The United Counties of Leeds and Grenville is a county in Ontario, Canada, in the Eastern Ontario subregion of Southern Ontario. It fronts on the Saint Lawrence River and the international boundary between Canada and the United States. The county seat is Brockville. The county was formed by the union of the historical counties of Leeds and Grenville in 1850.
The Sudbury Basin, also known as Sudbury Structure or the Sudbury Nickel Irruptive, is a major geological structure in Ontario, Canada. It is the third-largest known impact crater or astrobleme on Earth, as well as one of the oldest. The crater formed 1.849 billion years ago in the Paleoproterozoic era.
Leeds County is a historic county in the Canadian province of Ontario. The county was first surveyed in 1792 as one of the nineteen counties created by Sir John Graves Simcoe in preparation for the United Empire Loyalists to settle here. The county took its name from Francis Osborne, 5th Duke of Leeds; the "Leeds" of the Dukedom referred to Leeds in West Yorkshire, England and not for Leeds, Kent, England. In 1850, Leeds County merged with Grenville County to create the United Counties of Leeds and Grenville. This county was home to several townships as well as the city of Brockville.
Leeds—Grenville—Thousand Islands and Rideau Lakes is a federal electoral district in Ontario, Canada, that has been represented in the House of Commons since 1979. Prior to the 2015 election, the riding was known as Leeds—Grenville.
Makkovik is a town in Labrador in eastern Canada. It had a population of 361 persons in 2011. The main industry is fishing and there is a fishing cooperative.
The Superior Craton or Superior Province is an Archean craton which forms the core of the Canadian Shield lying north of Lake Superior for which it is named.
The Barrier is a lava dam retaining the Garibaldi Lake system in southwestern British Columbia, Canada. It is over 300 m (980 ft) thick and about 2.4 km (1.5 mi) long where it impounds the lake.
Harrington is a township municipality in the Laurentides region of Quebec, Canada, part of the Argenteuil Regional County Municipality. It is located in the Laurentian Mountains, about 40 kilometres (25 mi) north-west of Lachute.
The geology of Saskatchewan can be divided into two main geological regions, the Precambrian Canadian Shield and the Phanerozoic Western Canadian Sedimentary Basin. Within the Precambrian shield exists the Athabasca sedimentary basin. Meteorite impacts have altered the natural geological formation processes. The prairies were most recently affected by glacial events in the Quaternary period.
The Labrador Trough or the New Quebec Orogen is a 1,600 km (994 mi) long and 160 km (99 mi) wide geologic belt in Canada, extending south-southeast from Ungava Bay through Quebec and Labrador.
This is a list of articles related to plate tectonics and tectonic plates.
The Grenville dike swarm is a large Proterozoic dike swarm in the Canadian provinces of Ontario and Quebec. It is one of the several major magmatic events in the Canadian Shield and it possibly formed 590 million years ago along a triple junction that might have been related to a mantle plume. The maximum length of the Grenville dike swarm is 700 km (435 mi).
The Big Dan Shear Zone is a north-south trending shear zone in Northeastern Ontario, Canada, located in the municipality of Temagami.
The geology of North America is a subject of regional geology and covers the North American continent, third-largest in the world. Geologic units and processes are investigated on a large scale to reach a synthesized picture of the geological development of the continent.
The Aswa Dislocation, also called the Aswa mylonite belt, Aswa Lineament or Aswa Shear Zone is a north-west trending ductile shear zone that runs to the east of Lake Victoria in East Africa.
The Hottah terrane is a Paleoproterozoic terrane in the northwestern end of the Canadian Shield which is exposed near Hottah Lake, Northwest Territories. It is a belt of multi-deformed metasedimentary and metavolcanic rocks intruded by a series of diorite to granite plutons. Forming the western part of the Wopmay orogenic system, the 1.9 Ga Hottah terrane is separated from the Archean rocks of the orogen by the north-trending Wopmay fault zone and overprinted by the 1.875-1.85 Ga Great Bear magmatism.
The Grenville Province is a tectonically complex region, in Eastern Canada, that contains many different aged accreted terranes from various origins. It exists southeast of the Grenville Front and extends from Labrador southwestern to Lake Huron. It is bounded by the St. Lawrence River/Seaway to the southeast.
The geology of Newfoundland and Labrador includes basement rocks formed as part of the Grenville Province in the west and Labrador and the Avalonian microcontinent in the east. Extensive tectonic changes, metamorphism and volcanic activity have formed the region throughout Earth history.
