 Amtrak 12 Possible contract operators 12 Dispatching 13 Liability Insurance 13 Tracks and Right-of-Way 15 Upgraded Track 15 Safety: Grade Crossing Upgrades 15 Proposed Standard 16 Upgrades by segment 16 Cost of Upgrades 17 Safety 19 Platforms and Stations 20 Proposed Stations 20 Existing Stations 22 Construction Methods of New Stations 22 Current and Historical Precedents 25 Rail in Vermont 25 Regional Rail Service in the United States 27 New Mexico 27 Maine 27 Oregon 28 Arizona and Rural New York 28 Rural Massachusetts 28 Executive Summary For more than twenty years various studies have responded to a yearning in Vermont for a regional passenger rail service which would connect Vermont towns and cities. This White Paper, commissioned by Champ P3, LLC reviews the opportunities for and obstacles to delivering rail service at a rural scale appropriate for a rural state. Champ P3 is a mission driven public-private partnership modeled on the Eagle P3 which built Denver’s new commuter rail network. Vermont’s two railroads, Vermont Rail System and Genesee & Wyoming, have experience hosting and operating commuter rail service utilizing Budd cars. -
Battle of Valcour Island - Wikipedia
Battle of Valcour Island - Wikipedia https://en.wikipedia.org/wiki/Battle_of_Valcour_Island Coordinates: 44°36′37.84″N 73°25′49.39″W From Wikipedia, the free encyclopedia The naval Battle of Valcour Island, also known as the Battle of Valcour Bay, took place on October 11, 1776, on Battle of Valcour Island Lake Champlain. The main action took place in Valcour Part of the American Revolutionary War Bay, a narrow strait between the New York mainland and Valcour Island. The battle is generally regarded as one of the first naval battles of the American Revolutionary War, and one of the first fought by the United States Navy. Most of the ships in the American fleet under the command of Benedict Arnold were captured or destroyed by a British force under the overall direction of General Guy Carleton. However, the American defense of Lake Champlain stalled British plans to reach the upper Hudson River valley. The Continental Army had retreated from Quebec to Fort Royal Savage is shown run aground and burning, Ticonderoga and Fort Crown Point in June 1776 after while British ships fire on her (watercolor by British forces were massively reinforced. They spent the unknown artist, ca. 1925) summer of 1776 fortifying those forts, and building additional ships to augment the small American fleet Date October 11, 1776 already on the lake. General Carleton had a 9,000 man Location near Valcour Bay, Lake Champlain, army at Fort Saint-Jean, but needed to build a fleet to carry Town of Peru / Town of Plattsburgh, it on the lake. -
Lake Champlain Coordinates: 44°32′N 73°20′W from Wikipedia, the Free Encyclopedia
Lake Champlain Coordinates: 44°32′N 73°20′W From Wikipedia, the free encyclopedia Lake Champlain (French: lac Champlain) is a natural, Lake Champlain freshwater lake in North America, located mainly within the borders of the United States (states of Vermont and New York) but partially situated across the Canada—United States border in the Canadian province of Quebec. The New York portion of the Champlain Valley includes the eastern portions of Clinton County and Essex County. Most of this area is part of the Adirondack Park. There are recreational opportunities in the park and along the relatively undeveloped coastline of Lake Champlain. The cities of Lake Champlain near Burlington in early twilight Plattsburgh and Burlington are to the north and the village of Location New York / Vermont in USA; and Ticonderoga in the southern part of the region. The Quebec portion is located in the regional county municipalities of Le Quebec in Canada Haut- Richelieu and Brome–Missisquoi. Coordinates 44°32′N 73°20′W Primary Otter Creek, Winooski River, inflows Missisquoi River, Lamoille River, Contents Ausable River, Chazy River, Boquet River, Saranac River 1 Geology Primary Richelieu River 1.1 Hydrology outflows 1.2 Chazy Reef Catchment 21,326 km2 (8,234 sq mi) 2 History area 2.1 Colonial America and the Basin Canada, United States Revolutionary War countries 2.2 War of 1812 2.3 Modern history Max. le ngth 201 km (125 mi) 2.4 "Champ", Lake Champlain Max. width 23 km (14 mi) monster Surface 1,269 km2 (490 sq mi) 2.5 Ecology area 2.6 Railroad Average 19.5 m (64 ft) 3 Natural history depth 4 Infrastructure 122 m (400 ft) 4.1 Lake crossings Max. -
030321 VLP Fort Ticonderoga
Fort Ticonderoga readies for new season LEE MANCHESTER, Lake Placid News TICONDEROGA — As countered a band of Mohawk Iro- name brought the eastern foothills American forces prepared this quois warriors, setting off the first of the Adirondack Mountains into week for a new war against Iraq, battle associated with the Euro- the territory worked by the voya- historians and educators in Ti- pean exploration and settlement geurs, the backwoods fur traders conderoga prepared for yet an- of the North Country. whose pelts enriched New other visitors’ season at the site of Champlain’s journey down France. Ticonderoga was the America’s first Revolutionary the lake which came to bear his southernmost outpost of the War victory: Fort Ticonderoga. A little over an hour’s drive from Lake Placid, Ticonderoga is situated — town, village and fort — in the far southeastern corner of Essex County, just a short stone’s throw across Lake Cham- plain from the Green Mountains of Vermont. Fort Ticonderoga is an abso- lute North Country “must see” — but to appreciate this historical gem, one must know its history. Two centuries of battle It was the two-mile “carry” up the La Chute River from Lake Champlain through Ticonderoga village to Lake George that gave the site its name, a Mohican word that means “land between the wa- ters.” Overlooking the water highway connecting the two lakes as well as the St. Lawrence and Hudson rivers, Ticonderoga’s strategic importance made it the frontier for centuries between competing cultures: first between the northern Abenaki and south- ern Mohawk natives, then be- tween French and English colo- nizers, and finally between royal- ists and patriots in the American Revolution. -
Constraints on Lake Agassiz Discharge Through the Late-Glacial Champlain Sea (St
Quaternary Science Reviews xxx (2011) 1e10 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Constraints on Lake Agassiz discharge through the late-glacial Champlain Sea (St. Lawrence Lowlands, Canada) using salinity proxies and an estuarine circulation model Brandon Katz a, Raymond G. Najjar a,*, Thomas Cronin b, John Rayburn c, Michael E. Mann a a Department of Meteorology, 503 Walker Building, The Pennsylvania State University, University Park, PA 16802, USA b United States Geological Survey, 926A National Center, 12201 Sunrise Valley Drive, Reston, VA 20192, USA c Department of Geological Sciences, State University of New York at New Paltz, 1 Hawk Drive, New Paltz, NY 12561, USA article info abstract Article history: During the last deglaciation, abrupt freshwater discharge events from proglacial lakes in North America, Received 30 January 2011 such as glacial Lake Agassiz, are believed to have drained into the North Atlantic Ocean, causing large Received in revised form shifts in climate by weakening the formation of North Atlantic Deep Water and decreasing ocean heat 25 July 2011 transport to high northern latitudes. These discharges were caused by changes in lake drainage outlets, Accepted 5 August 2011 but the duration, magnitude and routing of discharge events, factors which govern the climatic response Available online xxx to freshwater forcing, are poorly known. Abrupt discharges, called floods, are typically assumed to last months to a year, whereas more gradual discharges, called routing events, occur over centuries. Here we Keywords: Champlain sea use estuarine modeling to evaluate freshwater discharge from Lake Agassiz and other North American Proglacial lakes proglacial lakes into the North Atlantic Ocean through the St. -
Valcour Primitive Area
Chambly Canal L’île Valcour comporte 12 km de Comprised of 1,100 acres, Valcour Island is the largest island sentiers de randonnée et 25 Couvrant 4,45 km2, l’île Valcour est la plus grande île du lac emplacements de camping on the New York side of Lake Champlain. It is managed by désignés. Des permis de camping Champlain, côté new-yorkais. Cette zone de nature protégée gratuits d’une durée maximale de the New York State Department of Environmental Conser- 14 jours sont émis par un gardien à l’intérieur du parc des Adirondacks est gérée par le New du parc. Par ailleurs, le site ayant vation as a primitive area within the Adirondack Park. Emphasis adopté le principe du premier York State Department of Environmental Conservation qui is placed on restoring its natural condition, preserving cultural arrivé, premier servi, aucune réser- préconise la restauration du milieu naturel et la préservation Quebec vation n’est acceptée. Pour de plus resources, and affording recreation that does not require amples renseignements sur l’île des ressources culturelles de l’île ainsi que les activités récréa- Beauty Valcour, veuillez communiquer Bay avec le Department of Environmen- Canada extensive man-made Valcour tives n’exigeant pas d’am- Landing tal Conservation au (518) 897-1200. United States facilities or motorized énagements importants equipment. ni de matériel motorisé. With eight miles of Avec sa côte de 13 km shoreline, consisting of constituée d’une variété Spoon Spoon New York a variety of rocky ledges Bay Island de corniches rocheuses and quiet sandy bays, the surplombant de paisibles You Are Here Boating along the rocky ledges of Valcour Island at the recreational potential on baies sablonneuses, le “Baby Blues,” similar to scenes found on Valcour Peru turn of the 19th century. -
The Biography of America's Lake Monster
REVIEWS] The Biography of America’s Lake Monster BENJAMIN RADFORD obert Bartholomew and his broth- er Paul grew up near the shores Rof Lake Champlain, which not The Untold Story of Champ: A Social History of America’s only sparked an early interest in the Loch Ness Monster. By Robert E. Bartholomew. lake monster said to dwell within the State University of New York Press, lake but also steeped them in the social Albany, New York, 2012. ISBN: 978-1-4384-4484-0. and cultural context of the mysterious 253 pp. Paperback, $24.95. beastie. In his new book, The Untold Story of Champ: A Social History of America’s Loch Ness Monster, Robert, a sociologist, Fortean investigator, and former broadcast journalist, takes a fresh look at Champ, long dubbed “America’s Loch Ness Monster.” Roy Mackal, and others who con- the Mansi photo, “New Information There have only been a handful of vened a 1981 conference titled, “Does Surfaces on ‘World’s Best Lake Mon- other books dealing in any depth or Champ Exist? A Scientific Seminar.” ster Photo,’ Raising Questions,” May/ scholarship with Champ, among them The intrigue between and among these June 2013.) Joe Zarzynski’s Champ: Beyond the Leg- researchers is interesting enough to fill Like virtually all “unexplained” phe- end, and of course Lake Monster Mys- several chapters. nomena, the history of Champ is in teries: Investigating the World’s Most There are several good books about part a history of hoaxes, and the book Elusive Creatures, coauthored by Joe the people involved in the search for examines several of them in detail, in- Nickell and myself. -
22 AUG 2021 Index Acadia Rock 14967
19 SEP 2021 Index 543 Au Sable Point 14863 �� � � � � 324, 331 Belle Isle 14976 � � � � � � � � � 493 Au Sable Point 14962, 14963 �� � � � 468 Belle Isle, MI 14853, 14848 � � � � � 290 Index Au Sable River 14863 � � � � � � � 331 Belle River 14850� � � � � � � � � 301 Automated Mutual Assistance Vessel Res- Belle River 14852, 14853� � � � � � 308 cue System (AMVER)� � � � � 13 Bellevue Island 14882 �� � � � � � � 346 Automatic Identification System (AIS) Aids Bellow Island 14913 � � � � � � � 363 A to Navigation � � � � � � � � 12 Belmont Harbor 14926, 14928 � � � 407 Au Train Bay 14963 � � � � � � � � 469 Benson Landing 14784 � � � � � � 500 Acadia Rock 14967, 14968 � � � � � 491 Au Train Island 14963 � � � � � � � 469 Benton Harbor, MI 14930 � � � � � 381 Adams Point 14864, 14880 �� � � � � 336 Au Train Point 14969 � � � � � � � 469 Bete Grise Bay 14964 � � � � � � � 475 Agate Bay 14966 �� � � � � � � � � 488 Avon Point 14826� � � � � � � � � 259 Betsie Lake 14907 � � � � � � � � 368 Agate Harbor 14964� � � � � � � � 476 Betsie River 14907 � � � � � � � � 368 Agriculture, Department of� � � � 24, 536 B Biddle Point 14881 �� � � � � � � � 344 Ahnapee River 14910 � � � � � � � 423 Biddle Point 14911 �� � � � � � � � 444 Aids to navigation � � � � � � � � � 10 Big Bay 14932 �� � � � � � � � � � 379 Baby Point 14852� � � � � � � � � 306 Air Almanac � � � � � � � � � � � 533 Big Bay 14963, 14964 �� � � � � � � 471 Bad River 14863, 14867 � � � � � � 327 Alabaster, MI 14863 � � � � � � � � 330 Big Bay 14967 �� � � � � � � � � � 490 Baileys -
Welcome to the Walk of Change Nature Trail
Welcome to the Walk of Change 3. Monarch butterflies former land clearing for farming. The size of the 6. Is this The End? Monarch butterflies have one of the most stones may reveal whether the adjacent land was As you walked to this stop you may have noticed Nature Trail unusual and extreme life cycles of North used for crops or pasture. Stone piles or walls with a change in light and temperature. You just walked American butterflies. Adults migrate north, large rocks usually suggest the adjacent land was through a climax community. In this case, it is a Here at Knight Island State Park, the arriving in the northeast early in the growing a mowed field or a pasture in which only the large patch of mature forest. This does not mean the end landscape has been affected by many physical season. After mating, a female lays her eggs rocks needed to be removed. Small stones need to of change, though, or static condition in the forest. environmental and cultural factors over the on Common Milkweed, like you can see here. be removed from cultivated plots annually. This New growth slows as the forest canopy becomes geologic timescale. These include weather pile of small stones reveals that the surrounding enclosed with fewer, larger trees that are more extremes, glaciers, human habitation and area was used for crops. The crops grown on spaced out. At this state in a forest’s evolution, livestock grazing. Enjoy a walk along the Knight Island were beans, com and peas. change is brought by natural events such as storms trail system, and keep watch for signs of Common milkweed bringing wind and ice, or from cultural means like these changes; you might even witness some logging. -
The Late Quaternary Paleolimnology of Lake Ontario
Western University Scholarship@Western Electronic Thesis and Dissertation Repository 9-4-2014 12:00 AM The Late Quaternary Paleolimnology of Lake Ontario Ryan Hladyniuk The University of Western Ontario Supervisor Dr. Fred J. Longstaffe The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Doctor of Philosophy © Ryan Hladyniuk 2014 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geochemistry Commons Recommended Citation Hladyniuk, Ryan, "The Late Quaternary Paleolimnology of Lake Ontario" (2014). Electronic Thesis and Dissertation Repository. 2401. https://ir.lib.uwo.ca/etd/2401 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. THE LATE QUATERNARY PALEOLIMNOLOGY OF LAKE ONTARIO (Thesis format: Integrated Article) by Ryan Hladyniuk Graduate Program in Earth Sciences A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy The School of Graduate and Postdoctoral Studies The University of Western Ontario London, Ontario, Canada © Ryan Hladyniuk 2014 Abstract We examined the oxygen isotopic composition of biogenic carbonates, carbon and nitrogen abundances and isotopic compositions of bulk organic matter (OM), and the abundances and carbon isotopic compositions of individual n-alkanes (C17 to C35) for samples from three, 18 m long sediment cores from Lake Ontario in order to: (i) assess how changing environmental parameters affected the hydrologic history of Lake Ontario, and (ii) evaluate changes in organic productivity and sources since the last deglaciation. -
Document Review and Archaeological Assessment of Selected Areas from the Revolutionary War and War of 1812
American Battlefield Protection Program Grant 2287-16-009: Document Review and Archaeological Assessment Document Review and Archaeological Assessment of Selected Areas from the Revolutionary War and War of 1812. Plattsburgh, New York PREPARED FOR: The City of Plattsburgh, NY, 12901 IN ACCORDANCE WITH REQUIREMENTS OF GRANT FUNDING PROVIDED THROUGH: American Battlefield Protection Program Heritage Preservation Services National Park Service 1849 C Street NW (NC330) Washington, DC 20240 (Grant 2287-16-009) PREPARED BY: 4472 Basin Harbor Road, Vergennes, VT 05491 802.475.2022 • [email protected] • www.lcmm.org BY: Cherilyn A. Gilligan Christopher R. Sabick Patricia N. Reid 2019 1 American Battlefield Protection Program Grant 2287-16-009: Document Review and Archaeological Assessment Abstract As part of a regional collaboration between the City of Plattsburgh, New York, and the towns of Plattsburgh and Peru, New York, the Maritime Research Institute (MRI) at the Lake Champlain Maritime Museum (LCMM) has been chosen to investigate six historical Revolutionary War and War of 1812 sites: Valcour Island, Crab Island, Fort Brown, Fort Moreau, Fort Scott, and Plattsburgh Bay. These sites will require varying degrees of evaluation based upon the scope of the overall heritage tourism plan for the greater Plattsburgh area. The MRI’s role in this collaboration is to conduct a document review for each of the six historic sites as well as an archaeological assessment for Fort Brown and Valcour Island. The archaeological assessments will utilize KOCOA analysis outlined in the Battlefield Survey Manual of the American Battlefield Protection Program provided by the National Park Service. This deliverable fulfills Tasks 1 and 3 of the American Battlefield Protection Program (ABPP) Grant 2887-16-009. -
Oxygen-Isotope Variations in Post-Glacial Lake Ontario Ryan Hladyniuk the University of Western Ontario, [email protected]
Western University Scholarship@Western Earth Sciences Publications Earth Sciences Department 1-5-2016 Oxygen-isotope Variations in Post-glacial Lake Ontario Ryan Hladyniuk The University of Western Ontario, [email protected] Fred J. Longstaffe The University of Western Ontario, [email protected] Follow this and additional works at: https://ir.lib.uwo.ca/earthpub Part of the Earth Sciences Commons Citation of this paper: Hladyniuk, Ryan and Longstaffe, Fred J., "Oxygen-isotope Variations in Post-glacial Lake Ontario" (2016). Earth Sciences Publications. 4. https://ir.lib.uwo.ca/earthpub/4 1 1 Oxygen-isotope variations in post-glacial Lake Ontario 2 3 Ryan Hladyniuk1 and Fred J. Longstaffe1 4 5 1Department of Earth Sciences, The University of Western Ontario, London, Ontario, 6 Canada N6A5B7 7 8 Corresponding authors, [email protected] 1-519-619-3857; [email protected], 1-519-661- 9 3177 10 11 Keywords: Lake Ontario, oxygen isotopes, glacial meltwater, Laurentide Ice Sheet, late- 12 Quaternary climate change 13 14 15 16 17 18 19 20 21 22 2 23 Abstract 24 The role of glacial meltwater input to the Atlantic Ocean in triggering the Younger Dryas 25 (YD) cooling event has been the subject of controversy in recent literature. Lake Ontario 26 is ideally situated to test for possible meltwater passage from upstream glacial lakes and 27 the Laurentide Ice Sheet (LIS) to the Atlantic Ocean via the lower Great Lakes. Here, we 28 use the oxygen-isotope compositions of ostracode valves and clam shells from three Lake 29 Ontario sediment cores to identify glacial meltwater contributions to ancient Lake 30 Ontario since the retreat of the LIS (~16,500 cal [13,300 14C] BP).