There are some outcrop knolls. Two kame deposits are within the site with local relief up to 60m. Being flat and having abundant wetland areas, the drainage of much of the area is poor. There are several significant streams that flow into the Sapochi and Odei Rivers and the few lakes within the area are small. Bog and fen occur on most of the low-lying terrain.
Permafrost occurs a few feet below the surface of the bogs.
It also occurs at a greater depth under thickly wooded slopes of some clay mantled ridges.