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Cascading Waterfall was originally surveyed as part of the Smithsonian's Save Outdoor Sculpture! survey in 1994. The fountain, reminiscent of 16th century Italian villas, focuses primarily on thirteen large semi-circular basins forming a water cascade that overlooks the historic park. The fountains are the largest of their kind in the United ...
The Waterfall. The Gerald D. Hines Waterwall Park, [1] formerly the Williams Waterwall and the Transco Waterwall, is a multi-story sculptural fountain that sits opposite the south face of Williams Tower in the Uptown District of Houston. The fountain and its surrounding park were built as an architectural amenity to the adjacent tower.
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The Waterfall under the Brooklyn Bridge from the South Street Seaport The Waterfall at Pier 35. The sites chosen for the four waterfalls were the East River Esplanade's Pier 35 in Manhattan; beneath the Brooklyn Bridge in DUMBO between piers 4 and 5, also in Brooklyn; and Governors Island to activate spaces that typically were not. [4]
The decade from 1810 to 1819 was the coldest in England since the 17th century. In 1812, the French Grande Armée was forced to retreat from Moscow by the advancing winter – known to the Russians as General Snow. These climactic events played a great part in the development of a new art genre, the winter landscape. [6]
The sump can either be contained within the water feature, or buried underground (in the case of an outdoor water feature). A water feature may be indoor or outdoor and can range in size from a desk top water fountain to a large indoor waterfall that covers an entire wall in a large building, and can be made from any number of materials ...
The final study for the painting. Horseshoe Falls, Niagara, 1856–57, oil on two pieces of paper, 29.2 × 90.5 cm. Olana State Historic Site [1]. Niagara is an oil painting produced in 1857 by the American artist Frederic Edwin Church.
Ithaca Falls [1] is a waterfall located within the city of Ithaca, New York. It is the last of a series of waterfalls along the hanging valley formed where Fall Creek intersects the glacial trough of Cayuga Lake. The falls are in an amphitheater formed by freezing and thawing of the weak shale which makes up most of the gorge walls.
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