An exposure of massive, shell-bearing stony sandy mud overlain by stony silty sand and fine to medium sand.
Drainage ditch where you need to enter the forested area |
Exposure of the glacial sediment |
Another view of the sediment cut |
Hammer for scale |
Fossils in the stony sand |
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Sand sediment is exposed here that originally was transported to the sea via a meltwater channel flowing along the Campbell River Valley. The sediments coarsen towards the apex of the delta, where they are mainly pebble-cobble gravel.
The right path to take |
The boardwalk over the meltwater channel |
Steep slopes on the east side of the channel |
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A large glacial erratic and a path with a view of the Abbotsford outwash plain.
The not-so-conspicuous sign and entrance |
The rock with person for scale |
Morphology of rock with quarter for scale |
Morphology of rock with quarter for scale |
View of the outwash plain to the south |
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Exposed are approximately 34m of gravel and sand overlain by up to 3m of lodgement till and 2m of eolian sand and silt.
Glacial Lake deposits.
Not Available
Sumas basal till (probably lodgement till) is exposed on a cut in the road.
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Latitude: 49°11'42.000"" N
Longitude: 122°10'55.000"" W
Elevation: 4.30m asl
Climate ID: 1108447
Environment Canada Site for Station
Not Available