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      The
      snow began to get a bit deeper after I passed the Hale Brook ravine. There were a 
		couple of small downed trees
      that I had to duck under, but for the most part, it was just a slow uphill 
		slog through snow that was gradually beginning to soften.             
		
		
      	There were maybe five or six 
		inches of new snow on top of a hard-packed base. The new snow was soft 
		and sticky and tended to adhere to the bottom of my snowshoes in large 
		clumps. It would have been good snowball- or snowman-making snow. I had 
		to stop fairly often and use my poles to knock it off as it made me feel 
		like I had heavy cement blocks attached to my boots. Even worse, it 
		covered the crampons on the bottom of my snowshoes, rendering them 
		useless and leaving me with no traction, not a good thing on a steep 
		trail. 
		
		The higher I climbed, the more snow there 
		was clinging to the branches of the fir and spruce trees that lined the 
		trail. Occasionally, I saw a yellow blaze on a tree at or below knee 
		level, a good indication of just how deep the snow still was this late 
		in March, considering that blazes are usually at eye level. 
      
		As the trail curved to the right and headed 
		in a southerly direction, I got a look back north or northeast (again 
		through the trees) toward what was probably either Cherry Mountain or Mt 
		Deception. 
		
		The temperature was quickly rising as the 
		day progressed, and the snow on the trees was beginning to melt and form 
		tiny icicles on the tips of the branches and needles. Climbing still 
		higher, the icicles grew larger and soon occupied most of the open 
		spaces between the evergreen boughs. 
		
		Almost at the top, the sunbeams broke though 
		the treetops from clear blue sky, revealing an entire forest shimmering 
		with transparent ice and bright white snow.              | 
            
               
				Hale Brook 
				Trail. On the other side of the ravine, the trail began to 
			switchback up the summit cone.  | 
            
               
				
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