It was quite cloudy on the top of Aonach Mor today, so no great pictures today. Through the course of the winter we see significant changes in snow cover. In certain areas the snow builds up to great depths. When standing at the top of, for example, Easy Gully, I often wonder just how much snow there is under my feet. I am still not sure, but thought I would put on some pictures of the top of the East Face taken recently (still quite early in the season), to compare with some taken in the summer to give an indication of snow depth, and how the character of the place changes.
Sunday, January 31, 2010
Now and then.
Monday, January 25, 2010
Sunday, January 24, 2010
Poor visibility weekend
Friday, January 22, 2010
Pictures from today
Monday, January 18, 2010
Soft cornices.
Last nights wind and snow has formed some large and fragile cornices. These are prone to collapse both spontaneously, or if disturbed, and can easily release the windslab on the slope below. Unfortunately the light was very flat, and you can't see much in any of the pictures that I took of the cornices. However, the picture shows the side/crown wall of a cornice triggered slab avalanche (notice the rope, I approached this safely via a short abseil from the top). Although this was not a large avalanche in the grand scheme of things (the release area was about 8m across), it would have easily have sent you tumbling should you have been climbing/walking below. Another such crown wall was just visible further along.
If climbing in these conditions it is wise to consider what is above you what is above your route, and avoid gullies with big cornices/areas of windslab above. With a bit of consideration and forward planning (some local knowledge helps as well though) routes which are safe from such objective dangers can almost always be found.
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Monday, January 11, 2010
Avalanche on Aonach Mor
On the way up Aonach Mor this morning we heard reports of a "wee slide" being triggered on the West Face at the lowly altitude of about 600 metres. We had been planning to head to that sort of area anyway, so we decided to go and investigate. What we found was a hard slab avalanche had occurred. It was about 50 metres wide, and had run about 200 metres down the hill side. The crown wall reached a maximum depth over a metre, and was 50cm to 1 metre deep from most of it's length. A bit bigger than a "wee slide" I thought. The avalanche had run on a deep and particularly hard layer of small rounded crystals. Today's snow profile is a profile of the crown wall.
Looking south to where the crown wall height was at it's greatest (about 110cm). The first two pictures were taken from the location of the figure in the third picture.
Sunday, January 10, 2010
Blowing snow.
Even a seemingly uniform layer of snow will contain many mirco-layers, created by constantly changing conditions as the snow was deposited. Usually these are not too evident, but the strong winds blasting this block of windslab that I dug up really made this micro-layering visible (the horizontal bands).Saturday, January 09, 2010
Shearing layers
Three very clean shears came out today when doing a tap test on at the top of the West Face of Aonach Mor. The lollipop sticks were included to mark layers shear, although they are pretty obvious in this case. I am not sure whether you will be able to read scale on the ruler, but in this test these shears occurred at a depth of 12, 20 and 33 cm. This photo was taken on a low angled (about 15 degree) slope with a Westerly aspect. I would be very wary of going onto any steep, snowy slopes with this aspect at the moment.
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Thursday, January 07, 2010
Deep drifts
Wednesday, January 06, 2010
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