Sifton Bog - London, Ontario - Places of Geologic Significance on Waymarking.com

From the website:

The bog is a product of glaciation. As the last ice sheet melted 13,000 years ago, a large block of ice broke off and settled in the glacial till (sand and gravel). When the block melted it left a kettle lake, cut off from any watercourses. Sedges, mosses and other plants gradually colonized the margins of the lake. Due to the cool, oxygen-poor conditions, when dead plants sank to the bottom, they did not break down fully, but became compressed as peat.

In time, the accumulating peat formed a semi-floating mat that crept from the outer edges of the bog towards the open water at the centre. As the mat became consolidated, Sphagnum mosses, heath plants and spruce trees grew on the drier hummocks.

Waymark is confirmed to be publicly accessible: yes Parking Coordinates: N 42° 58.463 W 081° 19.430 Access fee (In local currency): .00 Requires a high clearance vehicle to visit.: no Requires 4x4 vehicle to visit.: no Public Transport available: yes Website reference: [Web Link]

Visit Instructions:
No specific requirements, just have fun visiting the waymark.

Recent Visits/Logs:

Date Logged Log User Rating   06/19/2016 Keldar5 visited it