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Bellefonte Formation : ウィキペディア英語版 | Bellefonte Formation __NOTOC__ The Ordovician Bellefonte Formation (Obf) is a mapped bedrock unit in central Pennsylvania. ==Description== The Bellefonte is defined as a medium-gray, brownish-weathering, medium-bedded dolomite and minor sandstone. The very fine grained Tea Creek Member lies above, and the crystalline Coffee Run Member lies below.〔
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Bellefonte Formation」の詳細全文を読む
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