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Villa DeSales, built in 1877–1878, is a large five-by-three bay, three-story frame High Victorian Gothic dwelling with a two-story south service wing, located at Aquasco, Prince George's County, Maryland. The historic home is significant for its architectural character which includes a complex of six 19th century outbuildings.
A ravine is a landform that is narrower than a canyon and is often the product of streambank erosion. Ravines are typically classified as larger in scale than gullies, although smaller than valleys. [1] Ravines may also be called a cleuch, dell, ghout , gill or ghyll, glen, gorge, kloof (South Africa), and chine (Isle of Wight)
Canyon / Gorge – Deep chasm between cliffs; Chine – Steep-sided river valley; Couloir – Steep, narrow mountain gully; Defile (geography) – Narrow pass or gorge between mountains or hills; Gully – Landform created by running water and/or mass movement eroding sharply into soil; Mountain pass – Route through a mountain range or over a ...
Villa Anneslie is a historic home located at Towson, Baltimore County, Maryland, United States. It was built about 1855 as a summer home. Designed by architect John Rudolph Niernsee, it is an Italianate two-story villa built in brick and covered in clapboard. It features an asymmetrical design with a central three story tower over the entrance.
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Canyon – Deep chasm between cliffs, includes gorge. Dale (landform) – Open valley; Coulee – Type of valley or drainage zone; Gully – Landform created by running water and/or mass movement eroding sharply into soil; Ravine – Small valley, often due to stream erosion; Valley – Low area between hills, often with a river running through it
The Shaw Mansion is an Italianate style house in the George's Creek Valley of Allegany County, Maryland, built in 1872.The house is significant as an unusually large and well-preserved example of the style for its area, with stone trim, detailed brick bonding, cast-iron mantels and much of the original interior woodwork.
Look from Paria View to a valley in Bryce Canyon, Utah, with very striking shoulders. Depending on the topography, the rock types, and the climate, a variety of transitional forms between V-, U- and plain [clarification needed] valleys can form. The floor or bottom of these valleys can be broad or narrow, but all valleys have a shoulder.