Quote:
Originally Posted by cairnstone
Sandstone layer is typical and very dense material that supports the load. Piles are used on the out skirts of downtown typically as the material is of different composition. Shaw tower sits on Piles and so does some of the properties around False Creek.
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Can you point to a source for that? Generally, my understanding was Downtown sites (like this one) have 30 to 60 metres of glacial till. [
source] The sandstone layer would be quite a bit lower down, unless it's a spot where the glacial till is thinner (like where a stream flowed in the past, for example).
Obviously round the northern edge of Downtown there's a lot of infill on top of a natural beach, so buildings might need piles. Similarly, as you say, False Creek (which used to go to Clark Drive) was filled, so buildings along Terminal Avenue for example might be piled, and so were some Concord buildings near False Creek (although usually as coffer dams to stop the sides collapsing, rather than supporting piles).
I'm not aware of any deep underground parking excavations (like this one) having any additional piling. Unless the glacial till isn't compacted (which doesn't generally occur Downtown) it's perfectly capable of taking the weight of the building above. "Some tills are compact and concrete-like, whereas others are sandy and loose. Till commonly has a high bearing capacity and thus is an excellent foundation material." [
source] There's a different story in other parts of the Lower mainland, as geology changes quite a bit further east, but my observation of Downtown holes (and looking at McMinsen's pictures) are that they're dug, and then filled, without piles in most cases.