Mount Tremper | |
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Timothyberg, Tremper Mountain | |
![]() Mount Tremper from Route 28 to southeast | |
Highest point | |
Elevation | 2,740 ft (840 m) [1] |
Prominence | 300 ft (91 m) |
Coordinates | 42°4′27″N74°16′39″W / 42.07417°N 74.27750°W Coordinates: 42°4′27″N74°16′39″W / 42.07417°N 74.27750°W [1] |
Geography | |
Location | Shandaken, New York, United States |
Parent range | Catskills |
Topo map | Phoenicia |
Climbing | |
Easiest route | Trail/road |
Mount Tremper, officially known as Tremper Mountain and originally called Timothyberg, is one of the Catskill Mountains in the U.S. state of New York. It is located near the hamlet of Phoenicia, in the valley of Esopus Creek.
At 2,740 feet (840 m) in elevation, it is well below the higher peaks of the region. Its slopes were a source of two major local products during the 19th century: hemlock bark, a source of tannin, and bluestone used in construction. Later it was the site of Tremper House, one of the Catskills' earliest railroad resorts. Henry Ward Beecher and Oscar Wilde were among the guests there.
In the 20th century it was acquired by the state and became part of the Catskill Park Forest Preserve. Its location in the Esopus Valley between the northern and southern Catskills made it an ideal place for a fire lookout tower, which still stands on the mountain's summit. The Mount Tremper Fire Observation Station has been restored and listed on the National Register of Historic Places. Hikers often follow [2] the old road to it from Phoenicia, also a section of the Long Path long-distance trail, to enjoy the views from the tower.
Tremper is a sprawling mountain at the south end of a range of low-elevation peaks between Warners Creek and Silver Hollow on the north, Stony Clove Creek on the west, Esopus Creek on the southwest and the Beaver Kill on the southeast. The latter three are closely paralleled by state highways 214, 28 and 212. Its summit dominates the view from westbound Route 28 at the small hamlet of Mount Tremper. [1]
The mountain's lower slopes are gentle, becoming steep around 2,200 feet (670 m) and then leveling off again at the summit ridge. Unnamed tributaries of the surrounding creeks run down narrow valleys on the mountain's slopes. The summit ridge continues northeast to an unnamed summit and then Carl Mountain, both higher than Tremper at 2,820 feet (860 m) and 2,880 feet (880 m) respectively. [1]
Most of the mountain is within the Town of Shandaken, whose largest population center, the hamlet of Phoenicia, is at the southwest foot of the mountain. Another smaller settlement named after the mountain is to its south. A small portion of the mountain's lowest eastern slopes is within Woodstock. [1] Most of the land on the mountain is part of the Phoenicia Wild Forest management unit of New York's Forest Preserve, part of the Catskill Park. The rest, including most of the slower slopes, is privately owned. [3] The public land is managed by the state Department of Environmental Conservation (DEC). [4]
Like the Catskills as a whole, a dissected plateau, Tremper was formed not through the upthrust of rock layers but by the gradual erosion of stream valleys in an uplifted region about 350 mya. Its rock layers and bedrock are primarily Devonian and Silurian shale and sandstone. [5] Bluestone is present in enough quantity that a quarry was once located on the south side of the mountain at an elevation of 1,495 feet (456 m). Its remains are still visible today from the old road to the fire tower, which passes it. [6]
Because of its low elevation, the forests on Mount Tremper are dominated by a forest type referred to in the Catskills as southern hardwoods. [7] This is dominated by oak, hickory and pine species, with some basswood and poplar scattered in lower elevations. Chestnut were once common as well, but most died off in the blight of the early 20th century. Some eastern hemlocks, once more widespread before they were harvested for their tannin-rich bark, remain, primarily higher on the mountain where the barkpeelers never reached. The summit ridge has some areas of the northern hardwood forest (beech, birch and maple) more common on higher Catskill slopes. [6] The more shade-tolerant northern hardwoods are slowly invading the southern hardwoods as an understory; due to the cessation of human intervention in the forest they will eventually displace the southern hardwoods. [7]
Tremper has a typical assortment of animal life for the Catskills. Herbivores such as white-tailed deer, chipmunks and porcupines dominate the lower end of the food chain, with predators like fishers and black bear at the top. The ledges in the former quarry are one of the few rattlesnake habitats in the Catskills close to a hiking trail, with at least one confirmed den, [8] and visitors should exercise caution if they wish to explore it. [2] [9]
Tremper's human history has two stages. For the century after the area's first settlement it was primarily an economic resource, sustaining several industries. Since the end of that period it has become a recreational resource.
The mountain was first known as Timothyberg, in the vernacular of the early Dutch settlers of the Catskills. The area was first settled in the 1780s. Its location near the creeks and valleys made it ideal for barkpeeling, the first major industry of the Catskills. Bark from the many eastern hemlocks on its slopes was a rich source of tannin, and leather hides were often brought to the region to be tanned. The creek valley made it possible to easily transport them to and from the Hudson River at Kingston to the east, and the later development of the Ulster and Delaware Railroad (UDRR) made it even easier. The road up the south side of the mountain, which forest historian Michael Kudish calls the best example of an extant bark road in the Catskills, was built for this purpose. By the end of the century, since a synthetic process for creating tannin had made it less necessary to harvest large acres of forest, it was being used for quarrying instead. [6]
The railroad made another industry possible at that time. In 1879, after hotelier Jacob Tremper opened the Tremper House, a resort on its slopes near Phoenicia, that part of the mountain became known by his name, [10] He invited a number of prominent clergymen of the time to its dedication. Henry Ward Beecher, the main speaker, asked for God's blessing on the location and predicted a prosperous future. [11] Another celebrity guest, Oscar Wilde, shocked the region during a lecture at the Tremper House in 1882 when he proclaimed its location at the foot of the mountain aesthetically preferable to those of hotels such as the Catskill Mountain House located on mountaintops since in valleys, "there the picturesque and beautiful is ever before you". [12]
It remained in business until 1904, when the town, under pressure from UDRR magnate Samuel Coykendall, who owned several competing resorts, rescinded permission for it to become a sanatorium for tuberculosis patients. Coykendall, and other hoteliers in the region, alleged that tourists would avoid the region if those patients were present anywhere within it. [13] The vacant hotel burned down four years later, in 1908, and was never rebuilt. [6]
A decade earlier, the legislation that created the state's Forest Preserve, with its "forever wild" clause, had been added to the state constitution. The state acquired Tremper's summit and some of the other land on its eastern slope in 1901, and established a plantation there for reforestation. [10] A mix of eastern white pine, Norway spruce and Scots pine were planted. Unusually for the Catskills, the underlying land was not former pasture but forest that had been cut and burned repeatedly by barkpeelers. It did not establish itself although the land eventually reforested on its own. [6]
The Timothyberg side of the mountain was regularly burned over by blueberry pickers every year through 1916, the year the state built the 47-foot (14 m) fire lookout tower on the mountain and extended the old board road to make it accessible for observers coming by vehicle. It replaced another tower that had briefly stood on Slide Mountain, the Catskills' highest peak, a few years earlier. Tremper was chosen since it offered views of the lowlands that could not be seen so easily from the fire towers on Hunter and Belleayre mountains. [14]
In 1921 the state bought more of the mountain, allowing it to designate the road as a hiking trail. By 1931 it had been extended beyond the tower as a footpath, descending the northeast side of the mountain into Hoyt Hollow to Willow. Later in the 1930s a lean-to was built at the summit for backpackers to camp in. [6]
This trail system remained unchanged for most of the mid-20th century, save for the construction of a new lower section of trail and a trailhead about 0.3 mile (500 m) east of the foot of the road just outside Phoenicia. When the dormant idea of the Long Path was revived in the 1960s, the trail over Tremper was included. A wayward campfire led in 1966 to a wildfire that burned 10 acres (4 ha) just below the summit. Four years later the state closed the tower. [6]
In 1976 the state purchased some more land along the trail and built another lean-to at 2,100 feet (640 m), along the trail below the summit. The next year the tower's two support structures, the observer's cabin and a storage shed, were removed. These were the last significant changes to facilities on Tremper for two decades. [6]
At the end of the century interest in restoring and preserving the fire tower led to a local fundraising campaign after DEC proposed to remove it as a structure incompatible with the Forest Preserve. [15] It was reopened in spring 2001 and listed on the National Register in late 2001. [16] A new extension of the Long Path along the ridge past Carl Mountain to Plateau Mountain was opened that year as well.
The Phoenicia Trail, part of the Long Path, the former bark road extended to the fire tower, is a widely used route to Tremper's summit. Blazed with red plastic DEC markers, it begins 1.6 miles (2.6 km) south of Phoenicia along Old Route 28 (now Ulster County Route 40), across from the Esopus. It joins the old road after a half-mile (1 km) and follows it through several switchbacks past the old quarry, a spring, the Baldwin Memorial Lean-To and another spring. It reaches the lean-to and fire tower at 2.8 miles (4.5 km), after climbing nearly 2,000 vertical feet (610 m) from the trailhead. [3] [8] [9]
Less used is the approach from the northeast via the Willow Trail. Its yellow markers begin at the intersection of Jessup and Silver Hollow roads in Willow. It follows Jessup for a mile (1.6 km) before turning into the woods and ascending the south wall of Hoyt Hollow 1.5 miles (2.4 km) to its end at the blue-blazed Warners Creek Trail (also the Long Path). From there the summit and fire tower are 2.2 miles (3.5 km) to the south. This route requires less vertical ascent (1,640 feet (500 m)) but is longer (3.8 miles (6.1 km)). Hikers sometimes park cars at both Willow and Phoenicia to do a 7-mile (10.2 km) shuttle hike across the mountain. [17]
The Warners Creek Trail also makes a long approach possible from Stony Clove Notch to the north. It is 7.6 miles (12.2 km) from the parking area on Route 214 to Tremper's summit, with the trail going over one mountain and up the north slope of Tremper from Warners Creek. [18]
The Catskill Mountains, also known as the Catskills, are a physiographic province of the larger Appalachian Mountains, located in southeastern New York. As a cultural and geographic region, the Catskills are generally defined as those areas close to or within the borders of the Catskill Park, a 700,000-acre (2,800 km2) forest preserve protected from many forms of development under New York state law.
The Catskill Park is in the Catskill Mountains in New York in the United States. It consists of 700,000 acres of land inside a Blue Line in four counties: Delaware, Greene, Sullivan, and Ulster. As of 2005, 287,500 acres (116,300 ha) or 41 percent of the land within, is owned by the state as part of the Forest Preserve; it is managed by the Department of Environmental Conservation (DEC). Another 5% is owned by New York City to protect four of the city's reservoirs in the region that lie partially within the park and their respective watersheds.
Hunter Mountain is in the towns of Hunter and Lexington, just south of the village of Hunter, in Greene County, New York, United States. At approximately 4,040 feet (1,231 m) in elevation, it is the highest peak in the county and the second-highest peak in the Catskill Mountains.
Slide Mountain is the highest peak in the Catskill Mountains of the U.S. state of New York. It is located in the town of Shandaken in Ulster County. While the 4,180-foot (1,270 m) contour line on topographic maps is generally accepted as its height, the exact elevation of the summit has never been officially determined by the U.S. Coast and Geodetic Survey, and many informal surveys suggest the mountain may actually top 4,200 feet above sea level.
The Slide Mountain Wilderness Area is, at 47,500 acres (19,200 ha), the largest tract of state-owned Forest Preserve in New York's Catskill Park, and the largest area under any kind of wilderness area protection between the Adirondacks and the southern Appalachians. It is located in the towns of Shandaken, Denning and Olive in Ulster County.
Stony Clove Notch is a narrow pass, roughly 2,220 feet in elevation located in the Town of Hunter in Greene County, New York, deep in the Catskill Mountains. It is traversed by New York State Route 214, although in the past the Ulster and Delaware Railroad went through it as well.
Esopus Creek is a 65.4-mile-long (105.3 km) tributary of the Hudson River that drains the east-central Catskill Mountains in the U.S. state of New York. From its source at Winnisook Lake on the slopes of Slide Mountain, the Catskills' highest peak, it flows across Ulster County to the Hudson at Saugerties. Many tributaries extend its watershed into neighboring Greene County and a small portion of Delaware County. Midway along its length, it is impounded at Olive Bridge to create Ashokan Reservoir, the first of several built in the Catskills as part of New York City's water supply system. Its own flow is supplemented 13 miles (21 km) above the reservoir by the Shandaken Tunnel, which carries water from the city's Schoharie Reservoir into the creek.
Kaaterskill High Peak is one of the Catskill Mountains, located in the Town of Hunter in Greene County, New York, United States. It was once believed to be the highest peak in the entire range, but its summit, at 3,655 feet in elevation, places it only 23rd among the Catskill High Peaks. It is, however, the fourth most prominent peak in the range. Due to its situation as the easternmost High Peak, its summit is just outside the watersheds of New York City's reservoirs in the region.
Rusk Mountain is a peak located in the towns of Jewett and Lexington in Greene County, New York, United States. At 3,680 feet in elevation, it is the 20th-highest peak in the Catskill Mountains and considered a member of the Catskill High Peaks. While there is no maintained trail, a bushwhack to the summit is considered relatively easy, and required for membership in the Catskill Mountain 3500 Club.
Panther Mountain is one of the Catskill High Peaks, located in the Town of Shandaken in Ulster County, New York. At approximately 3,720 feet (1,130 m) in elevation, it is the 18th highest in the range. A combination of factors has led some geologists to believe the mountain is on the site of an ancient meteorite impact crater.
The Hunter Mountain Fire Tower is located on the summit of the eponymous mountain, second highest of the Catskill Mountains in the U.S. state of New York. It was the first of 23 fire lookout towers built by the state in the region, and the next-to-last of the five still standing to be abandoned.
Halcott Mountain is one of the Catskill Mountains of the U.S. state of New York. It is mostly located in Greene County, with some of its lower slopes in Delaware and Ulster counties. Its exact summit elevation has not been officially determined, but the highest contour line on the mountain is 3,520 feet (1,070 m). It is one of the peaks on the divide between the Delaware and Hudson watersheds.
Balsam Mountain is one of the High Peaks of the Catskill Mountains in the U.S. state of New York. Its exact height has not been determined, so the highest contour line, 3,600 feet (1,100 m), is usually given as its elevation. It is located in western Ulster County, on the divide between the Hudson and Delaware watersheds. The summit and western slopes of the peak are within the Town of Hardenburgh and its eastern slopes are in Shandaken. The small community of Oliverea is near its base on that side. Most of the mountain is publicly owned, managed by the New York State Department of Environmental Conservation as part of the state Forest Preserve, part of the Big Indian-Beaverkill Range Wilderness Area in the Catskill Park. The summit is on a small corner of private land.
Balsam Lake Mountain is one of the Catskill Mountains, located in the Town of Hardenburgh, New York, United States. It is the westernmost of the range's 35 High Peaks. Its exact height has not been determined, but the highest contour line on topographic maps, 3,720 feet (1,130 m), is usually given as its elevation.
Graham Mountain is the seventh highest of the Catskill High Peaks and the highest privately owned mountain in the range. It is located in the town of Hardenburgh, New York, United States.
The Red Hill Fire Observation Station consists of a fire lookout tower, cabin and pit privy located on the summit of Red Hill, a 2,990-foot (910 m) Catskill Mountain peak in Denning, New York, United States. It is the southernmost fire tower in the Catskill Park.
The Catskill Escarpment, often referred to locally as just the Escarpment or the Great Wall of Manitou, and known as the Catskill Front to geologists, is the range forming the northeastern corner of the Catskill Mountains in Greene and Ulster counties in the U.S. state of New York. It rises very abruptly from the Hudson Valley to summits above 3,000 feet (910 m) in elevation, including three of the Catskill High Peaks, with almost no foothills. The plateau to the south and west averages 2,000 feet (610 m) above sea level.
The Catskill Mountain fire towers were constructed to facilitate forest fire prevention and control in the Catskill Mountains of New York. 23 towers were built between 1908 and 1950. The towers fell into disuse by the 1970s as fire spotting from airplanes became more effective, and were gradually decommissioned. The Hunter Mountain Fire Tower was the last to be taken out of service in 1990. Most of the towers have been dismantled, but the five remaining towers have been renovated and opened to the public for observation: the aforementioned Hunter Mountain tower, the Balsam Lake Mountain Fire Observation Station, Overlook Mountain Tower in Woodstock, Tremper Mountain Fire Tower in the town of Shandaken and Red Hill Fire Tower in the town of Denning.
The Balsam Lake Mountain Fire Observation Station is located at the summit of the mountain of that name in the Town of Hardenburgh, New York, United States. It comprises a steel frame fire lookout tower, the observer's cabin and privy and the jeep road to the complex.
Deep Notch, sometimes West Kill Notch, or Echo Notch, is a mountain pass in Lexington, New York, United States. It divides two Catskill peaks, both subpeaks of high peaks of the range. The narrow groove between the steep, high slopes on either side is traversed by state highway NY 42 and the Shandaken Tunnel, part of the New York City water supply system. It has been called "striking" and "a marvel of grandeur and beauty".