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[[File:Sterns_20180325.jpg|thumb|300px|right| The telegraph pole at Sterns (spring)]]'''Sterns''' is situated between [[Hampton Loade]] and [[Bridgnorth]] at the foot of [[Eardington Bank]], at approximately [[Gradient profile and mileages|milepost 147]]. It is at a place where the [[River Severn]] approaches close to the railway at almost 90 degrees before turning away southwards towards Bewdley, and is notorious as a maintenance trouble spot due to the ground regularly slipping towards the river on numerous occasions over the history of the railway. During the last Ice Age, the valley of the River Severn was scoured out by glacial action and bands of different types of material were deposited at varying depths. This subsequently resulted in the formation of 'slip-planes' where the different layers can slide over each other, particularly when placed under a load such as the presence of a railway line and especially after periods of heavy rain. Slip-planes exist throughout most of the valley but have resulted in areas of majorinstability major instability at [[Jackfield Halt|Jackfield]] and Sterns.<ref name=Sowden>[[Bibliography#Books|Sowden (2012)]] pp. 12-14.</ref>