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Ox Close Wood - a historical background

机译:牛接近木-历史背景

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Ox Close lies by the River Wharfe in a landscape that must have changed very little in the preceding centuries (Fig.l). Positioned over a mile from the village centre, it was part of the common lands of East Keswick and used as a wooded pasture untilEnclosure at the beginning of the 19th century.Figure 1. Detail from a map in Vicaria Leodiensis: or the History of the Church ofLeedes in Yorkshire, Ralph Thoresby, 1724East Keswick has an interesting geology—the western side of the parish lies on Gritstone with overlying Boulder Clay, and to the east Magnesian Limestone. This mix makes Ox Close a very diverse habitat; it has rich alluvium by the river, a central bandof more acidic soil where there was once a conifer plantation and a substantial area on the limestone.
机译:Ox Close位于Wharfe河旁,其景观在过去几个世纪中变化很小(图1)。它位于距村庄中心一英里的地方,是东凯西克(East Keswick)普通土地的一部分,直到19世纪初被用作封闭地之前,一直被用作树木繁茂的牧场。图1. Vicaria Leodiensis地图的详细信息:或1724年,拉尔夫·托雷斯比,约克郡利兹教堂(Edward Church of Leedes),东凯西克(Keswick)有一个有趣的地质学-教区的西侧位于格里斯通(Gritstone)和上覆的博尔德(Boulder)粘土,并向东是镁质石灰石。这种混合使Ox Close成为一个非常多样化的栖息地。它在河边有丰富的冲积层,是较酸性土壤的中心带,那里曾经有针叶树人工林,石灰岩上有相当大的面积。

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