I have been accustomed to writing about hilly landscapes in the North and West of England and Wales, but this time I am going to discourse on the precise opposite, England's flattest land and some of its most-low-lying, land that is at points below sea-level, guarded from inundation by sea defences and intense drainage.This area is in the East of England, an area known as East Anglia.
If you look at the map below you will see a bay extending inland, which is called the Wash, wash being a geographical term for a shallow area of sand and mud.Extending southwards is an area of low-lying land drained, if that is a somewhat optimistic term, by several rivers. This flat marshy land is the Fens. The Wash was the tidal part of the Fens, the Fens being coastal marshes characterized by relatively high alkalinity and low nutrient levels.The reason for the wetness of the land is that it is low lying so river water travels but slowly over the surface and can if uncontrolled spread easily across the low-lying land, especially in Winter, when it is rainy
Historically the first attempt to control the water around the Wash was made by the Romans, who engineered some earthen sea defences, but the Romans left and as they went the economy of Britain slumped, as it had been built around sustaining high troop levels, and the incoming Angles [historically a tribe friendly to Rome] had not the resources to maintain them. It was only in the twelfth century that the Benedictine monks began to work on the creation of more effective defences that the fens began to be reclaimed for agriculture. The monks did a massive amount of work in turning Britain into the well-tilled land that it is, but they get little credit for it. One wonders why?
This is not to say that there were no people dwelling in the Fens, there were, for the land consisted of glacial islets on which people settled. Places such as Ely [Eel Island] and Anglesey [Angles Island] which is not to be confused with Anglesey in Wales, whose name has a different origin, are examples of such isles. Archaeologists have found remains of wooden footpaths made of laths of coppiced willows entombed in the preserving peat of Fenland deposits. These have been found in other marshy parts of Britain where residents wanted to walk dryshod from one island to another. It is also likely that some resident dwelt on crannogs, pile dwellings constructed on artificial islands in lakes, which were useful for defence against marauding neighbours [The Britons were not very friendly to each other!] One such site was at Must Farm where archaeologists found so many artefacts that were lost when crannnog was burned down, probably by marauders, that they dubbed it Britain's Pompeii.


Comments
frankbeswickJul 31, 2024
DerdriuMarrinerJul 31, 2024
Online sources associate a land-level rise in some places, such as (unspecified which countries of) Scandinavia, relieved of glacial- and ice-sheet weights.
Has such an occurrence happened in the part of highland Scotland without its once-permanent snow cover?
frankbeswickJul 31, 2024
DerdriuMarrinerJul 30, 2024
Online sources associate sea-level rise with warmer water temperatures that bring about water expansion beyond their original containment, whereby causing water to go the only way possible: upward.
They correlate apparent -- not actual -- sea-level decrease with land-level rise, the latter developing from land freed from glacier and ice sheets. They give the example of Scandinavia.
Is there any part of the British Isles so cold as to have glacial and ice sheets to melt?
frankbeswickJul 30, 2024
I know.
DerdriuMarrinerJul 29, 2024
Sea-level rise appears predominantly to arise from melting ice. Is there such a thing as sea-level decrease anywhere?
frankbeswickJul 27, 2024
DerdriuMarrinerJul 27, 2024
Sea-level rise intrigues me. Is there anything to do against it? Might it be possible to build shorelines upward?
frankbeswickSep 29, 2019
2:Anglesey probably derives its name from the Deceangli tribe, who lived there, though its Welsh name is Mona. Deceangli is a Latin rendering of a Welsh name that might have been Dchangli. Sey or Say or Ay is a common name ending for islands in British usage, It is a Scandinavian term. It probably came from the Norse seafarers, who named many coastal places.
3: Climate change predictions are that the east of England, where the fens are, will suffer more droughts, but the north and west will suffer more storms,and this is being proved to be so. Wind frequency cannot increase in the fens as the area tends to suffer strong and regular winds anyway. Wind strength might be worsening, but it is not the main problem. The main threat to the fens is sea level rise.
DerdriuMarrinerSep 28, 2019
Did King John really lose the royal treasure in the Wash? If so, has nothing ever been retrieved?
What is the etymology of the Welsh Anglesey?
Is the globally warmed climate change increasing the frequency and power of winds on England's fenlands? That's what's happening on the flattest lands along the coasts and Great Lakes on this side of the pond.
frankbeswickAug 11, 2018
dustytoesAug 10, 2018
frankbeswickAug 6, 2018
blackspanielgalleryAug 6, 2018