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The Penn State University main campus hosts the agricultural sciences as well as the information technology Schools of Excellence. Participants are required to be Pennsylvania high school students who have just completed their sophomore or junior years. Admission into the program is selective with sixty-four available spots.
These mountains are steep-sided and valleys are canoe-shaped, largely due to the area's complex folded structure. Most of the coal being mined from this section is from the Pennsylvanian-aged formations. Along with the Mazon Creek fossil field in Illinois, a tremendous amount of plant fossils has been studied from this area. [13]
Some of Pennsylvania's most important fossil finds were made in the state's Devonian rocks. [2] Carboniferous Pennsylvania was a swampy environment covered by a wide variety of plants. The latter half of the period was called the Pennsylvanian in honor of the state's rich contemporary rock record. By the end of the Paleozoic the state was no ...
Fossil of the Middle-Late Ordovician giant trilobite Isotelus. †Isotelus †Isotelus gigas †Kiaeropterus †Kingstonia †Kladognathus †Kootenia †Kutorgina †Lancastria †Langlieria †L. radiatus – type locality for species †L. smalingi – type locality for species [2] †Lepidostrobus †Leptomitus †Lenisicaris
Outcrop of the Devonian Catskill Formation with a well-displayed thrust fault, located about 3 miles west of the village of Juniata Crossing on the north side of Route 30, Bedford County, Pennsylvania. Fossil coral of the Devonian Keyser Formation in the New Enterprise New Paris Quarry, Chestnut Ridge Bedford County, Pennsylvania.
Farmer High School and also known as the Old Main. In 1855, before the Penn State College of Agricultural Sciences, it was a high school known as The Farmer's High School run by Evan Pugh. Pugh helped to transform the Farmer's High School into the Penn State College of Agricultural Sciences by supporting Congress to pass the Morrill Land-Grant Act.