factory lived, the entrance to the estate was between a pair of pillars, though they have long since been demolished. However the capitals were preserved and now sit on the two brick pillars at the Selhurst Road entrance to South Norwood Recreation Ground. In 2006, South Norwood Lakes in the north of the ward was the scene of a fatal stabbing. Governance South Norwood was within the County Borough of Croydon until 1965 when, following the enactment of the London Government Act 1963, it became part the local government of Greater London. The town is now part of the wards of South Norwood and Woodside in the local authority of Croydon, which has the responsibility for providing services such as education, refuse collection, and tourism. South Norwood Ward is part of the ethnically diverse Croydon North parliamentary constituency, which had one of the largest electorates in England at the 2010 general election, whereas Woodside Ward falls within the boundaries of the Croydon Central constituency. The sitting Member of Parliament (MP) for Croydon North is Steve Reed, a member of the Labour Party, following the death of Malcolm Wicks. The sitting Member of Parliament for Croydon Central is Sarah Jones, also a member of the Labour Party. Policing services are provided by the Metropolitan Police via the Croydon Police Station branch in Park Lane, Croydon. The London Fire Brigade provide services for the area and Greater London as a whole; the nearest fire station is at Woodside which has only one pumping appliance. Geography South Norwood is bordered by Anerley to the north, Selhurst to the south, Woodside due east and Thornton Heath to the west. The northernmost point of South Norwood is at Beaulieu Heights (alternatively spelt Beulah Heights, Beaulah Heights and Beulieu Heights) which contains Beulah Heights Park, overlapping with Upper Norwood and New Town. The northern part of the district is situated on the lower parts of the hill that forms Upper Norwood. South Norwood lies on the southern slopes of the Norwood Ridge which forms the southern edge of the London Basin. This line of hills runs from north-east to south-west for about three miles (5 km) and rises to approximately above sea level at its highest point. It is formed by a ridge of grey silty deposits known as London Clay, capped in places with the gravel of the Claygate Beds. Because of this gravel working