In reply to spenser:
> Your hypothesis matches up with the asperity contact theory of friction covered in my tribology module this year, a reasonable explanation of this can be found at the bottom of this page:
> As a route receives traffic the peaks of the asperities are snapped off reducing their overall height, this means that a greater normal force must be applied to the surface to achieve the same amount of friction. If there is a grain of sand on the sole of your shoe the asperities in close contact with it, due to the very limited contact area between the two, will be subject to a much greater amount of stress than if in contact with the sole of the shoe which deforms around the asperity therefore maximising the contact area between the two surfaces. Obviously the grains of sand also act like ball bearings against the rock which considerably decreases the amount of friction at the shoe rock interface. This explains why sandy shoes polish rock very quickly, decreases the friction between shoe and rock.
I think that what the OP is referring to, is the way that different rubbers will perform in those circumstances.
I like the explanation of how the newer, low rebound rubbers work, given in the article I posted a link to:
" Give It Time To Work
Knowing how sticky rubber works can actually help you to make the most of its grip. If you simply step onto a polished hold and push off, you may find that your foot slips slightly. To make the most of the grip, place your foot on the hold then weight your foot to put some pressure on the area and wait for a few seconds.
The weighting and waiting gives the chance to the rubber compound to conform to the surface of the hold and quite often you'll find you can now stand up on a hold which previously felt way too slippery to use. It's a trick that works with both rock boots and sticky-soled approach shoes."
(Reference here to the newer "sticky rubber")
Perhaps A lower asperity surface will reduce the effectiveness of this?