Cockermouth History
Flooding occurred after three days of almost continuous rain with a fall of 4 inches in the Keswick area and more than double that in the Borrowdale valley. Nearly 3 inches fell in one day at Keswick and 6 inches in Borrowdale. In Borrowdale it was said to be the highest flood for 36 years (Cumberland News) and more generally the Carlisle Journal reported that the floods were the most extensive experienced for over 40 years in the area between Keswick and the coast.
Low-lying land between Thirlmere and Keswick was inundated as Thirlmere overflowed. The Greta at Keswick threatened to overflow but it fell short by a few inches and there was no serious flooding there.
With the highest rainfall over Borrowdale, Derwentwater and Bassenthwaite were said to be the biggest and highest ever known having become one lake The water was up to the edge of the pathway down to Friar’s Crag. Boat landings and sheds and their contents were washed into the lake. The boathouse on Derwent Island was almost submerged. Downstream, the River Derwent overflowed at Portinscale Bridge and at Braithwaite Bridge and in the main road in both places was 2 to 3 feet under water.
The main damage was done however downstream at Cockermouth from the sequential effects of the Derwent and Cocker. The Cocker rose rapidly on Friday 16th, then subsided but later rose again to a peak around 0400 on 17th, flowing over the Barrel Bridge and into the houses on High Sand Lane. During the 17th the Derwent started to rise and between 2300 on 17th and 0100 on 18th it overflowed and rushed down streets finishing up with 3 feet of water at the junction of Main Street and Sand Lane. The Main Street was inundated to a depth of 2 feet for 300 yards. It was in the Globe Hotel to a depth of 8 inches. In side streets and alleys over 100 houses were completely isolated, and in some ‘it was barely a foot from the ceilings of the kitchens and parlours’. ‘It went up Lindsey’s yard and Irving’s court like a torrent’ . In the thoroughfare behind Main Street on the banks of the Derwent, water flowed like a millrace and inhabitants were confined to upper rooms. Houses in High Sand Lane and Waterloo Street were flooded to half way up their windows.
Two hundred people in the area known as The Goat were marooned. Sandair cricket field was under water eight feet deep and the rugby field was little better. All roads into the town were impassable for more than an hour.
Four photographs which appeared in the Cumberland News are reproduced as Figure 3. Two photographs from Bradbury (1995) show the River Cocker again overtopping the Barrel bridge are reproduced as Figure 4 and 5. Figures 6, 7 and 8 (again from Bradbury, 1995) show Cockermouth Main Street looking towards the Mayo statue, a fisherman in the Main Street and the River Cocker taking a short cut down South Street, looking towards Quaker Bridge.
Although both Cocker and Derwent caused flooding it was the effects of the River Derwent which were more serious during this event.
The river Derwent caused damage to land and property in the Great Broughton district, inundating several hundred acres of land. A house at the Penny Bridge Great Broughton was surrounded and the road from Great Broughton to the main Cockermouth Workington road was impassable at Stoneybeck Lane. The roads from Great Broughton to Ribton and Camerton were also flooded several feet deep in places. At Carr Meadow the footpath to Camerton Parish Church had water spread over 100 yards. At Salmon Hall the water reached the top of the railway fencing. At Workington it inundated the Mill Field and flooded houses in Park View to a depth of one foot.
Flooding also occurred in Carlisle from the River Eden but more unusually also at the Maryport suburb of Grasslot from a small channel. Sixty houses and several shops were flooded and only two streets were unaffected. Floods were unknown there to ‘all residents under 40 years of age’.
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