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E. J. Loomis The building was formally Loomis School. Formally part of the building was also used as the university's daycare. Today it is home the university's Communications Arts and Science College. The building is slated to be removed in the University's master plan. E. J. Loomis was an 1890 BW graduate and became the mathematics chair in 1885.
Location of Morgan County in Ohio. This is a list of the National Register of Historic Places listings in Morgan County, Ohio. It is intended to be a complete list of the properties and districts on the National Register of Historic Places in Morgan County, Ohio, United States. The locations of National Register properties and districts for ...
Loomis Observatory (also known as the Elias Loomis Observatory) is the second oldest observatory in the United States, located in Hudson, Ohio. Construction was completed in 1838. It is on the campus of Western Reserve Academy, a college preparatory school.
At Ascend Erie climbing gym, employee Wade Desai, 35, helps check routes on the 52-foot wall in Erie on Nov. 2, 2023. The long-anticipated new gym opens to the public on Nov. 6. Rock climbers have ...
A climbing wall is an artificially constructed wall with manufactured grips (or "holds") for the hands and feet. Most walls are located indoors, and climbing on such walls is often termed indoor climbing. Some walls are brick or wooden constructions but on modern walls, the material most often used is a thick multiplex board with holes drilled ...
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Buildings and structures designed by Morgan, Walls & Clements — an architecture firm active from the 1890s through 1930s in California. The regionally prominent design studio was based in Los Angeles, and was responsible for many of the city's landmarks. Architect Stiles O. Clements was a design partner from c.1910 to 1937.
Mary Campbell Cave, also known as Old Maid's Kitchen, is a small secondary rock shelter in Cuyahoga Falls, Ohio. The cliff and cave roof are sandstone of the Sharon Formation, while the cave wall is shale of the Meadville formation. The cavity in the cliff was formed when water passing through the porous sandstone eroded the shale, leaving a ...