Lack of reference leads to a confused impression of this torrent of water. An adult human, standing on the lower rock ledges, will be dwarfed by the surroundings.
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Lucifer Falls at moderate spring flood. The Gorge Trail is closed for the winter due to the danger of falling rock. The water volume can sweep an unwary hiker quickly over the brink.
The potential for fatalities is increased by black ice on the smooth slate walkways along the torrent. Can you spot the barrier blocking access to the path? I am at a secure perch at the falls overlook on the Rim Trail, opened at this season.
These shots were hand held. I used a Sony Alpha 700 dslr with a variable “zoom” lens, great for framing compositions.
Robert H. Treman New York State Park.
Click for a slideshow of this Waterfall of the Old Mill sequence
Copyright 2019 All Rights Reserved Michael Stephen Wills
Walking the level the these red might be overlooked hanging sparsely under nodding branches. From the leaf shape you may wrongly identify this as Solomon’s Seal. This specimen, growing on a shale ledge of the glen, reveals sparse red fruit, not the plentiful dark blue of Solomon’s Seal. This is Rose Twisted-Stalk (Streptopus roseus), a member of the Lily family. The two are often found close together. I found no Solomon’s Seal this trip.
The moss beneath the Rose Twisted-Stalk is plentiful here beneath the constantly dripping porous shale glen wall, mini swamps. I am not confident enough to following identification to each the red fruit. From the damp location and leaf shape I am guessing this to be mountain- cranberry (Vaccinium vitis-idaea). The first photograph of this posting is an overview.
A shallow grotto
Finely layer shale in the following photograph is sediment eroded over 50 million years from the Arcadian Mountains, washed into the shallow inland sea of the Appalachian Basin. We see here a transition between fine, fragile shale and another, harder, durable sedimentary rock, limestone. There was a stone on the otherwise flat surface of the limestone around which the sediments forming the shale grew.
We see the detail because here is a persistent, sparse spring. The trail builds created a well here to carry the outflow, preventing trail erosion.
Copyright 2019 Michael Stephen Wills All Rights Reserved