Kazabazua, Quebec
| Kazabazua | |
|---|---|
| Municipality | |
 |
|
| Nickname(s): Kaz, Kazu | |
 Kazabazua
|
|
| Coordinates: 45°57′N 76°01′W / 45.950°N 76.017°WCoordinates: 45°57′N 76°01′W / 45.950°N 76.017°W | |
| Country |
 Canada
|
| Province |
 Quebec
|
| Region | Outaouais |
| RCM | La Vallée-de-la-Gatineau |
| Settled | 1835 |
| Constituted | January 1, 1862 |
| Government | |
| • Mayor | Ota Hora |
| • Federal riding | Pontiac |
| • Prov. riding | Gatineau |
| Area | |
| • Total | 182.00 km2 (70.27 sq mi) |
| • Land | 174.66 km2 (67.44 sq mi) |
| Population (2011) | |
| • Total | 847 |
| • Density | 4.8/km2 (12/sq mi) |
| • Pop (2006–11) |
 1.0% |
| • Dwellings | 791 |
| Time zone | EST (UTC−5) |
| • Summer (DST) | EDT (UTC−4) |
| Postal code(s) | J0X 1X0 |
| Area code(s) | 819 |
| Access Routes |
 Route 105 Route 301
|
| Website | www |
Kazabazua is a village and municipality in La Vallée-de-la-Gatineau Regional County Municipality, Quebec, Canada. The village is about halfway between Maniwaki and Hull at the intersection of Route 105 and Route 301, just west of the Gatineau River.
The village and municipality are named after the Kazabazua River which passes through it. Like many other Amerindian names, Kazabazua has had many spellings, such as Kazaluzu, Kasubasua, Cazabasua, Cazibazouis, Cazebalzuac, Cajibajouis. This word comes from the Algonquin word kachibadjiwan, from kach ("hidden") and djiwan ("current"), hence it means "underground river". This name is a reflection of the local topography because the Kazabazua River disappears underground and resurfaces a few dozen metres downstream. The river then flows through rapids and passes under a natural stone bridge.
The communities of Kazabazua Station, Aylwin, and Aylwin Station are also located within the municipality.
The bedrock of the region Kazabazua is composed predominantly of marble dating from the Precambrian Era and represent metamorphic sedimentary rocks from the Grenville orogeny.
At the Kazabazua River, marble is calcitic and contains crystals of graphite and grossular garnet. The marble has been chemically and mechanically eroded by water from the river to form a karst stone bridge. The inclusion of gneiss in the marble illustrates erosion differential.
The Kazabazua Plain is a geomorphological phenomenon unique to Quebec. It is made up of metamorphic rocks which are covered with a network of ancient sand dunes and bogs within which many rare plant species and threatened species have been identified. The topography is the result of water and wind action since the withdrawal of the last glacier. After this withdrawal, the region was covered by the Champlain Sea, which left a layer of marine clay. When the sea level lowered, the area was submerged under a postglacial delta which deposited large volumes of sand.
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Wikipedia