*** Welcome to piglix ***

Kejimkujik National Park

Kejimkujik National Park
IUCN category II (national park)
Little River in Fall.jpg
Little River
Map showing the location of Kejimkujik National Park
Map showing the location of Kejimkujik National Park
Location of Kejimkujik National Park in Canada
Location Nova Scotia, Canada
Nearest city Halifax
Coordinates 44°23′57″N 65°13′06″W / 44.39917°N 65.21833°W / 44.39917; -65.21833Coordinates: 44°23′57″N 65°13′06″W / 44.39917°N 65.21833°W / 44.39917; -65.21833
Area 404 km2 (156 sq mi)
Established 1967
Visitors 36,090 (in 2015-16)
Governing body

Parks Canada

Official name Kejimkujik National Historic Site of Canada
Designated 1994

Parks Canada

Kejimkujik National Park (often called Keji for short) is part of the Canadian National Parks system, located in the province of Nova Scotia. The park consists of two separate properties: the main park is located in the upland interior of the Nova Scotia peninsula bordering Queens and Annapolis counties; and the smaller Kejimkujik Seaside unit, located on the Atlantic coast of Queens County. The park covers 404 km2 (156 sq mi). The inland unit is designated a National Historic Site of Canada, making Kejimkujik unique in the park system as the only national park whose virtually entire area is a National Historic Site.

The bedrock of the park consists of Precambrian to Ordovician period quartzite and slate, plus Devonian period granite. All of these rocks, especially quartzite, have a high silica content and provide scanty amounts of nutrients to the soils that develop on them. The slate, however, is fine-grained and produces a loamy soil which yields its nutrients more quickly than the stony sandy loams and loamy sands found over the coarse-grained rocks. Most of the slaty loams occur around Kejimkujik Lake. Deep outwash sands and gravels form a band west of the lake. Elsewhere the soil landscape is dominated by the cobbly, often shallow granite or quartzite material. Podzols underlie most well-drained areas. Gleysols and peat bogs dominate where drainage is poor. The park receives acid rain, and its soils have few available acid-buffering minerals, so strong acidity is the rule for soils and waters—even large bodies of water such as Kejimkujik Lake.


...
Wikipedia

...