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Ontario, Canada
ONTARIO, CANADA Featuring Niagara Falls July 19 - 30, 2019 Everyone knows Ontario for the Canadian side of Niagara Falls, but did you know that around 40% of Canada’s population lives in Ontario. Did you also know that Ontario is larger than France and Spain combined and it has over 250,000 lakes, which contains a fifth of the planet’s fresh water! Join us as we explore this amazing Canadian province and all it has to offer. Niagara Falls at Dusk DAY 1: Marshall, MN to Davenport, IA Relax and enjoy the scenery aboard your luxury motor coach as you make your way to Davenport, IA today. BW Plus Steeplegate Inn DAY 2: Davenport, IA to Windsor, Ontario Today will be a travel day as you journey to Ontario. Enjoy the stunning scenery of Ilinois, Indiana, and Michigan before crossing the border into Canada. Holiday Inn Express * Breakfast Included DAY 3: Windsor, Ontario to Niagara Falls, Ontario As you continue on to Niagara Falls, Ontario today, you’ll stop in Hamilton for a guided tour of the Dundurn Castle and Gardens. Your costumed guide will take you through the 40-room Italian-style villa that was built in the 1830’s by Sir Allan Napier MacNab, a railway magnate, lawyer and Premier of the United Canadas. You’ll hear stories about the family that lived there and the people who worked there to support their affluent lifestyle. At dusk, you’ll view Niagara Falls as it is transformed into an incredible, multi-colored water and light masterpiece. Comfort Inn Fallsview * Breakfast & Dinner Included DAY 4: Niagara Falls, Ontario to Toronto, Ontario Your day begins with a Niagara Falls guided tour. -
Of the American Falls at Niagara 1I I Preservation and Enhancement of the American Falls at Niagara
of the American Falls at Niagara 1I I Preservation and Enhancement of the American Falls at Niagara Property of t';e Internztio~al J5it-t; Cr?rn:n es-un DO NOT' RECda'dg Appendix G - Environmental Considerations Final Report to the International Joint Commission by the American Falls International Board June -1974 PRESERVATION AND ENHANCEMENT OF AMERICAN FALLS APPENDIX. G .ENVIRONMENTAL CONSIDERATIONS TABLE OF CONTENTS Paragraph Page CHAPTER G 1 .INTRODUCTION G1 CHAPTER G2 .ENVIRONMENTAL SETTING . NIAGARA RESERVATION AND SURROUNDING REGION GENERAL DESCRIPTION ............................................................... PHYSICAL ELEMENTS ..................................................................... GENERAL .................................................................................... STRATIGRAPHY ......................................................................... SOILS ............................................................................................ WATER QUALITY ........................................................................ CLIMATE INVENTORY ................................................................... CLIMATE ....................................................................................... AIR QUALITY .............................................................................. BIOLOGICAL ELEMENTS ................................................................ TERRESTRIAL VEGETATION ..................................................... TERRESTRIAL WILDLIFE ......................................................... -
Summer Reading Program
OUR MISSION SUMMER READING PROGRAM Recent Improvements To strengthen our community through lifelong learning with access to varied collections, • Archives catalog online for Summer Reading Program 2019 programs, and assistance with digital literacy. researchers to browse, Jan. 2019 Each year the Niagara Falls Public Library participates in New York State Summer (https://nflh.libraryhost.com/ ) Reading Program. For 2019, the theme was A Universe of Stories and the Niagara Falls he theme of NFPL services is a vision to build a stronger • In partnership with the Niagara Falls Heritage Area, Public Library had 130 children participate in our “Read and Bead” challenge. Upon community. We are looking forward, planning the directive registering, participants received a chain; time spent reading earned whimsically shaped beads to add to the chain. Tof library services. comprehensive, multi phase inventory of Local History In a January 2020 nationwide Gallup poll, Americans visited their In addition, through generous support from the Friends of the Library and Nioga Library System, we hosted a collection, Phase 1 - May local libraries more frequently than attending the movie theater. On 2019, Phase 2 began in June 2020 family entertainment series that included Dave and Kathleen Jeffers “Make Space for Reading” Show, Checkers average, U.S. adults took 10.5 trips to a local library in 2019, twice the Inventor’s “Back to the Moon Show” and a weekly family film series on Friday afternoons. We offered weekly as many times as going to a movie, theatrical event, or visiting a • Continued Digitization of local history items national/historic park. With this increase in usage, coupled with a through RBD grants and Senator Ortt Bullet Aid story hours for preschoolers and summer fun clubs with space-related STEAM themes for grade school children; need for electronic services, the NFPL is looking towards the future, monies. -
Indiana Glaciers.PM6
How the Ice Age Shaped Indiana Jerry Wilson Published by Wilstar Media, www.wilstar.com Indianapolis, Indiana 1 Previiously published as The Topography of Indiana: Ice Age Legacy, © 1988 by Jerry Wilson. Second Edition Copyright © 2008 by Jerry Wilson ALL RIGHTS RESERVED 2 For Aaron and Shana and In Memory of Donna 3 Introduction During the time that I have been a science teacher I have tried to enlist in my students the desire to understand and the ability to reason. Logical reasoning is the surest way to overcome the unknown. The best aid to reasoning effectively is having the knowledge and an understanding of the things that have previ- ously been determined or discovered by others. Having an understanding of the reasons things are the way they are and how they got that way can help an individual to utilize his or her resources more effectively. I want my students to realize that changes that have taken place on the earth in the past have had an effect on them. Why are some towns in Indiana subject to flooding, whereas others are not? Why are cemeteries built on old beach fronts in Northwest Indiana? Why would it be easier to dig a basement in Valparaiso than in Bloomington? These things are a direct result of the glaciers that advanced southward over Indiana during the last Ice Age. The history of the land upon which we live is fascinating. Why are there large granite boulders nested in some of the fields of northern Indiana since Indiana has no granite bedrock? They are known as glacial erratics, or dropstones, and were formed in Canada or the upper Midwest hundreds of millions of years ago. -
Trails in the Niagara River Greenway
Lower River Upper River The Headwaters LAKE ONTARIO 4 1 2 5 93 3 y. Pk es s PORTER Mo ert b Ro 6 7 Buffalo Ave. 7 8 1 WHEATFIELD 9 18 3 4 5 Ri NIAGARA RIVER ver Rd. LEWISTON 2 8 104 17 CITY OF NORTH 22 VILLAGE OF 190 14 LEWISTON TONAWANDA THE LANDSCAPE 1 12 15 15 16 14 16 TUSCARORA 13 CANADA 18 Parks INDIAN RESERVARION 12 17 E. Robinson KENMORE 17 21 2 GRAND ISLAND 23-26 Aqua Lane Park . 1 13 CANADA Whitehaven Rd. 27/28 34 Black Rock Canal Park. 3 11 . 30-33 20 19 Broderick Park . 3 22 er Rd40 Buffalo River Fest Park . 68 31 23 Riv 4 17 21 38 CITY OF 5 198 16 20 H Cazenovia Park* . 92 10 13 yde 37 TONAWANDA 36 290 Delaware Park* . 13 8 11,12 P 9 190 Lockport Rd. 35 265 Forest 15 27 ar Erie Basin Marina & Gardents . 65 25 k 31 26 30 Front Park* . 25 190 NIAGARA d. Baseline Rd. West Ferry East Ferry R Gallagher Beach . .. 90 28 29 WHEATFIELD r TONAWANDA 20 33 e CITY OF 34 Rd. Ward Sheridan Dr. LaSalle Park . 33 CANADA 21 e. Riv t. BUFFALO 67 Av NIAGARA FALLS 66 S . e Niaga Martin Luther King Jr. Park*. 30 r ra Falls B 22 26 30 35 36 lvd. 68 Rd wa 190 2 23 a Main y Riverside Park* . 62 25 l 31 37 38/39 Ni 27 ar 24 ag De it l South Park* . 93 41 40-54 i 33 63 65 41 KENMORE ara M 33 56 57 58-60 64 Squaw Island Park. -
River Related Geologic/Hydrologic Features Abbott Brook
Maine River Study Appendix B - River Related Geologic/Hydrologic Features Significant Feature County(s) Location Link / Comments River Name Abbott Brook Abbot Brook Falls Oxford Lincoln Twp best guess location no exact location info Albany Brook Albany Brook Gorge Oxford Albany Twp https://www.mainememory.net/artifact/14676 Allagash River Allagash Falls Aroostook T15 R11 https://www.worldwaterfalldatabase.com/waterfall/Allagash-Falls-20408 Allagash Stream Little Allagash Falls Aroostook Eagle Lake Twp http://bangordailynews.com/2012/04/04/outdoors/shorter-allagash-adventures-worthwhile Austin Stream Austin Falls Somerset Moscow Twp http://www.newenglandwaterfalls.com/me-austinstreamfalls.html Bagaduce River Bagaduce Reversing Falls Hancock Brooksville https://www.worldwaterfalldatabase.com/waterfall/Bagaduce-Falls-20606 Mother Walker Falls Gorge Grafton Screw Auger Falls Gorge Grafton Bear River Moose Cave Gorge Oxford Grafton http://www.newenglandwaterfalls.com/me-screwaugerfalls-grafton.html Big Wilson Stream Big Wilson Falls Piscataquis Elliotsville Twp http://www.newenglandwaterfalls.com/me-bigwilsonfalls.html Big Wilson Stream Early Landing Falls Piscataquis Willimantic https://tinyurl.com/y7rlnap6 Big Wilson Stream Tobey Falls Piscataquis Willimantic http://www.newenglandwaterfalls.com/me-tobeyfalls.html Piscataquis River Black Stream Black Stream Esker Piscataquis to Branns Mill Pond very hard to discerne best guess location Carrabasset River North Anson Gorge Somerset Anson https://www.mindat.org/loc-239310.html Cascade Stream -
East/South Landfill Gas Project – a Revenue Generator
East/South Landfill Gas Project – A Revenue Generator Mike Watt, Exec VP • [email protected] • (905) 321-3292 Walker Environmental Group A Division of Walker Industries Walker Environmental Group Organics Recycling and Disposal •Composting •Environmental Projects •Biosolids Management •Residential Drop-off •Renewable Energy •IC&I Waste Haulage •Grease Trap, Organics and •Waste Transfer Used Cooking Oil Collection •Landfill Disposal (2) •Soil Disposal and Remediation Technical Services •Environmental Projects •Carbon Neutral Buildings •Carbon Services Biosolids Drop-off Admin Offices Compost East Landfill Landfill Gas Plant South Landfill What is Landfill Gas? • 50% Methane • 50% CO2 • Trace gases and particulate, especially Oxygen and Nitrogen • Half heating value of natural gas LFG Utilization Across Canada (IGRS) Ontario: – Ottawa – Niagara – Essex – Moose Creek – Mississauga Outside Ontario: – Brandon, MB – Winnipeg, MB Niagara Falls, ON Landfill Gas Utilization South/East Landfill - Opportunities The System East Landfill • 3565 m header pipe • 112 well heads Current South Landfill • 1382 m header pipe • 35 well heads WEG Landfill Gas Curve - 20 Year Projection 10,000 9,000 8,000 7,000 6,000 LFG Curve 5,000 ELF Curve SLF Curve 4,000 Project Usage WEG Landfill Gas Supply (scfm) Supply Gas Landfill WEG 3,000 2,000 1,000 0 Energy Production • 1 MW FIT contract • 12 cents/kw +/- • 350 CFM +/- • Siloxane treatment • With pre-existing infrastructure and investment – Generates positive revenue Pipeline to Resolute • Two pipelines • 2000 CFM +/- • Displaces 60% + of NG needs($2-$3m/yr sales) • 100% recycled paper mill • Intermittent production (Newsprint market) ERC Credits • 3M tonnes traded since 2007 • East only (not required by regulation) – Eliminated in 2016 by regulation. -
Doing Niagara Falls If You're Stuck on the American Side
Meiqianbao/ Shutterstock Doing Niagara Falls If You're Stuck on the American Side By Jason Cochran The legendary Niagara Falls, one of the greatest natural attractions in North America, straddles the border between Ontario, Canada, and New York State. In an ideal tourism situation, you'd be able to drive or stroll across the Rainbow International Bridge to enjoy the view from both banks of the Niagara River. But sometimes you just can't get over the border. Maybe you don't have enough time. Maybe your legal status won't allow it. Or maybe you happen to be living through a once-in-a-lifetime global pandemic that has sealed national borders. It's all good! If you're restricted to the U.S. side, you won't find yourself over a barrel. There's plenty to do. In fact, some of the best activities in the Niagara Falls area are on the American side. Pictured above: Terrapin Point, at right, juts into the eastern side of the Falls from Niagara Falls State Park in New York State. Niagara Falls State Park Niagara Falls State Park If we're being honest, the Canadian side has richer options for quality lodging and tourist amenities, although the stuff on that riverbank tends toward cheesy honky-tonk. New York's territory beside the Falls, on the other hand, has been preserved from development since the 1880s. In fact, the area is now the oldest state park in the United States. The more-than-400-acre Niagara Falls State Park, which is separated from the core of town by a breakaway river, is speckled with whitewater-spanning bridges, river islands, curving walkways, and native animals. -
Michigan Academy of Science, Arts and Letters Volume
MICHIGAN ACADEMY OF SCIENCE, ARTS AND PAPERS OF THE MICHIGAN ACADEMY OF LETTERS SCIENCE ARTS AND LETTERS EDITORS VOLUME XII EUGENE S. MCCARTNEY UNIVERSITY OF MICHIGAN CONTAINING PAPERS SUBMITTED AT THE ANNUAL MEETING IN 1929 PETER OKKELBERG UNIVERSITY OF MICHIGAN (The papers in Botany and Zoölogy of the 1929 meeting appear in Volume XI.) UNIVERSITY OF MICHIGAN he annual volume of Papers of the Michigan 1930 T Academy of Science, Arts and Letters is issued All rights reserved under the joint direction of the Council of the Academy and of the Executive Board of the Graduate School of Copyright, 1930, BY GRADUATE SCHOOL, UNIVERSITY OF MICHIGAN the University of Michigan. The editor for the Academy EDITOR, EUGENE S. MCCARTNEY is Peter Okkelberg; for the University, Eugene S. Set up and printed, McCartney. February, 1930 Published, March, 1930 Previous publications of The Michigan Academy of PRINTED IN THE UNITED STATES OF AMERICA Science now known as The Michigan Academy of BY THE PLIMPTON PRESS · NORWOOD · MASS. Science, Arts and Letters, were issued under the title, Annual Report of the Michigan Academy of Science. Twenty-two volumes were published, of which those OFFICERS FOR 1929 numbered 1, 21 and 22 are out of print. Copies of the other volumes are still available for distribution and will President be sent on exchange so long as the editions last. W. H. WORREL Applications for copies should be addressed to the University of Michigan Librarian of the University of Michigan. Vice-President L. A. KENOYER Annual Reports embracing the proceedings of the Western State Normal College Academy will however, continue to be published. -
Waterfalls: Forms, Distribution, Processes and Rates of Recession
QUAESTIONES GEOGRAPHICAE 39(1) • 2020 WATERFALLS: FORMS, DISTRIBUTION, PROCESSES AND RATES OF RECESSION ANDREW S. GOUDIE School of Geography, Centre for the Environment, University of Oxford, Oxford, United Kingdom Manuscript received: December 15, 2019 Revised version: February 2, 2020 GOUDIE A. S., 2020. Waterfalls: forms, distribution, processes and rates of recession. Quaestiones Geographicae 39(1), Bo- gucki Wydawnictwo Naukowe, Poznań, pp. 59–77. 8 figs, 3 tables. ABSTRACT: A waterfall is a very steep (commonly nearly vertical) fall of some magnitude in a river course. Waterfalls are widespread fluvial landforms that have been described from many parts of the world. Thirty-eight World Heritage Properties include waterfalls in their designation. In addition, some waterfalls are actual or potential geomorphosites. Waterfalls occur in almost all climatic environments, though they are particularly common in formerly glaciated areas. They occur on a huge diversity of rock types, although in general, they do not form persistent or large falls on soft or unconsolidated rocks. Waterfalls also occur in a wide range of geomorphological settings: glaciated areas, areas of ac- tive tectonism, areas of sea-cliff retreat and sea-level change, great escarpments on passive margins, basins with river capture, rifted and faulted areas and areas that have been subjected to megaflooding. Multiple processes account for waterfall retreat and varying rates of recession. Although the greatest interest has been in rates of waterfall recession, there are examples of waterfalls that prograde as a result of tufa deposition. KEY WORDS: waterfalls, caprock, knickpoints, plunge pools, tufa Corresponding author: Andrew Goudie, [email protected] Introduction distribution and rates of retreat. -
Downtown Neighborhood City of Niagara Falls: Phase I
Intensive Level Survey Historic Resources – Downtown Neighborhood City of Niagara Falls: Phase I 3.0 Historical Overview This section provides a narrative history of the City of Niagara Falls with specific emphasis on the Downtown neighborhood. The overview addresses significant trends and themes associated with the city’s historic context. The Downtown neighborhood’s period of significance is identified and examined in this chapter. Martin Wachadlo, architectural historian, conducted the background historic research. 3.1 Niagara County: Physiology and Geology Figure 3-1. Niagara Falls, Niagara Falls, New York Niagara County borders the southern shore of Lake Ontario in the extreme northwestern corner of New York State, and occupies part of the Huron and Ontario Plains. The Ontario Plain comprises part of Lake Ontario to the foot of the Niagara Escarpment1, and the Huron plain extends from the crest of the escarpment southward beyond the county line. The Niagara Escarpment begins in Watertown, New York, USA and extends westerly along the Manitoulin Island in the Province of Ontario, Canada. The escarpment continues through Wisconsin and Illinois. With geological material measuring 64-ft thick, the stratigraphy at Niagara Falls provides a glimpse into the overall rock types comprising the Niagara Escarpment (Figure 3-1). The top layer is Lockport Dolomite, a hard rock referred to as the "Lower Silurian Group." Below the top layer is Rochester Shale, which is much softer and wears away easily with the effects of erosion. Under the shale are harder strata of limestone and dolostone known as the "Clinton Group." Below the harder strata is Grimsby sandstone. -
September Gsat 03
GSA 2007 Annual Meeting Technical Program, p. 20 VOL. 17, No. 9 A PublicatioN Of the GeoloGical SoCiety Of AMeRica SePteMbeR 2007 Blue Nile incision on the Ethiopian Plateau: Pulsed plateau growth, Pliocene uplift, and hominin evolution Section Meetings Cordilleran and Rocky Mountain Joint Meeting, p. 49 Northeastern Section Meeting, p. 52 South-Central Section Meeting, p. 53 Penrose Conference Report, p. 55 Field Forum Report, p. 57 VoluMe 17, NuMbeR 9 SePteMbeR 2007 Cover: image (~40 × 20 km): 3-D perspective view (vertical exaggeration 5) of part of the Gorge of the Nile on the northwestern ethiopian Plateau (south of Mount Choke) generated by draping advanced spaceborne thermal emission and reflection radiometer (ASTER) image (7-3-1) over 15-m horizontal resolution ASTER digital elevation GSA TODAY publishes news and information for more than 20,000 GSA members and subscribing libraries. GSA Today model. trunk river (blue Nile) is flowing toward the lead science articles should present the results of exciting new viewer. Photo (~10 × 7 km): Section from the same research or summarize and synthesize important problems area, where the blue Nile deeply dissects Mesozoic or issues, and they must be understandable to all in the sandstones. See “blue Nile incision on the ethiopian earth science community. Submit manuscripts to science Plateau: Pulsed plateau growth, Pliocene uplift, and editors Stephen Johnston, [email protected], or David Fastovsky, hominin evolution,” by Gani et al., p. 4–11. [email protected]. GSA TODAY (ISSN 1052-5173 USPS 0456-530) is published 11 times per year, monthly, with a combined April/May issue, by SCIENCE ARTICLE The Geological Society of America, Inc., with offices at 3300 Penrose Place, Boulder, Colorado.