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River in Ontario, Canada
The Eramosa River is a river in Wellington County in southwestern Ontario which rises near Erin, Ontario, and flows southwest through the city of Guelph
Eramosa_River
Urban walking trail in Guelph, Ontario, Canada
The Eramosa River Trail is a 4.1 km (2.5 mi) urban walking trail that runs alongside the Eramosa River in Guelph, Ontario, Canada, stretching from the
Eramosa_River_Trail
Township in Ontario, Canada
Guelph/Eramosa (/ˈɡwɛlfˈɛrəˈmɒsə/) is a township located in Wellington County, in midwestern Ontario, Canada. It partly encircles the city of Guelph,
Guelph/Eramosa
River in Ontario, Canada
north of Waterloo. The Eramosa River joins the Speed River in Guelph. The Speed River joins the Grand in Cambridge. The Nith River joins the Grand in Paris
Grand_River_(Ontario)
Protected area in Ontario, Canada
the city of Guelph, this conservation area is on both sides of the Eramosa River and is a central location within Southern Ontario. The nearby Highway
Rockwood_Conservation_Area
Unincorporated community in Ontario, Canada
unincorporated community in the Township of Guelph/Eramosa, Wellington County, Ontario, Canada. Located on the Eramosa River, the Eden Mills Writers' Festival is an
Eden_Mills,_Ontario
River in Canada
where it is joined by the Eramosa River, then through the towns of Hespeler and Preston, finally uniting with the Grand River in north-west Cambridge.
Speed_River
Depression formed by glaciers or floodwaters
sediment, or vegetation. If the kettle is fed by surface or underground rivers or streams, it becomes a kettle lake. If the kettle receives its water from
Kettle_(landform)
City in Ontario, Canada
of the Speed River and the Eramosa River, which have numerous tributaries. The Speed River enters from the north and the Eramosa River from the east;
Guelph
Warmer periods within an ice age
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Interglacial
Long, winding ridge of stratified sand and gravel associated with former glaciers
the River Tweed valley. Great Esker Park, containing one of the highest eskers in North America at 27 m (90 ft), runs along the Weymouth Back River in
Esker
Geographic and geologic area of North America
Northern Peninsula of Newfoundland, most of Quebec north of the St. Lawrence River, much of Ontario including northern sections of the Ontario Peninsula, the
Canadian_Shield
Time period c. 12,900–11,700 years ago
Ocean. While there is evidence of meltwater travelling via the Mackenzie River, this hypothesis may not be consistent with the lack of sea level rise during
Younger_Dryas
Piece of rock that has been moved by a glacier
narrow belt for about 600 kilometres (370 mi) from Alberta's Athabasca River Valley to the southwest of the province. White Rock, British Columbia gets
Glacial_erratic
Geological region in the Midwestern US
is called the Blufflands, due to the steep bluffs and cliffs around the river valleys. The western half is known as the Rochester Plateau, which is flatter
Driftless_Area
Large lake in central North America at the end of the last glacial period
through the Traverse Gap into Glacial River Warren (parent to the Minnesota River, a tributary of the Mississippi River), east through Lake Kelvin (modern
Lake_Agassiz
Fjord in Norway
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Hardangerfjord
Rise of land masses after glacial period
the Uimaharju esker at the southwestern end of the lake, creating a new river (Pielisjoki) that runs to the sea via Lake Pyhäselkä to Lake Saimaa. The
Post-glacial_rebound
Glacial stage
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Kansan_glaciation
Period of major glaciations of the Northern Hemisphere (115,000–11,700 years ago)
of the glaciation, as is the course of the Ohio River, which largely supplanted the prior Teays River.[citation needed] With the assistance of several
Last_Glacial_Period
Type of sediment deposition by a melting glacier
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Outwash_fan
Annual writing festival in Eden Mills, Ontario, Canada
a children's site, and musical events. Eden Mills is located on the Eramosa River and the festival's principal readings take place on its banks. In 1989
Eden_Mills_Writers'_Festival
Climatic cooling after the Medieval Warm Period (16th–19th centuries)
River Thames frost fair was in 1608 and the last in 1814. Changes to the bridges and the addition of the Thames Embankment have affected the river's flow
Little_Ice_Age
This is the list of rivers which are in and flow through Ontario. The watershed list includes tributaries as well. Dee River, flows between Three Mile
List_of_rivers_of_Ontario
Continental glacier in North America during the last ice age
Louis, Missouri, and then followed the present course of the Missouri River up to the northern slopes of the Cypress Hills, beyond which it merged with
Laurentide_ice_sheet
Stratigraphic unit of the Lockport Formation
the bituminous dolomites exposed below the Guelph Formation along the Eramosa River, northeast of Guelph, Ontario. No detailed description of the type section
Eramosa_Member
Post glacial seaway in eastern North America
Lake Champlain, Lake of Two Mountains on the lower Ottawa River, and the lower Saguenay River, as well as other lakes, islands and shores. The mass of
Champlain_Sea
Glacial erratic in Alberta, Canada
quartzite, which occurs only within the Gog Group and is found in the Athabasca River Valley of central western Alberta. Big Rock is the largest erratic within
Okotoks_Erratic
Name list
Canajoharie, New York Arkell Spring Grounds, bedrock aquifer along the Eramosa River in Ontario, Canada Arkell's Brewery, privately held English brewery
Arkell
Circa 24,000–16,000 BCE; most recent era when ice sheets were at their greatest extent
develop during the LGM, in particular in south-facing slopes. In the Hex River Mountains, in the Western Cape, block streams and terraces found near the
Last_Glacial_Maximum
Period of long-term reduction in temperature of Earth's surface and atmosphere
meltwaters. The old Teays River drainage system was radically altered and largely reshaped into the Ohio River drainage system. Other rivers were dammed and diverted
Ice_age
Abrupt climatic cooling event during the last glacial retreat
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Oldest_Dryas
Glaciation in North America during the Last Glacial Period
America. This glaciation radically altered the geography north of the Ohio River, creating the Great Lakes. At the height of the Wisconsin Episode glaciation
Wisconsin_glaciation
Provincial park in Ontario, Canada
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Lion's_Head_Provincial_Park
Glacial age that occurred before the Last Glacial Period
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Penultimate_Glacial_Period
Mound formed on a retreating glacier and deposited on land
undisturbed kame features. They are Minnitaki Kames Provincial Park and Bonheur River Kame Provincial Park. Drumlin Esker Glacial Kame culture Glacial landforms
Kame
Moraine in the midwestern United States
Creek into the sluiceway of the Kankakee River. An additional release may have been in the vicinity of the Deep River – Stoney Run divide east of Crown Point
Tinley_Moraine
Type of moraine that forms at the terminal of a glacier
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Terminal_moraine
Former lake in North America
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Lake_Stanley
Massif in Switzerland and Italy
perpendicular to the main watershed between Switzerland and Italy (the river basins of the Rhône and the Po on the Swiss and Italian side, respectively)
Monte_Rosa
First epoch of the Quaternary Period
2018). "Viable Nematodes from Late Pleistocene Permafrost of the Kolyma River Lowland". Doklady Biological Sciences. 480 (1): 100–102. doi:10.1134/S0012496618030079
Pleistocene
Lake formed by the action of ice
a confluence where the other branch carries an unfrozen river. The glacier blocks the river, which backs up into a proglacial lake, which eventually
Proglacial_lake
Interglacial period which began 130,000 years ago
by Pieter Harting (1875). He named the beds "Système Eémien", after the river Eem on which Amersfoort is located. Harting noticed the marine molluscan
Last_Interglacial
Periods of colder and warmer climate during the Quaternary period
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Stadial_and_interstadial
Provincial park of Ontario, Canada
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Arrowhead_Provincial_Park
Glacial melt water landform
Upon entering a proglacial lake at the end (terminus) of a glacier, the river/stream deposit these sediments. This landform can be observed after the
Kame_delta
Major ice sheet
may have extended into the northeast extremity of Oregon and the Salmon River Mountains in Idaho. It is probable, though, that its northern margin also
Cordilleran_ice_sheet
State Natural Area in Wisconsin
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Two Creeks Buried Forest State Natural Area
Two_Creeks_Buried_Forest_State_Natural_Area
Early and middle Pleistocene glacial and interglacial periods in North America
1029/2004PA001071 McKay, E.D. (2007). "Six Rivers, Five Glaciers, and an Outburst Flood: the Considerable Legacy of the Illinois River". Proceedings of the 2007 Governor's
Pre-Illinoian
Plain of glacial till
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Till_plain
Glacial till landform above Lake Ontario, Canada
southern Ontario, the moraine gets its name from the rolling hills and river valleys extending 160 km (99 mi) east from the Niagara Escarpment to Rice
Oak_Ridges_Moraine
Natural spring and water source in Ontario
groundwater seeps where the Arkell Spring feeds into the Eramosa River. A 1982 report by the Grand River Implementation Committee determined that the recharge
Arkell_Spring_Grounds
Provincial park in British Columbia
Prince George. The park protects an area of the 40-kilometre (25 mi) Stuart River Eskers Complex. Eskers are winding ridges of gravel formed by glaciers which
Eskers_Provincial_Park
Long-distance hiking trail in the United States
western end of the trail is at Interstate State Park along the St. Croix River, which is the border between northwestern Wisconsin and eastern Minnesota
Ice_Age_Trail
Prehistoric lake in Wisconsin, United States
United States. Before the last glacier, a somewhat different Wisconsin River drained the north-central part of the state, running around the east end
Glacial_Lake_Wisconsin
United States National Natural Landmark in Douglas County, Washington
lies in the northwest corner of the Columbia River Plateau. The plateau is formed on top of the Columbia River Basalt Group a large igneous province that
Withrow Moraine and Jameson Lake Drumlin Field
Withrow_Moraine_and_Jameson_Lake_Drumlin_Field
Hills in Alberta and Saskatchewan, Canada
separates rivers that drain south to the Gulf of Mexico via the Missouri River system from those that drain to northeast to Hudson Bay via the Nelson River system
Cypress_Hills_(Canada)
Vast body of ice in Greenland, Northern Hemisphere
equivalent to 0.7% of freshwater entering the oceans from all of the world's rivers. This meltwater is not pure, and contains a range of elements - most notably
Greenland_ice_sheet
Prehistoric lake from the Wisconsin Glacial Period
by retreating glaciers, it drained southwest through the Chicago Outlet River. The city of Chicago lies in a broad plain that, hundreds of millions of
Lake_Chicago
Depositional forms in channeled scablands
the flood (e.g., depth and speed). Columbia Plateau Altai Mountains Alsek River Giant current ripples are an important feature of the Channeled Scablands
Giant_current_ripples
Last interglacial stage in the North American regional subdivision of the Quaternary
of the Glasford Formation, which fill an ancient and buried Mississippi River valley in north-central Illinois. The age of fluvial sediments overlying
Sangamonian
Topics referred to by the same term
Interest in Stoney Creek, Ontario Eramosa marble, a building stone obtained from the Eramosa Eramosa River, a river in Wellington County, Ontario This
Eramosa_(disambiguation)
Moraine in the midwestern United States
till and sand. The Valparaiso Moraine defines part of the St. Lawrence River Divide, bounding the Great Lakes Basin. It begins near the border of Wisconsin
Valparaiso_Moraine
Glacial lake in Vermont, New York and Ontario
drained into Glacial Lake Candona, a geologic predecessor of the St. Lawrence River. At one time, Lake Vermont may have reached nearly as far south as to what
Lake_Vermont
Group of glacial erratic rocks in Canada
Structural Geology of the Foothills Between Savanna Creek and Panther River, S.W. Alberta, Canada : guidebook. Calgary, Alberta, Canada: Canadian Society
Foothills_Erratics_Train
Deposits created by outbursts of Pleistocene glacier-dammed lakes
deposits of sediments that could not be explained by the historic action of rivers and seas. Diluvium was initially argued to have been deposited by the action
Diluvium
Ancient shoreline of Lake Michigan
reside. Then it began to drop. It appears that the outlet to the Illinois River, was cutting downward, keeping pace with the lowering lake. At around 620
Calumet_Shoreline
Lake in the United States
formed 14,000 years before present (YBP) in the valley of the Kankakee River. It developed from the outwash of the Michigan Lobe, Saginaw Lobe, and the
Lake_Kankakee
California. St. Lawrence River drainage, i.e., the Great Lakes Champlain Sea; 11,800 – 8,200 YBP on the lower St. Lawrence, from Ottawa River to the Gulf of St
List_of_prehistoric_lakes
Prehistoric proglacial lake
reaching the Mattawa River, which joined the Ottawa River at Mattawa, which led out the St. Lawrence to the ocean. Mattawa River is a chain of lakes.
Nipissing_Great_Lakes
National State Wildlife Area, Dodge and Fond du Lac counties, Wisconsin
waters from the melting glacier and forming Glacial Lake Horicon. The Rock River slowly eroded the moraine, and the lake drained. As the levels of silt,
Horicon_Marsh
State Park in Sauk County, Wisconsin
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Devil's Lake State Park (Wisconsin)
Devil's_Lake_State_Park_(Wisconsin)
Conservation authority in Ontario, Canada
2857139°W / 43.3759000; -80.2857139 (Grand River Conservation Authority Head Office) The Grand River Conservation Authority (GRCA) is a conservation
Grand River Conservation Authority
Grand_River_Conservation_Authority
United States historic place
named Interstate State Park. They straddle the Dalles of the St. Croix River, a deep basalt gorge with glacial potholes and other rock formations. The
Interstate_Park
winter. The Wendat peoples settled into Southern Ontario along the Eramosa River around 8,000–7,000 BCE (10,000–9,000 years ago). They were concentrated
Indigenous_peoples_in_Canada
Multi-unit protected area in Wisconsin, USA
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Ice Age National Scientific Reserve
Ice_Age_National_Scientific_Reserve
Territorial park in Nunavut
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Ovayok_Territorial_Park
Geological period in North America in the Quaternary
704257. McKay, E.D., 2007, Six Rivers, Five Glaciers, and an Outburst Flood: the Considerable Legacy of the Illinois River. Proceedings of the 2007 Governor's
Illinoian_(stage)
Former lake in North America
The lake drained through three outlets, the Chicago Outlet River, the St. Clair-Detroit River, and through the Trent Valley. The first stage occupied only
Lake_Algonquin
Geological period of the Earth
were thickets of dwarf birch, willow, sea buckthorn, and juniper. In the river valleys and uplands, to the south, were open birch forests. The first trees
Older_Dryas
Canadian poet
with numerous publications to her credit. She lives and writes in the Eramosa River valley near Guelph, Ontario, and also works as an editor, independent
Katherine_L._Gordon
Obsolete geologic period of the early Quaternary of North America
183-196. McKay, E.D., 2007, Six Rivers, Five Glaciers, and an Outburst Flood: the Considerable Legacy of the Illinois River. Proceedings of the 2007 Governor's
Yarmouthian_(stage)
redeposited as drift or till. Much of this drift was dumped into old preglacial river valleys, while some of it was heaped into belts of hills (terminal moraines)
Glacial_history_of_Minnesota
Railway operator in Toronto, Canada
once located include the walking trails along the south bank of the Eramosa River, the Smith Property loop in Puslinch and the Halton County Radial Railway
Toronto_Suburban_Railway
Drainage basin of Lake Erie in North America
southern Ontario at 2,600 sq mi (7,000 km2) Grand River Conestogo River Eramosa River Nith River Speed River Nanticoke Creek (Ontario) Big Creek Big Otter
Lake_Erie_Basin
Network of routes connecting natural sites
2,000 ft (610 m)-high ice dam that blocked the mouth of the Clark Fork River, creating glacial Lake Missoula, which impounded greater than 2,000 km3
Ice Age Floods National Geologic Trail
Ice_Age_Floods_National_Geologic_Trail
Moraine bordering Lake Michigan
(400 m). These continue south to Baldwin. The ridges south of Muskegon River are just under 800 feet (240 m). The steep declines become more gradual
Lake_Border_Moraine
North American ice age, 9,000–16,000 BCE
advanced out of the mountains of British Columbia following the Fraser River and Fraser Valley. The Vashon Glaciation is an extension of the Fraser Glaciation
Vashon_Glaciation
between the Speed River and Victoria Road, and north of the Eramosa River. Ward 3 (St John's) is west and north of the Speed River, and east of the Hanlon
Guelph_City_Council
Park) Barber Memorial Scout Camp (in Guelph, Ontario adjacent to the Eramosa River) Camp BEL (in Dorchester, Ontario east of London, Ontario) The Bryson
Scouting and Guiding in Ontario
Scouting_and_Guiding_in_Ontario
Township in Ontario, Canada
the village, or the Arkell Springs trail which stretches along the Eramosa River from Watson Rd. Just north of Arkell, east to nearby Eden Mills near
Puslinch,_Ontario
Unincorporated community in Ontario, Canada
and the Townships of Nichol, Pilkington, West Garafraxa, and part of Eramosa. The first settlers to this area were freed slaves, who formed what was
Fergus,_Ontario
Moraine in Indiana
It is on the north side of the Wabash River as far as Logansport, continuing along the north side of the Eel River. In Miami and Wabash Counties the moraine
Packerton_Moraine
List of county roads
27-29 in former Eramosa Township (now a part of Guelph-Eramosa); and 30-41 in former Guelph Township (also now a part of Guelph-Eramosa) and Puslinch,
List of numbered roads in Wellington County
List_of_numbered_roads_in_Wellington_County
State park in Chippewa County, Wisconsin
Rock (glacial erratic), Alberta Cypress Hills (Canada), Saskatchewan Eramosa River, Ontario Eskers Provincial Park, British Columbia Foothills Erratics
Chippewa Moraine State Recreation Area
Chippewa_Moraine_State_Recreation_Area
Arboretum in Guelph, Ontario, Canada
54083; -80.21500, in close proximity to the confluence of the Speed and Eramosa rivers, and less than a kilometre from Hanlon Creek. The area's geology features
University of Guelph Arboretum
University_of_Guelph_Arboretum
Limestone containing fossils
Biostratigraphy Blue Lias Carnian Chalk Group Ediacara biota Elk Point Group Eramosa Galena Group Hirnantian La Tour-Blanche Anticline Mannville Group Madison
Fossiliferous_limestone
Geologic group in Eastern and Midwestern, USA
The Black River Group is a geologic group that covers three sedimentary basins in the Eastern and Midwestern United States. These include the Appalachian
Black_River_Group
Unincorporated community in Ontario, Canada
Nichol, Pilkington, and West Garafraxa (along with the northwestern part of Eramosa.) The decision — along with the Ontario government’s role therein — remains
Elora,_Ontario
Lake in Ontario, Canada
Guelph Lake is a man-made reservoir on the Speed River, in the Township of Guelph/Eramosa. It is located upriver and slightly northeast of the city of
Guelph_Lake
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