周辺の天然記念物・トップ7

This outcrop tells a story of when Kenilworth lay just north of the Equator in a semi-desert climate with market wet and dry seasons. Many buildings in Old Kenilworth, notably the Castle, the Abbey and St. Nicholas Church, are built of the local Kenilworth Sandstone that you can observe here.

Nice for a walk and close to the the lake

Old structure converted into a potential home for bat's and also explaining the plight of these enigmatic creatures.

Kenilworth Sandstone exposed in Kenilworth old railway cutting Warwickshire Museum. Situated at the eastern end of the Kenilworth Greenway, the cycle and pedestrian path that runs south-east of the new Coventry Road bridge passes through a disused railway cutting, excavated partly through the local natural bedrock. This can seen in the banks adjacent to the path and consists of thick beds of red sandstone. This is the so-called Kenilworth Sandstone, dating back roughly 280 million years to the Permian Period. The sandstone originated as river sand, deposited on river floodplains at a time when what is now Warwickshire was much closer to the equator, and enjoyed a hot, semi-arid climate. The Kenilworth Sandstone was once quarried locally for building stone, and can be seen in many of the older buildings in and around the town. Kenilworth Castle is undoubtedly the best known example.

This is a beautiful peaceful hike with amazing views.

Clowes Wood is a piece of history as it was the first reserve owned by Warwickshire Wildlife Trust, acquired thanks to the generosity of an anonymous donor in 1974. Clowes Wood has probably been wooded since the last ice age, though it was almost cleared of trees in the early 1900s. It is cut through by the Birmingham to Stratford railway and habitats found here today include heathland, woodland, and wet meadow. Wildflowers to be seen here include bluebell, lily of the valley, cow-wheat and bilberry. Fifty species of bird breed here, such as jay, chiff chaff, nuthatch and treecreeper, and also woodcock and all three woodpeckers. Badgers live in this woodland and red fox, muntjac and brown hare are all regular visitors to this reserve.

The cutting on the approach to the tunnel on the north side is a designated site of special scientific interest. Sites of special scientific interest (SSSIs) are protected by law to conserve their wildlife or geology. The cutting exposes a sequence in Arden sandstone of the late Triassic period in which grey-green shales and siltstones with wavy and lenticular bedding pass into white fine-grained well sorted dolomitic sandstones. The facies (character of a rock expressed by its formation, composition, and fossil content), thus indicates marine (intertidal) deposition conditions.

The name "Berkswell" has long been attributed to the presence of the well - "In Domesday book it is written Berchewelle, having first had that denomination (as I guess) from the large Spring which boileth up on the South side of the Churchyard" wrote the Warwickshire historian Sir William Dugdale in the mid 18th century. The English place names society suggested that the name Berkswell means Well or Spring of Bercul, a personal name that is found in Mercia ( wherein "Berkswell" lay) in the eighth century. Christianity had been brought to this area by travelling monks from Lichfield. A local leader, Bercul, is said to have been baptised in the well. The well was the source of water for many villagers, including the school, right up until the mid twentieth century. In the nineteenth century a pipe was laid from the Well to Berkswell Hall where a hydraulic water ram lifted it for use in the Hall up until the eve of the second world war. The well was refurbished in to its present form in 1851.