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BY RIVER TO BANBURY?

机译:乘河到班伯里?

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To today's boaters heading south along the Oxford Canal, Banbury is the last main town they pass through before they reach Oxford. But historically it was once served not by canal but (in a somewhat rudimentary way) by river; in the canal age it very nearly became a junction between canal and navigable river; and the river still has an influence on the Banbury to Oxford length of the canal today. The River Cherwell rises near Hellidon, south west of Daventry (incidentally very close to the sources of both the Nene and the Learn - their waters ending up in the Thames, the Wash and the Severn respectively). From there it meanders southwards and westwards to reach Cropredy, merging with other streams so that by the time it gets to Banbury it's become a decent sized watercourse for the rest of its route southwards via King's Sutton, Upper and Lower Heyford and Thrupp to join the Thames just downstream of the city centre in Oxford. Sufficiently 'decent sized' that by the 17th century, a good 100 years before the start of the Canal Age, it was being considered as a possible navigation.
机译:对于今天沿着牛津运河向南航行的划船者来说,班伯里是他们在到达牛津之前经过的最后一个主要城镇。但从历史上看,它曾经不是通过运河,而是(以一种有点简陋的方式)通过河流服务;在运河时代,它几乎成为运河和通航河流之间的交汇处;这条河今天仍然对班伯里到牛津运河的长度有影响。切尔韦尔河(River Cherwell)发源于达文特里(Daventry)西南部的赫利顿(Hellidon)附近(顺便说一句,它非常靠近内内河和诺尔河的源头——它们的水分别汇入泰晤士河、沃什河和塞文河)。从那里它向南和向西蜿蜒到达克罗普雷迪,与其他溪流汇合,因此当它到达班伯里时,它已经成为一个相当大的水道,其余路线向南经过国王萨顿、上海福德和下海福德以及斯鲁普,在牛津市中心下游汇入泰晤士河。到17世纪,也就是运河时代开始前100年,它被认为是一种可能的航行方式。

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    《Canal boat》 |2022年第3期|51-52|共2页
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