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Fonthill Kame
The Fonthill Kame is a geological feature in the Niagara Peninsula in Pelham, Ontario, Pelham, Ontario, Canada. A ''kame'' is a moraine in the form of a large, isolated hill. It is composed of sand and gravel deposited by the retreating glaciers of the last ice age. The Fonthill Kame rises about above the surrounding land (290 m above sea level) and is the highest elevation in the region. Some sources say that the kame is no longer the highest point owing to the removal of sand and gravel. Despite what some sources may say, the kame is simply the highest natural geographic feature in Niagara and the highest point would remain on the kame. There is some debate about the actual highest point though because locals seem to remember a plaque in a farmers field, south of Tice Road and East on Effingham Road, on un-excavated land that marked the highest point. The kame is east to west and north to south. It slopes gradually on the west side, more steeply on the south and east and m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Niagara Peninsula
The Niagara Peninsula is an area of land lying between the southwestern shore of Lake Ontario and the northeastern shore of Lake Erie, in Ontario, Canada. Technically an isthmus rather than a peninsula, it stretches from the Niagara River in the east to Hamilton, Ontario, in the west. The peninsula is located in the Golden Horseshoe region of Southern Ontario, and has a population of roughly 1,000,000 residents. The region directly across the Niagara River and Lake Erie in New York State is known as the Niagara Frontier. Government The greater part of the peninsula is incorporated as the Regional Municipality of Niagara. Cities in the region include St. Catharines, Niagara Falls, Thorold, Port Colborne and Welland. Towns include Niagara-on-the-Lake, Lincoln, Pelham, Grimsby and Fort Erie, as well as the townships Wainfleet and West Lincoln. The remainder of the peninsula encompasses parts of the City of Hamilton and Haldimand County. History The area was originally inhabite ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Short Hills Provincial Park
Short Hills Provincial Park is a provincial park located in the centre of the Niagara Peninsula, bordering the city of St. Catharines and the town of Pelham in the Niagara Region in southern Ontario, Canada. It occupies an area of . It also borders the new vineyard sub-appellation called the Short Hills Bench. Located on the southern edge of the Niagara Escarpment, the park is a jumble of small but steep hills ("short hills") and valleys created by the last ice age. The effect was only compounded when the Twelve Mile Creek cut through the sedimentary deposits and glacial till. Wildlife inhabiting the park include white-tailed deer, coyote, and meadow vole. Being at the north end of the Carolinian zone, many plants grow here that do not grow or are rarely found in other parts of Canada, including pawpaw, sweet chestnut and tulip-tree. The only park of its scale in Niagara, Short Hills Provincial Park is a prime destination for residents of nearby cities, especially St ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of The Regional Municipality Of Niagara
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fonthill, Ontario
Fonthill is a community in the town of Pelham, Ontario, Canada. It has a few small industries, but is primarily a residential suburb known for its fruit orchards, nature trails, and neighbourly attitude. As a bedroom community, most residents commute to Welland, St. Catharines and some as far as Buffalo, Hamilton and Toronto daily for work. Geography and geology Fonthill shares its name with the Fonthill Kame, on which it is located, formed by glacial deposits. Effingham Creek, a cold-water stream, originates in the glacial silts and sands of Short Hills area of the moraine, northwest of Fonthill. Effingham Creek is a tributary to Twelve-Mile Creek, which empties into Lake Ontario.Short Hills Nature Sanctuary . Accessed 2012-11-28. For more about the geology of the town, see [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ministry Of The Environment (Ontario)
The Ministry of the Environment, Conservation and Parks is an Ontario government ministry responsible for protecting and improving the quality of the environment in the Canadian province of Ontario, as well as coordinating Ontario's actions on climate change. This includes administration of government programs, such as Ontario's Drive Clean and Clean Water Act. The ministry headquarters are located inside the Ontario Government Buildings. History The Ministry of the Environment was originally established as a portfolio in the Executive Council of Ontario (or provincial cabinet) in 1972. The ministry was merged with the Ministry of Energy to form the Ministry of Environment and Energy from 1993 to 1997, and briefly again in 2002, before being split back up again. Following the 2014 Ontario election, the addition of climate change to the ministry's portfolio was announced on June 24, 2014, and its name changed from the Ministry of the Environment to the Ministry of the E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hydrogeology
Hydrogeology (''hydro-'' meaning water, and ''-geology'' meaning the study of the Earth) is the area of geology that deals with the distribution and movement of groundwater in the soil and rocks of the Earth's crust (commonly in aquifers). The terms groundwater hydrology, geohydrology, and hydrogeology are often used interchangeably. Hydrogeology is the study of the laws governing the movement of subterranean water, the mechanical, chemical, and thermal interaction of this water with the porous solid, and the transport of energy, chemical constituents, and particulate matter by flow (Domenico and Schwartz, 1998). Groundwater engineering, another name for hydrogeology, is a branch of engineering which is concerned with groundwater movement and design of wells, pumps, and drains. The main concerns in groundwater engineering include groundwater contamination, conservation of supplies, and water quality.Walton, William C. (November 1990). ''Principles of Groundwater Engin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vine
A vine (Latin ''vīnea'' "grapevine", "vineyard", from ''vīnum'' "wine") is any plant with a growth habit of trailing or scandent (that is, climbing) stems, lianas or runners. The word ''vine'' can also refer to such stems or runners themselves, for instance, when used in wicker work.Jackson; Benjamin; Daydon (1928). ''A Glossary of Botanic Terms with their Derivation and Accent'', 4th ed. London: Gerald Duckworth & Co. In parts of the world, including the British Isles, the term "vine" usually applies exclusively to grapevines (''Vitis''), while the term "climber" is used for all climbing plants. Growth forms Certain plants always grow as vines, while a few grow as vines only part of the time. For instance, poison ivy and bittersweet can grow as low shrubs when support is not available, but will become vines when support is available. A vine displays a growth form based on very long stems. This has two purposes. A vine may use rock exposures, other plants, or other ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Niagara Escarpment
The Niagara Escarpment is a long escarpment, or cuesta, in Canada and the United States that runs predominantly east–west from New York through Ontario, Michigan, Wisconsin, and into Illinois. The escarpment is most famous as the cliff over which the Niagara River plunges at Niagara Falls, for which it is named. The escarpment is a UNESCO World Biosphere Reserve. The reserve has the oldest forest ecosystem and trees in eastern North America. The escarpment is not a fault line but the result of unequal erosion. It is composed of an outcrop belt of the Lockport Formation of Silurian age, and is similar to the Onondaga Formation, which runs in a parallel outcrop belt just to the south, through western New York and southern Ontario. The escarpment is the most prominent of several escarpments formed in the bedrock of the Great Lakes Basin. From its easternmost point near Watertown, New York, the escarpment shapes in part the individual basins and landforms of Lake Ontario, Lak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pelham, Ontario
The Town of Pelham (2016 population 17,110) is located in the centre of Niagara Region in Ontario, Canada. The town's southern boundary is formed by the Welland River, a meandering waterway that flows into the Niagara River. To the west is the township of West Lincoln, to the east the city of Welland and the city of Thorold, and to the north the city of St. Catharines and the town of Lincoln. North Pelham contains the picturesque Short Hills (see attractions). Two important creeks have their headwaters within Pelham; Coyle Creek, which flows south into the Welland River, and Twelve Mile creek, a spring-fed stream that flows north into Lake Ontario. History Pelham Township was part of the original Welland County since the late 1780s. The Town of Pelham (est. 1970) derives its name from Pelham Township, which John Graves Simcoe named in the 1790s. In the beginning, the townships were only numbered and not named. The policy of Simcoe was to adopt township names from England. Pel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gravel
Gravel is a loose aggregation of rock fragments. Gravel occurs naturally throughout the world as a result of sedimentary and erosive geologic processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb). Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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