Well, that looks like the northern Presis in the background, and the Carter Range to your right? Are you and Cath headed up Shelburne Moriah? Haven't a clue what # it is though. Not into NHHH.how sweet it was..
another sweet peakbragging hunt...any of you grid experts care to guess the peak and the #???
I'll guess about 425 of the grid for you...and about 4000 for Flo.how sweet it was..
another sweet peakbragging hunt...any of you grid experts care to guess the peak and the #???
Interesting formation...While huntin', we couldn't help but notice that Kissin' Rock (which naturally comes a bit before the rock known as "Second Base") was covered with thick ice, which had this amazing surface to it; very small, slightly raised polygons about 1/4" or less etched in frost. All purdy like.
I can't seem to find an explanation of how this particular phenomena happens.
Any ideas? Warm moist air hitting the cold icy rock and being drawn into hex shapes by ... ? Voodoo?
how sweet it was..
another sweet peakbragging hunt...any of you grid experts care to guess the peak and the #???
OK. I had misinterpreted the 1/4" as the height.Doug, the cells of the honeycomb pattern were about 1/4" or less.
It looks to me like the edges of the polygons were touching (or connected) at one point and the edges withdrew (or cracked apart and withdrew) and frost formed in the cleared boundaries.My latest theory is that the pattern was formed by an evenly distributed layer of water droplets that had formed by the icy rock "sweating" under mild temps, then freezing/drying quickly in the cold wind, and that the surface tension of each drop created the pattern as the frost crystals formed along the shrinking circumference of the drop where it joins the rock's thick icy surface.
Or something.
This is the ding ding ding for me. I've seen videos of this years ago. The white edges are the frosted joining points of the outward growth of each polygon meeting each other. Each one individual would have a smooth glaze ice appearance but when they meet they are like two separate growth patterns coming together in a non structured form.Another wild guess: vapor freezing (depositing) directly on cold rock (possibly initiated by droplets). Each individual ice crystal starts at a different nucleation site and grows outward. When the crystals meet, the crystal lattices are mismatched and the crystals don't join. The join lines then grow upward faster than the non-edge surfaces. (Crystals grow at different speeds on different faces. This conjectures that the dislocation at the junctions grows upward faster than the flat surfaces.)
Doug
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