The park is located in a flat plain.
Its highest point, Mount Tom, is at 180m.
Precambrian to Ordovician quartzite and slate form the bedrock, along with Devonian granite.
These rocks provide few nutrients to the soils that develop from them.
Podzols are found in well-drained areas, which poorly-drained areas are dominated by Gleysols and peat bog.

Fifteen per cent of the park is covered by lakes.
Evidence of the Last Glacial Period include drumlins, erratics, and eskers.
Major rivers include the Mersey, and the Shelburne, major lakes include Kejimikujik, and Luxton.

Kejimujik National Park Seaside includes white sandy beaches and coastal wetland areas.
The park is located in a flat plain. Its highest point, Mount Tom, is at 180m. Precambrian to Ordovician quartzite and slate form the bedrock, along with Devonian granite. These rocks provide few nutrients to the soils that develop from them. Podzols are found in well-drained areas, which poorly-drained areas are dominated by Gleysols and peat bog.
Fifteen per cent of the park is covered by lakes. Evidence of the Last Glacial Period include drumlins, erratics, and eskers. Major rivers include the Mersey, and the Shelburne, major lakes include Kejimikujik, and Luxton.
Kejimujik National Park Seaside includes white sandy beaches and coastal wetland areas.
Kejimkujik National Park