Jug Rock is a natural geological formation located outside of Shoals, Indiana, in the valley of the East Fork of the White River. It is composed of sandstone, and is the largest free-standing table rock formation in the United States east of the Mississippi River. It is part of the Mansfield formation, laid down in the Pennsylvanian geological epoch, roughly 325 to 286 million years ago. Erosion along fracture lines separated it from a nearby cliff. A companion feature, House Rock, stands opposite Jug Rock.
Mount Sopris is a twin-summit mountain in the northwestern Elk Mountains range of the Rocky Mountains of North America. The prominent 12,965-foot (3,952 m) mountain is located in the Maroon Bells-Snowmass Wilderness of White River National Forest, 6.6 miles (10.7 km) north by northeast of the community of Redstone in Pitkin County, Colorado, United States.
The West Elk Mountains are a high mountain range in the west-central part of the U.S. state of Colorado. They lie primarily within the Gunnison National Forest, and part of the range is protected as the West Elk Wilderness. The range is primarily located in Gunnison County, with small parts in eastern Delta and Montrose counties.
Camelback Mountain or Big Pocono is a conspicuous geographic feature on the Pocono Plateau. It is not a mountain, but rather a peninsular section of the Pocono Plateau, that when viewed from three sides, appears to be a mountain. The summit of Big Pocono "Mountain" is actually nearly level with land to the west and northwest, together comprising the top of the Glaciated Pocono Plateau, which is part of the larger Allegheny Plateau.
Martin Hill is a mountain ridge which connects Tussey Mountain to its east and Evitts Mountain to its west. Martin Hill is located in the Martin Hill Wild Area, which is a part of the Buchanan State Forest, in Bedford County, Pennsylvania, United States. The summit of Martin Hill is one of the few in the Commonwealth which is void of any towers or transmitters; such equipment is located instead on a lesser nearby summit in the same mountain complex. Martin Hill is the second highest in Pennsylvania's Ridge and Valley Appalachians, the highest being Wills Mountain to its west at 2,780 ft (850 m).
Bradley Mountain, 700 feet (210 m), is a traprock mountain located 3 miles (5 km) west of New Britain, Connecticut, United States, in the towns of Southington and Plainville. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. Bradley Mountain, popular as an outdoor recreation destination in the metropolitan Hartford/ New Britain area, is known for its clifftop scenic vistas overlooking Plainville Reservoir, unique microclimate ecosystems, and rare plant communities. Bradley Mountain is traversed by the 62.7-mile (101 km) Metacomet Trail.
Rattlesnake Mountain is a traprock mountain, 750 feet (230 m) above sea level, located 9 miles (14 km) southwest of Hartford, Connecticut in the town of Farmington. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. Rattlesnake Mountain, a popular outdoor recreation resource of the metropolitan Hartford area, is known for its cliff-top scenic vistas, unique microclimate ecosystems, and rare plant communities. Will Warren's Den, a boulder cave located on the mountain, is a local historic site. Rattlesnake Mountain is traversed by the 51-mile (82 km) Metacomet Trail.
Pinnacle Rock, 600 feet (180 m), is a traprock mountain peak located 10 miles (16 km) southwest of Hartford, Connecticut in the towns of Farmington and Plainville. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. Pinnacle Rock, popular as an outdoor recreation destination in the metropolitan Hartford area, is known for its clifftop scenic vistas, unique microclimate ecosystems, rare plant communities, and as a seasonal raptor migration path. Pinnacle Rock is traversed by the 51-mile (82 km) Metacomet Trail.
Parnell Knob is a mountain in the Ridge and Valley Appalachians region of south central Pennsylvania. This knob rises above the village of St. Thomas, where Front Mountain and Broad mountain come together. It is a feature sculptured by the hard dense Tuscarora quartzite of the Silurian age. Parnell Knob is conspicuous in that it rises abruptly above the relatively level Great Appalachian Valley.
Cross Mountain is the highest peak in the Bear Pond Mountains, a sub range of the Appalachian Mountains. This grouping of mountains straddle the Maryland and Pennsylvania border.
Mt. Pisgah is a peak located in northeastern Pennsylvania's Glaciated Low Plateau region, also known as the Endless Mountains. The mountain peak lies next to a state park named after the mountain, Mt. Pisgah State Park. There is a hiking trail to the summit that has a view of the surrounding countryside, 1,000 feet (305 m) feet below. Stephen Foster lake is also located at the base of the mountain.
The Bear Pond Mountains are a sub-range in the Appalachian Mountains, that straddle Pennsylvania and Maryland in the United States. These mountains are a part of the Ridge and Valley Appalachians and reach their highest point at Cross Mountain (Pennsylvania) 2,062 feet (628 m). A unique geologic feature known as the "Punchbowl" occurs in this range. This feature was created by the weathered shales of the Ordovician age in the center of a south-plunging anticline, having been eroded to expose a large amphitheater-like feature (punchbowl). Cross and Hearthstone Mountain are made of hard resistant quartzite of the Tuscarora Formation of the Silurian age, which form the walls of the bowl.
Miller Mountain is a peak located in Wyoming County, Pennsylvania. This mountain is one of the more recognizable peaks in the Endless Mountains region of the Commonwealth. Miller Mountain is a "stand alone" peak from the rest of the Allegheny Plateau. The Susquehanna River flows past the mountain where the slopes rise to over 1,600 feet (490 m) above the river banks and the town of Tunkhannock.
Mount Ararat is a mountain located in the Pennsylvania villages of Belmont Corners and Orson. Its summit, which is in Orson, is the highest point in Wayne County, Pennsylvania, and one of the higher points in eastern Pennsylvania. Mount Ararat is located in the Glaciated Low Plateaus geological section of Pennsylvania. This section is characterized with low rolling hills and modest relief. This summit is of low relief but stands as a peak above the countryside.
Rays Hill is a mountain ridge in Pennsylvania's Ridge and Valley Appalachians region. It is bordered to the east by Sideling Hill. About halfway along its run, the west side of Rays Hill ties into Broad Top Mountain, a large plateau. On its west it is bordered by Tussey Mountain south of Broad Top Mountain and Rocky Ridge north of Broad Top Mountain.
Forkston Mountain is a mountain located in Wyoming County, Pennsylvania. This mountain is located in the region of Pennsylvania known as the Endless Mountains. Forkston Mountain is a part of the Allegheny Plateau and rises over the Susquehanna River. Forkston Mountain has a fire tower located at the summit.
Osterhout Mountain is a summit located in Wyoming County, Pennsylvania. Osterhout is located on the east bank of the Susquehanna River opposite its sister peak Miller Mountain. The mountain has communication towers on its summit and rises over the town of Tunkhannock Pennsylvania.
Albert Mountain is a mountain in North Carolina's Nantahala Range of the Appalachian Mountains. The Appalachian Trail goes along its summit, which is around 5,200 feet (1,600 m) high. A fire tower offers views of the Blue Ridge and the Little Tennessee River valley.
Pisgah Mountain or Pisgah Ridge is a ridgeline running 12.5 miles (20.1 km) from Tamaqua to Jim Thorpe, Pennsylvania. It is oriented north-northeast to south-southwest, and its north-side valley is followed by U.S. Route 209 from river gap to river gap. The ridge is a succession of peaks exceeding 1,440 feet (438.9 m) rising 300 to 540 feet above the boroughs of Lansford, Coaldale, and Tamaqua in the Panther Creek valley. The highest point on Pisgah Mountain is at 1,611 feet (491 m) in the borough of Summit Hill, which sits atop the ridge. Near Summit Hill was the "Sharpe Mountain" (peak) where in 1791 Phillip Ginter is documented as having discovered anthracite, leading to the formation of the Lehigh Coal Mine Company. In 1818 the Lehigh Coal Company took over the mines, and the mining camp gradually became a settlement and grew into Summit Hill.
Haystack Mountain (Pennsylvania), is an otherwise non-descript 1871 ft peak forming the steep southwestern faces of the Solomon Gap mountain pass's saddle connecting and dividing the Wyoming Valley from the Lehigh Valley.
