Mick,
If you photograph something like this it is normal to include a scale. If you can't get a 'proper' scale bar use a ruler, coin or something everyone knows the size of. In the field geologists, sedimentologists etc often use their G-pick, shovel or camera lens cap. (I've also heard of less appropriate scale bars but lets not go there.)
At the moment I don't know whether the rock is 0.1mm across or 1mm, 10mm, 10cm or half a football field.
There are a few ways such an 'erratic' may have go on to the granite. If there is higher ground nearby it may have washed down, and that could have happened so long ago that it is no longer near a stream. The surface in your first photo looks pretty much like an effect caused by flowing water that is cavitating (I've forgotten the term). Otherwise, was the rock near a road or other places where people have moved things around? That is a trick for young players.
Carl suggested you check the streak. Density and hardness are other characteristics you can easily check.