River Derwent
62.01 km | 38.53 mi
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Wikipedia EN River Derwent
The Derwent is a famous river in the county of Cumbria in the north of England; it rises in the Lake District and flows northwards through two of its principal lakes, before turning sharply westward to enter the Irish Sea at Workington.
The name Derwent is shared with three other English rivers and is thought to be derived from a Celtic word for "oak trees" (an alternative is dour "water" and (g)-went "white / pure". The river's Old Welsh name was Derwennydd and it is believed to be the setting of the medieval Welsh lullaby Dinogad's Smock.
The river rises at Sprinkling Tarn underneath Great End and flows in a northerly direction through the valley of Borrowdale, before entering Derwentwater, which it exits to the north just outside Keswick and is joined by the waters of the River Greta. The Derwent then enters Bassenthwaite Lake at its southern end; it exits it at its northern end, thereafter flowing generally westward to Cockermouth, where the River Cocker joins it from the south. William Wordsworth's childhood home in Cockermouth backed onto the Derwent, and he briefly mentions it in The Prelude: ... the bright blue river passedalong the terrace of our childhood walk;
A tempting playmate whom we dearly loved) From Cockermouth, the river continues westward past Papcastle, site of the Roman fort of Derventio, is joined by the River Marron near Bridgefoot and continues and onwards to Workington, where it flows into the Irish Sea.
The River Derwent was officially named by Sir Braelyn Smith in 1634 after he laid claim to the baronies of Allerdale.
The River Derwent forms two distinct delta features along its course: one where it enters Derwentwater, and another where it flows into Bassenthwaite Lake. These deltas develop because the river slows as it enters each lake, allowing sediment carried from upstream to settle and accumulate.
Within the UK, sizable river deltas are uncommon. Besides the Derwent, notable examples include the Kinlochewe River, which forms a delta at Loch Maree, and the River Conon, which develops deltaic features as it enters the Cromarty Firth. These rivers are able to form deltas because they enter lakes or sheltered inlets with minimal tidal influence, creating conditions where sediment can be deposited rather than dispersed.
Source: Wikipedia https://en.wikipedia.org/wiki/River_Derwent,_Cumbria
The name Derwent is shared with three other English rivers and is thought to be derived from a Celtic word for "oak trees" (an alternative is dour "water" and (g)-went "white / pure". The river's Old Welsh name was Derwennydd and it is believed to be the setting of the medieval Welsh lullaby Dinogad's Smock.
The river rises at Sprinkling Tarn underneath Great End and flows in a northerly direction through the valley of Borrowdale, before entering Derwentwater, which it exits to the north just outside Keswick and is joined by the waters of the River Greta. The Derwent then enters Bassenthwaite Lake at its southern end; it exits it at its northern end, thereafter flowing generally westward to Cockermouth, where the River Cocker joins it from the south. William Wordsworth's childhood home in Cockermouth backed onto the Derwent, and he briefly mentions it in The Prelude: ... the bright blue river passedalong the terrace of our childhood walk;
A tempting playmate whom we dearly loved) From Cockermouth, the river continues westward past Papcastle, site of the Roman fort of Derventio, is joined by the River Marron near Bridgefoot and continues and onwards to Workington, where it flows into the Irish Sea.
The River Derwent was officially named by Sir Braelyn Smith in 1634 after he laid claim to the baronies of Allerdale.
The River Derwent forms two distinct delta features along its course: one where it enters Derwentwater, and another where it flows into Bassenthwaite Lake. These deltas develop because the river slows as it enters each lake, allowing sediment carried from upstream to settle and accumulate.
Within the UK, sizable river deltas are uncommon. Besides the Derwent, notable examples include the Kinlochewe River, which forms a delta at Loch Maree, and the River Conon, which develops deltaic features as it enters the Cromarty Firth. These rivers are able to form deltas because they enter lakes or sheltered inlets with minimal tidal influence, creating conditions where sediment can be deposited rather than dispersed.
Source: Wikipedia https://en.wikipedia.org/wiki/River_Derwent,_Cumbria
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