In reply to WEYHILL8689:
Taking avalanche advice off random users of a forum isn't ideal, but you've had some good advice to look at the Be Avalanche Aware framework. You can use the basic principals of this to help you try and make sound decisions. The Chris Walker trust has some good collated information you might find helpful: https://chriswalkertrust.co.uk/avalanche-awareness-resources/
Snowpack analysis whilst on the mountain is actually of limited use outside of general interest and confirming what you know. If you're looking at windslab and worrying about it, then you're in the wrong place and should have taken that into account in the planning phase. Use the BAA framework to assess the hazards and work out how to avoid them.
However, to answer your questions:
1: Generally, you are correct that windslab and cornices both build in the lee of the wind. Sometimes this is as simple as the opposite side of the mountain to the prevailing wind direction, sometimes localised topography has a huge effect and can cause accumulations in places you wouldn't expect. A cornice won't form 'in' a gully but around the rim at the top. Windslab can occur anywhere.
2: Full depth avalanches can occur to ground level and many different layers can build during one snowfall event. E.g snowfall on bare ground overnight could form: 5cm of powder, 10cm of windslab, 1cm of graupul and 10cm of windslab giving hazardous layers even if there was no snow on the mountain the day before. This example is quite extreme, but illustrates that one snowfall event isn't just even snowfall.
3: Powder avalanches can occur, but theres rarely enough fresh powder in Snowdonia to make this an issue. Windslab is far more prevalent. From a climbing and enjoyment perspective, battling up Parsley Fern Gully when it's full of powder is going to be slow and unpleasant.
4: Given settled cold conditions, any snow which falls will stay in the state it has formed in. Cold settled conditions where the snow does not change condition will preserve any weak layers in the snow. A wet, thawing, avalanche would only occur if it's thawing, often full depth sliding on the grass which has been lubricated by melt water.
Your ideal conditions for climbing easy snow gullies come after a cold spell to cool the ground and freeze the turf, a big dump of wet snow, a slight thaw and then a hard freeze. This thaw-freeze cycle will turn powdery or mushy unconsolidated snow into firm neve which is easy and enjoyable to climb, although serious in the event of a slip or fall.
Post edited at 22:51