The snow in Observatory gully is similar to what was there last spring as well. My flatmate Guy was out climbing on the 12th, see [
guysteven.blogspot.com]
Although that was a few days ago now, there has been essentially no change in snow cover since the 7th of Jan at this level. I know this as crown walls of avalanches that released on that day remain clearly visible in some locations.
Compare the top picture, to the one that I took on myself and Firefly's trip up there last year in early April [
www.flickr.com]
You can see that, similar to other locations in the West, that the was roughly the same (perhaps slighlty more snow) snow about in early April last year as there is now. Comparing the two pictures, there is a small flat ledge on the buttress on the left, that the snow was up to the right hand end of last year, but is not quite there at the moment. Also the rock patches on both the other sides of the gully, are sticking out a bit more at the moment. However, these differences are pretty minimal (less than I metre I would say). As Firefly mentioned the snow at the moment is hard and icy. It is presumable is is the mass of snow in any location, rather just the depth, which, all other things being equal, controls how quicky it melts. It is relatively easy to keep an eye on the depth, while the density (other than the very surface layers) is much harder to know. How much the average density of the snowpack varies from year to year during the melt season?, how much of a difference does it actually make?
As regards the crevasse in Coire an Lochan, big crack is not uncommon in that location. It forms at the top of an area of slabs, which can be seen at , and is caused by water lubrication the base of the snowpack below the crack, causing it to creep downards. I am sure it will fill in again in the next snow cycle.
Edited 1 times. Last edit at 16.45hrs Wed 18 Jan 12 by balir.