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Tussey Mountain (ski resort)

Buildings and structures in Centre County, PennsylvaniaSki areas and resorts in PennsylvaniaTourist attractions in Centre County, Pennsylvania

Tussey Mountain is a ski resort and all-seasons recreation area located in Boalsburg, Centre County, Pennsylvania, near State College and Penn State University and is the gateway to the Rothrock State Forest. Tussey Mountain includes the Tussey Mountain Amphitheater for concerts and festivals, a Lodge for weddings and parties, and a Fun Centre that offers go-karts, mini-golf, batting cages, a skate park, driving range and a par 3 golf course. Discounted rates are offered for students of Penn State University. In the winter season, Tussey Mountain has 14 trails, with the longest one being about 3/4 of a mile. The top elevation at Tussey Mountain is 1,819 feet (554 m), and there are 38 acres (150,000 m2) skiable at the Tussey Mountain Ski Area.

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Tussey Mountain (ski resort)
Bear Meadows Road,

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Latitude Longitude
N 40.7682 ° E -77.752 °
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Bear Meadows Road
16827
Pennsylvania, United States
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Linden Hall Historic District
Linden Hall Historic District

The Linden Hall Historic District is located in Linden Hall, Harris Township, Centre County, Pennsylvania, U.S. The district was added to the National Register of Historic Places in 1990. The district incorporates the historic village of Linden Hall, which dates from the late 1700s. The resources within the district, which total 33 structures, range in date from 1810 to 1919. The district represents an excellent collection of diverse 19th and early 20th century vernacular dwelling styles representative of small rural villages in central Pennsylvania. Linden Hall is one of the oldest continually inhabited communities in western Penns Valley and closely resembles in its scale and mix of resources, other local villages which evolved around mills established in the early 19th century.The town originally developed as a mill site along Cedar Run around 1800. The village expanded northward from the mill site throughout the 19th century. Though never very large, Linden Hall reached its greatest extent around the turn of the century. A train station was added to the village when the railroad was extended through the valley in 1885. Today, the early commercial enterprises are gone, robbing Linden Hall of a central focus and leaving gaps among the homes that remain. Major buildings include the Rock Hill School, the Evangelical Methodist Church and the Irvin residence. Homes are principally Victorian in style and are of frame construction. Although some are only one story in height, most range from two to two-and-a-half stories.

Clinton Group
Clinton Group

The Clinton Group (also referred to as the Clinton Formation or the Clinton Shale) is a mapped unit of sedimentary rock found throughout eastern North America. The interval was first defined by the geologist Lardner Vanuxem, who derived the name from the village of Clinton in Oneida County, New York where several well exposed outcrops of these strata can be found. The Clinton Group and its lateral equivalents extend throughout much of the Appalachian Foreland Basin, a major structural and depositional province extending from New York to Alabama. The term has been employed in Kentucky, Maryland, Michigan, New York, Ohio, Pennsylvania, Tennessee, Virginia, and West Virginia, though in many of these areas the same interval is referred to as the Rose Hill, Rockwood, or Red Mountain Formations. Historically the term "Clinton" has also been assigned to several lower Silurian stratigraphic units in Ohio and Kentucky which are now known to be significantly older than the Clinton Group as it was originally defined. Many parts of this succession are richly fossiliferous, making the Clinton Group an important record of marine life during the early Silurian. Several economically valuable rock-types are found within this interval, though it is perhaps best known as a significant source of iron ore Stratigraphically, the Clinton Group overlies the coarse siliciclastics of the Medina Group in New York, The Albion Group in the Subsurface of Ohio, the Clinch Sandstone in Virginia and West Virginia, and the Tuscarora Sandstone in Pennsylvania. It is overlain by the shales and carbonates of the Lockport Group in New York, the McKenzie Formation in Pennsylvania, and the Sneedville Limestone in Tennessee. Owing to the great difference in resistivity between the relatively soft, readily weathering Clinton Group and the massive dolomites of the overlying Lockport, the former tends to erode preferentially out from underneath the latter. This has resulted in the formation of numerous cateracts such as Niagara Falls and the High Falls of Rochester, New York which are but local manifestations of a regional geographic feature called the Niagara Escarpment.