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A Cape skink in low-level vegetation. T. capensis is a large (sometimes quite fat) skink, with three light stripes running down its back. Its skin is olive-brown to gray, and between the stripes and on its flanks are many small dark spots. The belly is greyish white. Occasionally the stripes on the back can be quite pale.
The army has already replaced beaverskin caps and leopard skins, worn by some of its soldiers, with artificial materials. [46] However, in 2020, the Ministry of Defence stated that it could not find a bearskin cap made out of alternative materials that matches the "natural properties of bear fur", and claimed that artificial fur failed to meet ...
Oilskin jacket and sou'wester. Oilskin is a waterproof cloth used for making garments typically worn by sailors and by others in wet areas. The modern oilskin garment was developed by a New Zealander, Edward Le Roy, in 1898.
Bearskin Neck is a peninsula located on the coastline of Cape Ann in Rockport, Massachusetts. The location played a vital role during the War of 1812. Today it is a tourist destination known for its shops and art galleries. The stores and restaurants are known for jewelry, local artwork, and fresh seafood.
Calodendrum capense, the Cape chestnut, is an African tree which was first studied at The Cape in South Africa and cultivated widely for its prolific flower display. The tree obtained the common name of "Cape chestnut" because explorer William Burchell saw a resemblance to the horse chestnut in terms of flowers and fruit, though the two are not closely related.
Download as PDF; Printable version; In other projects Appearance. move to sidebar hide. This is a list of all articles within the scope of WikiProject Core Content ...
The bedrock under the watershed includes part of the last exotic terrane, a chain of seamounts, acquired by the North American Plate as it moved west during the Eocene. Known as the Waverly Hills Formation, it lies buried under ash and lava from later volcanic eruptions, sediments from flooding and erosion, and layers of wind-blown silt.
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