Kingston Crossing Halt railway station

Kingston Blount is a village about 4 miles (6.4 km) southeast of Thame in South Oxfordshire, England. The village is a spring line settlement at the foot of the Chiltern Hills escarpment. The ancient pre-Roman Ridgeway and Icknield Way pass through the parish. The Ridgeway is now a National Trail.

Crowell is a village and civil parish in Oxfordshire, about 4 miles (6.4 km) southeast of the market town of Thame and 1 mile (1.6 km) southwest of the village of Chinnor. The 2001 Census recorded the parish's population as 100. Crowell village is a spring line settlement at the source of a stream called the Pleck at the foot of the Chiltern Hills escarpment. The toponym "Crowell" is derived from the Old English for "crow's spring" or "crow's stream".Crowell is a strip parish about 3 miles (5 km) long on a northwest – southeast axis and less than 1⁄2-mile (800 m) wide at its widest point. The northwest part of the strip is low-lying land in the Vale of Oxford about 350 feet (110 m) above sea level; the southeast part of the strip is in the Chilterns and rises to 774 feet (236 m) above sea level. The southeastern part of the parish is bounded on three sides by Buckinghamshire.

Butt's Way is a cricket ground between the villages of Aston Rowant and Kingston Blount in Oxfordshire.

Aston Rowant Woods is a 209.7-hectare (518-acre) biological Site of Special Scientific Interest near Aston Rowant in Oxfordshire and Buckinghamshire. Part of it is in Aston Rowant National Nature Reserve, and a large part is in the Chiltern Beechwoods Special Area of Conservation. The site is also in the Chilterns Area of Outstanding Natural Beauty.The site is described by Natural England as "of national importance as a large, unfragmented area of ancient semi-natural woodland characteristic of the Chilterns scarp". It is composed of Grove Wood, Aston Wood, Juniper Bank, Kingston Wood, High Wood and Crowell Wood. Flora include 52 species indicative of ancient woods, and there are over 100 species of fungi, while damp hollows and fallen trees provide diverse habitats for invertebrates. Uncommon species include the herb Paris quadrifolia and the flower green hellebore. There are small areas of scrub and chalk grassland.

Stokenchurch BT Tower is a telecommunications tower built of reinforced concrete at Stokenchurch, Buckinghamshire, England. Reaching to 340.5 metres (1,117 ft) above mean sea level, it dates from 1963 and is 99.4 metres (326 ft) tall. There are four platforms at the top that are used to attach microwave transmission drums and other antennas. The Stokenchurch Tower is one of the fourteen BT towers built of reinforced concrete. Seven of the fourteen are of similar design, known as the 'Chilterns' type, after this tower's location on the Chiltern Hills. They are identical except for their heights, which vary considerably; the Stokenchurch BT Tower is the second tallest out of the set. The towers are located at:-

Oakley Hill is a 13-hectare (32-acre) nature reserve south of Chinnor in Oxfordshire, England. It is managed by the Berkshire, Buckinghamshire and Oxfordshire Wildlife Trust.This hill has chalk grassland, beech woodland and scrub. Flowering plants include Chiltern gentian, wild thyme, clustered bellflower, pyramidal orchid, yellow-wort, dog's mercury, bluebell, common rock-rose and harebell.

The Chiltern Hills are a chalk escarpment in the UK northwest of London, covering 660 square miles (1,700 km2) across Oxfordshire, Buckinghamshire, Hertfordshire, and Bedfordshire, stretching 45 miles (72 km) from Goring-on-Thames in the southwest to Hitchin in the northeast. The hills are 12 miles (19 km) at their widest. In 1965, almost half of the Chiltern Hills was designated as an Area of Outstanding Natural Beauty (AONB). The northwest boundary is clearly defined by the escarpment. The dip slope is by definition more gradual, and merges with the landscape to the southeast. The southwest endpoint is the River Thames. The hills decline slowly in prominence in northeast Bedfordshire.

Oakley is a spring line settlement at the foot of the Chiltern Hills on the route of the Lower Icknield Way. It is about 4.5 miles (7.2 km) southeast of Thame in Oxfordshire, England. It is in the civil parish of Chinnor, and 20th century housing developments have absorbed Oakley into that village.

Aston Rowant railway station was opened in 1872 and was a part of the Watlington and Princes Risborough Railway. Having closed in 1961, there have been proposals to reopen the station not only to the heritage services of the Chinnor and Princes Risborough Railway, but also National Rail commuter services operated by Chiltern Railways.

Aston Rowant (anciently Aston Rohant) is a village, civil parish and former manor about 4+1⁄2 miles (7 km) south of Thame in South Oxfordshire, England. The parish includes the villages of Aston Rowant and Kingston Blount, and adjoins Buckinghamshire to the southeast. The 2011 Census recorded the parish's population as 793. The Lower Icknield Way passes through the parish southeast of the village.

Aston Rowant Cutting is a 3.5-hectare (8.6-acre) geological Site of Special Scientific Interest south of Aston Rowant in Oxfordshire. It is a Geological Conservation Review site.Aston Rowant Cutting, also known as the Stokenchurch Gap or Aston Hill cutting, or locally "The Canyon" is a steep chalk cutting, constructed through the Chiltern Hills on the border between Buckinghamshire and Oxfordshire, England during the early 1970s for the M40 motorway. It is 1,200 metres (3,900 ft) long and a maximum of 47 metres (154 ft) deep, and is located approximately 13 kilometres (8.1 mi) from High Wycombe and close to the village of Stokenchurch. Despite the names, the cutting is in the parish of Lewknor rather than Aston Rowant or Stokenchurch. The cutting (along with the nearby village of Stokenchurch) is subject to frequent heavy fog during the winter months.

Chinnor Chalk Pit is a 20.4-hectare (50-acre) geological Site of Special Scientific Interest south of Chinnor in Oxfordshire. It is a Geological Conservation Review site.This site is described by Natural England as "important for its excellent exposures of Totternhoe Stone", dating to the mid-Cenomanian stage of the Cretaceous period, around 100 million years ago. It has yielded many fossils of ammonites from the Lower and Middle Chalk.