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Abbey Fields is set in the dramatic valley of the Finham Brook and enjoys views of the historic town and Kenilworth castle. Grassy slopes, a lake, historic buildings and veteran trees recall Abbey Fields’ past as the farmland of St Mary’s Abbey, whose ruins adjoin the park. Because of its important heritage, Abbey Fields is a Scheduled Ancient Monument.

Babbs Mill Lake sits in the Babbs Mill Local Nature Reserve and has a designated cycle path running right the way through. There are benches dotted around and ample open space for a sit-down and picnic. Make sure to say hi to the local wildlife who you'll spot milling around the lake.

Nestled on the outskirts of Solihull, Elmdon Nature Park shines as a splendid Green Flag Park and Local Nature Reserve. Designed with families in mind, it invites joy, tranquillity, and exploration amid its expansive and open landscapes.

A picturesque lake in the middle of the Kingfisher Local Nature Reserve. Fed by the River Cole with an array of wildlife.

Shustoke Reservoir is managed by Severn Trent. The reservoir was completed in 1884 to provide water for Birmingham. Nowerdays the reservoir supplies Nuneaton and the surrounding area.

The history of Shustoke Why were the reservoirs created here?  In 1870 the Industrial Revolution was in full swing, as was the birthrate and the need for clean water was becoming more pressing.  The Birmingham Water Works Company therefore applied to Parliament for  permission for water to be taken from the Rivers Bourne and Blythe, whose gathering grounds in rural areas to the East of Birmingham were declared to be away from pollution, and to impound the water from the Bourne in a reservoir which was built at Shustoke.   A pumping station, filter beds and another small reservoir was also constructed at Whitacre. What was here before? Before the reservoir was built, the land was occupied by Whitacre Lodge which was part of the Hams Estate. This was sold by Lord Norton in 1879, for the building of Shustoke Reservoir.       How long did it take to build the Reservoirs? The time-scale granted for this work was 10 years and although most of the work at Whitacre was completed in the time scheduled, an extension of five years was applied for in 1879 as the reservoir at Shustoke had hardly been started; the eventual completion was around 1884.         What is the Reservoirs role in the water supply network? When the reservoirs were built they were to supply water to the nearby Whitacre Treatment Works, which was to provide 28 million litres of water daily to Birmingham. As the city grew this soon became inadequate and with the completion of the Elan Valley scheme in 1904 Whitacre was relegated to standby duty. In 1908 Whitacre was recommissioned to supply water to Coventry to supplement the local borehole supplies. In the 1050’s Whitacre also started to supply Nuneaton and now about 10% of the water from Shustoke supplies Coventry with the rest going to Nuneaton and the surrounding districts of Bedworth and Atherstone. Where does the water come from? The water is gravity fed by the nearby River Bourne which runs along the north of the two reservoirs. How deep and big are the reservoirs? The reservoirs consist of a settling pool of 7.8 acres and a storage reservoir of 92 acres.  Combined they have a capacity of around 460,000,000  gallons.

Lovely park with a great view over lake in the centre of old Kenilworth

The Blythe Valley Countryside Park is 87 acres in size. The circular path includes several small lakes and a bird hide. The site is like a cross between New Hall Valley Country park in Sutton Coldfield and Plantsbrook in Pype Hayes and is home to a mixture of conservation woodland, 38,000m² of new woodland, grassland, hedgerows, streams and wetland. The 3.5km path is be great for cycling and running, too. Work on the business park commenced in August 1998 and was a joint development between Solihull MBC, Doughty Hanson & Co Real Estate and Liberty Property Trust. The River Blythe has been designated a Site of Special Scientific Interest (SSSI) and there are local damp willow woodlands, emergent reeds and wet grassland. In a rare UK approach, storm water from the built up area is cleaned by several processes en route to the river.