The Rivers of Great Britain, Descriptive, Historical, Pictorial: Rivers of the East CoastVarious
History
The Rivers of Great Britain, Descriptive, Historical, Pictorial: Rivers of the East Coast
Various
Great Britain -- Description and travel; Rivers -- Great Britain
There is in the crypt an alabaster tomb of a knight in armour, dating
from the fifteenth century; and in front of the old gateway is another
relic of ancient days. This is the base of a cross, which, to judge
from the number of steps, must have been of considerable size, and
probably indicated the original market-place; for its proximity to the
church and the priory would enable the country folk to attend to the
affairs of this world, while at the same time they did not entirely
neglect the concerns of the other. One trace both of ancient name and
ancient importance is still retained by Repton, for all Derbyshire
south of the Trent is called the "Hundred of Repington." This part of
the river-course is about twenty-four miles in length. Previous to
this it separates for a space Derbyshire from Staffordshire, and it
leaves the former county at the junction of the Erewash, a stream from
Sherwood Forest, which, for the greater part of its course, forms a
parting from Nottinghamshire. Below Repton for several miles there is
no place of special interest in the valley of the Trent, though some of
the villages in or near it are of considerable antiquity. The sketch of
the "Crow Trees," now fewer than formerly, at Barrow, gives a good idea
of the quiet but pleasant riverside scenery. At Swarkestone the river
is crossed by a curious old bridge, the raised approaches across the
water-meadows being about a mile in length. The bridge is assigned by
the guide-books to the twelfth century, and is traditionally reported
to have been the work of two maiden sisters, who spent upon it all
their living. It was the cause of a smart struggle in the civil war
of 1643, and was occupied by the advanced guard of the Jacobites in
1745. Chellaston, a short distance from the opposite bank, is a name
familiar to geologists. There are extensive workings here for gypsum,
and the occurrence of a number of minute fossils (_foraminifera_) in a
deposit usually destitute of the remains of organic life has attracted
especial attention to the locality. It is, however, now doubted
whether these organisms have not been obtained from a deposit of later
age. After Stanton-by-Dale and Weston-on-Trent comes Donington Park,
with its ample lawns and shady groves extending around the mansion,
which was the home of the Hastings family, of one of whom more than
enough was heard some few years since. Behind the park the village
of Castle Donington straggles down and along the high road leading
from Ashby-de-la-Zouch towards the Trent. Here some remnants of a
castle are to be seen, said to have been founded by John of Gaunt, and
from which the village obtains its distinctive name. Beyond this are
Ashton-on-Trent and Cavendish Bridge, which crosses the river a short
distance above the confluence of the Derwent. This bridge obtains its
name from the family of Cavendish, by members of which it was erected
about the middle of the last century.
Public-domain text, read in full here on John Shaqi.
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