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A pyramidal peak, sometimes in its most extreme form called a glacial horn, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point.hese horns are a common shape for mountain tops in highly glaciated areas. The number of faces of a horn depends on the number of cirques involved in the formation of the peak: three to four is most common. Horns with more than four faces include the Weissmies and the Moench. mÃ¶nch
The soft substance filling the medullary cavities and cancellous extremities of the long bones. Surgery, with Special Reference to Podiatry Maximilian Stern Bone may be compact, or loose and spongy in character, when it is known as cancellous bone. These horn cores are formed internally of cancellous bone, and on them the true epidermal horns are borne. The tympanic is not fused to the periotic and has a small bulla not filled with cancellous bone. The Vertebrate Skeleton Sidney H. Reynolds The spongy or cancellous osteoma is really an ossified chondroma, and is met with at the ends of the long bones (Fig. 52).