The best running trails around Sydenham

A lovely little church, didn't get a chance to go inside by was nice to take a stop at

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!

Robin Gibb’s grave and across the road his home (The Prebendal )

Quaint British pub as you would imagine. Here there is no painted sign in front of the entrance, but six bells have been placed here, three at the top, two in the middle and one at the bottom.

Very cute small village close to the Phoenix Trail and Thame. Easily accessible from cycle route 57.

This quarry is a Site of Special Scientific Interest and well known by geologists for its phenomenal history. Packed with fossils, some of the finds here date back 100 million years. There's no public access, but you can catch glimpses of its bright high-alkaline water from the surrounding footpaths.

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 earliest record of the Church of England parish church of Saint Andrew is from 1160. The nave was rebuilt in the 13th century, when the present arcades of four and a half bays for first the north aisles and then the south aisle were built. Building of the present tower began towards the end of the 13th century. Early in the 14th century St Andrew's was remodelled. The chancel was entirely rebuilt, the tower was made higher and the porch was built. The aisles were widened, given new windows, and extended westwards to flank either side of the tower. A rood screen was installed between the chancel and nave. The chancel and high altar were dedicated in 1326, which may therefore have been the year that the remodelling was completed. The high-pitched 13th century nave roof was replaced, probably later in the 14th century, with a Perpendicular Gothic clerestory and low-pitched roof. https://chinnorunitedchurches.co.uk/churches/st-andrews-chinnor https://en.wikipedia.org/wiki/Chinnor#Church_of_England