Soft geology |
"I've been hurried, I've been scurried, I've been dragged from door to door, now here I lie on this squallid floor."

We used to talk about "solid ground" or terra firma, as though the land around us could always be relied upon to support us from the abyss below, but today we talk about continental drift and soft geology.
I came upon a fine illustration of the latter while walking on the Suffolk coast, north of Southwold where the road to the beach from the village of Covehithe simply leads you over a cliff. Thankfully that road is closed now, but I guess it is only a matter of time before the cliff erodes back to the village and the church.
Most of the sand and gravel that falls from the cliffs is mobilised in the cloudy shallows close to the shore and carried southward by the current to be deposited in the lee of somewhere solid. That's how Orford Ness was formed.
Fishing is a characteristic industry of this coast but there is a shortage of accessible harbours. Most boats are pulled up onto the steep shingle beaches using static winches or aged, rusty tractors. The exception is at Southwold and Walberswick where the River Blythe runs deep enough to form a navigable channel that has been reinforced in various ways to form landing stages along a quayside.

The Southwold harbour area still has a great deal of character and Walberswick has retained a lot of it's charm. Go there before it becomes almost too gentrified.
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