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hogback

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hogback, sharp-crested ridge with steep slopes on both sides, formed by the erosion of steeply tilted rock layers. Hogbacks are commonly formed along the eroded flanks of large, tightly folded anticlines and synclines (see fold fold, in geology, bent or deformed arrangement of stratified rocks. These rocks may be of sedimentary or volcanic origin. Although stratified rocks are normally deposited on the earth's surface in horizontal layers (see stratification), they are often found inclined
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). Impressive hogbacks are seen in the foothills east of the Front Range of the Rocky Mts. in Colorado, where they are formed by the vertical or steeply dipping layers of Dakota sandstone. This region forms the intake area for the Dakota artesian system. Hogbacks are also common in the Black Hills of South Dakota where sedimentary rocks were uplifted by the intrusion of Black Hills granite. See cuesta cuesta , asymmetric ridge characterized by a short, steep escarpment on one side, and a long, gentle slope on the other. The steep side exposes the edge of erosion-resistant rock layers that form the cuestas.
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.
hogback [′häg‚bak]
(geology)
Alternate ridges and ravines in certain areas of mountains, caused by erosive action of mountain torrents.


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Price includes: return flights from Heathrow to New York, time to soak up those vivid fall colours, including a full-day tour through Vermont, taking in Quechee Gorge, quintessential Woodstock and Hogback Mountain.
Old Macdonald, on the other hand, is set mostly in a huge bowl between a fore dune along the beach and the large inland sand hogback that runs the length of the Bandon Dunes property.
One exception is Valley Curtain in Rifle, Colorado, between Grand Junction and Glenwood Spring, where a group of workers fastened an orange curtain made of woven nylon fabric in the Grand Hogback Mountain Range.
 
 
 
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