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Quadricentennial Challenge
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Catskills Live! Trails & Wilderness Association
issues a challenge to all — venture forth and seek all 15
Quadricentennial Challenge geocaches. Go to many great places
throughout Ulster County — visit the shores of the Hudson,
feel the cool air in an historic cement mine, enjoy our small
parks, bicycle on our rail trails, summit two Catskill peaks, and
savor the breath-taking view from Gertrude's Nose in Minnewaska
State Park Preserve. Bask in our county's treasures with family and
friends, exercise your body, and build lasting memories. Over 100
specially minted commemorative Quadricentennial geocoins were
released from 15 Challenge geocaches set up in 2009 in celebration
of the 400th anniversary of the exploration of New York State by
Henry Hudson. Congratulations to Joe The Mailman, the first person
to complete all 15 caches! Funding for the Challenge was provided
by Ulster County and the Hudson River Valley
Greenway.
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| High Point Mountain |
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At 3080 feet above mean sea level (3080 ft. msl), High Point
Mountain is the 83rd highest peak in the New York State Catskill
Forest Preserve. It is 1100 feet lower than Slide Mountain, the
highest peak in the Catskills.
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Sometimes referred to as Ashokan High Point Mountain, High Point
Mountain stands prominently out from other mountains situated
further to the north, northwest, and west. For this reason, it was
considered for a mountaintop hotel in the 1800s. Its lofty heights
provide excellent views of the region, especially during leaf-off
conditions.
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The elevation gain from Kanape Brook, near the parking area, to
the summit is about 1,980 feet and is strenuous in places, but
mostly only near the top of the mountain. This moderately strenuous
route with the summit trail loop is about an 8 mile round trip.
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This is a most pleasant Catskill Mountain hike.
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Glacial Lake Shandaken and Wagon Wheel
Gap
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The forested and sculpted landscape you hike up through on the
way to the summit is the product of hundreds of thousands of years
of erosion by streams and glaciers.
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Today, the waters of Kanape Brook (followed along the lower
trail) slowly wind their way down hill, first joining the Bush
Kill, and then flowing into the Ashokan Reservoir, which is
actually the dammed up Esopus Creek (at 585 ft. msl). While the
12-mile long Ashokan Reservoir seems large by today's standards, it
would have been dwarfed by the glacial lakes once present
there.
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About 14,000 years ago, the waters of the Esopus Creek were
impounded in an expansive glacial lake behind a huge ice dam that
extended between Overlook and High Point Mountains, as well as far
to the north and south. NYS Quad Challenge - Tremper Mountain
(GC1V6F3) discusses Glacial Lake Peekamoose that drained out
the Peekamoose gap at 1830 ft. msl.
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As this massive ice dam pressed against the east side of High
Point Mountain began to melt down, it eventually decreased in
height until another lower outlet elevation was reached. This
occurred along the flank of High Point Mountain. When the surface
elevation of the glacial dam dropped to about 1600 ft. msl, the
water level of Glacial Lake Peekamoose rapidly dropped in response
to a lower release point. It quickly cut a V-notched water-gap in
the side of High Point Mountain where a bedrock-walled gorge now
roared with surging glacial melt waters. This gap, located about
2/3 of the distance down the flank of the mountain, is referred to
by geologists as the Wagon Wheel Gap. One good observation point is
from the Ashokan Reservoir Dividing Weir along Reservoir Road,
especially during leaf-off conditions.
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As
this narrow gorge was down cut, the glacial lake level fell first
from 1830 ft., to about 1600 feet, and then downward to about 1330
feet. This new lake is referred to as Glacial Lake Shandaken. Clues
documenting the presence of this glacial lake are found in
sediments in the Esopus Creek watershed, in the now dry relict
plunge pools and water falls on the east side of High Point
Mountain, and in the form of water gap itself. |
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As
you climb the mountain, picture yourself first crossing Kanape
Brook at about 1100 ft. msl on the bottom of a vast glacial lake,
some 730 feet and 230 feet beneath the surfaces of Glacial Lakes
Peekamoose and Shandaken, respectively. The maximum depths of these
glacial lakes were about 1435 and 935 feet near the Ashokan
Reservoir. Then picture yourself ascending through the surface of
Glacial Lake Shandaken, upward another 1750 feet to the summit
amidst the thundering roar of melt water and icebergs cascading
through nearby Wagon Wheel Gap. Glacial melt water from the Esopus
and other streams have, through time, helped carve and deepen the
Hudson River so that it was navigable by Henry Hudson and as it
continues to this day. |
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The Mountainside Today
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Kanape Brook is crossed and followed in the early stages of this
hike. Vestiges of previous settlement are seen in a laid stone
spring, stone walls, stone piles, and the remains of an old dam now
only partially across Kanape Brook.
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A large portion of the trail is quite gentle and is used for
crosscountry skiing. In places, sandstone ledges with cross-bedded
layers whisper of deposition in braided stream channels almost 400
million years ago.
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Closer to the summit, steep trail sections are generally short
in nature, followed by more gentle trail segments. It is by far the
better plan to complete the upper trail loop in a counter-clockwise
direction, thereby continuing straight at the loop junction point.
Also, this direction is preferable relative to both the ease of
ascending and descending from the mountain's summit.
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While more scenic vantage points are present during times of
leaf-off, a number of excellent vistas are present year round
— especially the summit vista. The broad summit area itself
is well worth the hike, as dwarf oaks and expansive blueberry
meadows will bring a smile to all. Be sure to stay on the trail and
protect this area.
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The Cache and Parking Access
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Access to the cache is from Route 42, the Peekamoose Road, found
extending westward from Route 28A out of West Shokan. An
established parking area is present along the northwest side of
Route 42. The parking area and trail are illustrated on NY-NJ Trail
Conference Map 43 of southern Catskill Trails. The trail begins on
the opposite side of the road from the parking area.
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The cache is a 2-liter cylindrical poly bottle hidden a short
distance from the trail. It is not located on the summit of the
mountain, but rather down slope and west of the summit at an
elevation of about 2810 ft. msl. The cache is best approached by
following the upper loop portion of the trail in a
counter-clockwise direction, continuing past the summit and
beyond.
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The cache is filled with kid-friendly items and, initially, four
NYS Quadricentennial Challenge geocoins designed to travel
throughout the world. This geocache was approved by the New York
State Department of Environmental Conservation.
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Please Cache In and Trash Out!
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