엘즈버러‬에서 가장 멋진 ‪11‬개의 호수

This is one of the quarries here, a part of the former Chinnor Chalk Pit, now flooded and known as Old Kiln Lakes. The lakes are freshwater, but very alkaline, and there was a warning to the public issued in 2012 to not swim in there. It's a striking and moon-like place, looking very dramatic and slightly out-of-this-world. A definite must!

Great family friendly rides around the lakes, 3 will signed routes of different distance. Great fun 🙏

The Marsworth Reservoirs act as a magnet for anglers, dog walkers, boaters, birdwatchers and walkers, especially over a sunny weekend, but few ever really venture much beyond the car parks and tearooms. The walk begins with a flight of locks along the Grand Union Canal, before heading down a stretch of the partially restored Wendover Arm. The route then diverts into open countryside before regaling the walker with a magnificent view of the large Wilstone Reservoir, one of four on this walk. Here there is an option to enter a bird hide to view the many species who call this water their home at different times of the year. The other reservoirs follow, making this a relaxing six miles of relatively easy walking following a circular route. Allow a good couple of hours to complete the walk, longer if you want to linger.

Good place for walk or mountain bike tour. Bird watching hide is there.

Chinnor, Chalk and Cement Mr. W. Benton's Cement and Lime Works opened in Chinnor in 1908, but cement making on a truly industrial scale did not begin until 1919. Output of cement from Chinnor peaked at about 5600 tonnes per week in the 1990s. Up to 120 people were employed at any one time. The cement works closed in 1999 and there are plans for the re-development of the site, using the flat areas for housing but also with opportunities for recreation and conservation in the water filled quarries The scale of chalk extraction for cement making can be seen from a short walk along the Ridgeway National Trail. The Ridgeway runs on a high causeway between the large quarries, giving views of the pits through the boundary fences. (Do not cross over or through the fences). Geology One of the chalk quarries has been protected as a geological Site of Special Scientific Interest as it has particularly good exposures of both the Lower Chalk and Middle Chalk geological layers. Both layers have given upimportant fossil ammonites.

The Lyde, a tributary of the River Thames, rises here and the garden is planted with primulas, astilbes, gunnera and hostas. Originally three watercress beds, surrounded by large and beautiful wych elms, it has — as a result of elm disease — become a wilderness. The garden is open at the owners’ discretion from 9am – 4pm daily. Dogs are not permitted. See: carington.co.uk/gardens/lyde-garden

Archaeological Surveys undertaken in Park Wood have revealed a fascinating past for this quiet area of deciduous woodland. Lynchets and banks within the woods give evidence of ancient field systems which may date back to the late Iron Age/early Roman period (or they may be medieval). In the beech woodland opposite the pond is evidence of a late thirteenth/early fourteenth homestead in the woodlands and in Tudor times (1485 – 1603) the woodland was a deer park. Much of Park Wood was converted to beech woodland from the late 18th until the early 20th century to cater for the High Wycombe furniture industry. Associated features include sawpits, tracks and charcoal burning platforms. https://www.nationaltrust.org.uk/chilterns-countryside/trails/bradenham-beech-woods-and-bunkers-trail