バルサルの天然記念物・トップ9

Large green park with many tarmac'd paths in good condition. Also contains football and cricket pitches, foot-golf course, tennis courts, skate park and childrens' activity playground. There are two cafes within the two pavillions, along with ornamental areas with ponds. There is a large War Memorial monument. The park is also home to Coventry Park Run.

Coventry’s War Memorial Park opened in July 1921 as a tribute to the 2,587 Coventrians who died during the First World War. Coventry City Council used money donated by the public to purchase the land from the Lords of Styvechale Manor, the Gregory-Hood family. At the time it was a large grassed area that was part of Styvechale (Stivichall) Common. The landscaped gardens and sports areas were created in the late-1920s and 1930s. During the Second World War, barrage balloons and anti-aircraft guns were sited in the park and the large concrete blocks where they were positioned still exist.

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

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.