There are large glaciolacustrine deposits in the Okanagan. They are 50-75 m in height. You can see in the last two photos how big they are. There is a road that runs along the lake and the last pic has a white dot on it that’s a semi.
My theory is that these are beach sediments, as they texture out to silt loam, which is typical for post-glacial lakes in the area. If it were lake sediment itself, it would be much finer in texture (CL, SiCL, C, HC).
There are large glaciolacustrine deposits in the Okanagan. They are 50-75 m in height. You can see in the last two photos how big they are. There is a road that runs along the lake and the last pic has a white dot on it that’s a semi.
My theory is that these are beach sediments, as they texture out to silt loam, which is typical for post-glacial lakes in the area. If it were lake sediment itself, it would be much finer in texture (CL, SiCL, C, HC).
Above 75 m is bedrock and soils on residual