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Worcester break 7.

As mentioned earlier in the week there is what I call a ‘hutment colony’, although now mostly caravans, near Camp House (s.p.b.s) beside the River Severn. The photo shows one substantial hutment. Hutment ‘colonies’ often developed after the Great War in the 1920s, sometimes earlier, in an age before strict planning regulations came into force. […]

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Worcester break 6.

At the Camp House (s.p.b.s) the waters of the River Severn are always flowing downstream, the extent of the tidal impact on the flow of the River being from the Severn Estuary upstream to Gloucester. The Severn Bore, a moving wave pushing upstream, also does not reach Worcester. The ‘Bore’ results from spring-tides pushing water

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Worcester break 5.

Although I have no definative evidence I think that, in this part of Worcestershire at least, the River Severn has an incised river valley. This means that the original river valley is left ‘high and dry’ when changes in sea level or earth movements cause the river to start eroding a new river valey within

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Worcester break 3.

Today’s photo shows the hillside beside the lane leading from Hallow, past the ‘cottage’, to Camp House (s.p.b.), the lower part of the hillside showing a ripple-effect in the topsoil. These don’t qualify as ‘linchets’ (lynchets) as the bedrock isn’t chalk but are they a natural feature or evidence of past man-made terracing? I would

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