[Journal entry for March 4, 2017; Blauvelt Mountain,
Harriman State Park NY] The morning is very cold for March, about twenty
degrees Fahrenheit. I’m wearing thermal
underwear and a couple of heavy shirts.
The dawn sky was clear, but clouds are starting to fill up the sky. A gusty wind blows. I park at the end of Johnsontown
Road in Sloatsburg NY and take the White Bar Trail (blazed in white)
northward. I make a little detour to
visit what appears to be a terrace that once hosted a house (though no part of
any building remains). The rivulet
besides the terrace has been spanned by a small stone bridge and its banks have
been reinforced with stones. The area
must once have been a pretty place to live, especially since enormous and
picturesque boulders decorate the adjacent woods.
I connect with an old woods road that heads
west. I cross Spring Brook at the ford,
stepping from stone to stone. It is
running strongly. A little ice rings boulders mid-stream. A take the left hand turn at a fork and the
road rise steadily uphill. The ridge is called Dater Mountain in the south, Pound
Mountain in the middle and Blauvelt Mountain in the north. I leave the road near when it approaches a
prominent cliff, one of the many south-facing scarps in the Hudson Highlands
that were formed by glacial plucking during the Ice Age. I hike over to the cliff; it’s made of gneiss
with a sub-horizontal foliation and has a layered appearance. One end of the
cliff has a small, boxy tower (or tor,
as they are called in the Highlands). A
weak layer near its base of the cliff has eroded back, making a shallow
cave. I peer in, thinking that it might
be large enough to shelter a person. I
continue uphill, passing a small wetland with swamp vegetation. I’m always amazed that the water does not
leak out of these mountain top pools, for the rock on the cliffs is fractured,
yet I know of many in the park. Further
uphill, I poke around a second, larger cliff.
This one had icicles clinging to its face.
The land above the cliff is fairly open, especially
along the western edge of the hilltop, where wide rock ledges command pretty
views to the west. I cross the Tuxedo-Mount
Ivy Trail (blazed in white with a red bar) and continued my northward
bushwhack, climbing up to the summit of Blauvelt Mountain. The land here is also open, with good views
in most directions. I will need to come
back when the vegetation is green and when the sun is lighting up the views,
for the summit then will be a delightful place.
Today, the wind, the grey sky and the leafless brown bushes make it
bleak. The view to the east is the most
interesting, for in the distance I can see a blue sliver of Lake Sebago, and
Conklin Mountain, beyond it. I prowled
around the summit area, coming across a 1964 United States Geodetic Survey
benchmark affixed to a rock ledge.
I hike down the steep northern flank of Blauvelt
Mountain, following a gulley with a prominent rocky cliff on its western
side. The lower part of the cliff has
been torn apart (by now-defunct glaciers, I guess), making a small lemon
squeezer. I have fun scrambling through
it. The downhill face of the cliff is a
flat overhanging wall that is rather striking in its appearance, especially
since it had icicles hanging off of it. Eventually, I cross Spring Brook and
rejoined the White Bar Trail near Dutch Doctor Shelter. I had stayed in the shelter on my overnight
trip a couple of weeks ago, and so do not visit it today. Instead, I head back south on the White Bar
Trail.
I decide I have time for a detour, for noon is still
a half hour away, so I once again take the woods road, but this time follow it
until it intersects with the Blue Disk Trail (blazed in blue). I take this trail southward toward Pound
Mountain. It passes through a very
interesting bowl that is walled on three sides by high cliffs. Shortly
thereafter, I reach the overlook by the cliff on Pond Mountain that is called Almost Perpendicular. The trail descends this cliff through a gulley. At the bottom, I connect with the Kakiat Trail (blazed in white) and head back east, crossing
Spring Brook one last time. I follow the
brook downstream for a few hundred yards, admiring the ice formations on rocks
and branches. I have to work to get back
to the White Bar Trail, even though it is just a few tens of yards east of the
brook, for the way is mostly blocked by barberry and other thorn bushes. A few minutes later, I was back at my car.
I say almost no wild life on my hike – just a few
Turkey Vultures and a Downy Woodpecker.
About 3:30.