- right Laverton Brook - max 86 m/s (3,037 cu ft/s) Source Cleeve Hill Country United Kingdom | - average 0.66 m/s (23 cu ft/s) Basin area 95 km² Mouth River Avon, Warwickshire | |
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- location Cotswolds, Gloucestershire - location Hampton, Worcestershire | ||
The River Isbourne is 14 mile (22km) long tributary of the River Avon which flows through Gloucestershire and Worcestershire in the Midlands of England.
Contents
Map of River Isbourne, United Kingdom
CourseEdit
The source of the river is a series of springs that occur on the northern flank of Cleeve Hill, on the edge of the Cotswold Hills. These springs occur where the permeable Jurassic limestone, meets the impermeable Upper Lias mudstone and clays that underlie most of the Isbourne catchment.
The river flows from Cleeve Hill in a steep valley in a northerly direction through the hamlet of Postlip, before reaching the town of Winchcombe which it passes along its eastern side. Beyond the town, it continues northwards to Toddington, through the grounds of Toddington Manor, and then past the village of Wormington. The river then crosses into Worcestershire and is joined by the Laverton brook, before it reaches the village of Sedgeberrow. Flowing directly north the Isbourne passes through the village of Hinton on the Green, it then continues through an area of market gardens on the outskirts of Evesham, and passes under the Pershore road, before joining the River Avon near Hampton.
CatchmentEdit
The Isbourne catchment covers an area of 125 square kilometres (48 sq mi) and lies between the Badsey Brook to the east, the Merry Brook and Carrant Brook to the west with the Cotswolds to the south. It has an average annual rainfall of 704 millimetres (27.7 in), which is somewhat drier than the average for England at 828 millimetres (32.6 in).
Land use in the catchment is predominantly rural, with 80 percent made up from a mixture of arable, horticulture and pasture; the remainder being woodland, with a minor fraction of urbanised area of less than 2 percent.
In terms of geology, apart from the headwaters which are underlain by the Cotswold limestone, the majority of catchment is Lias clay. This impermeable clay means that Isbourne can become responsive in terms of runoff to heavy rainfall events.
FloodingEdit
The Isbourne has a history of flooding along its course, especially in Sedgeberrow, the most recent occasion being in summer 2007.