Brownhills is located at 52°38′49.20″N 1°55′58.80″W on the edge of Cannock Chase and lies mostly at a height of approximately 150 metres (492 ft) above sea level, although there is a sharp incline to nearly 180 metres (590 ft) at the eastern end of the town.
The highest point of Cannock Chase, standing at 244 metres (801 ft) above sea level, lies approximately 4 miles (6 km) from the town.
Although a small river called Crane Brook flows slightly to the east of Brownhills, the only significant bodies of water in the area are human-made, namely the canal and the 3 km² (1.2 sq mi) reservoir Chasewater, which lies to the north, between Brownhills and Cannock Chase.
The reservoir was constructed in the 18th century and reshaped by reclamation schemes as recently as the 1970s.

Immediately to the west of the town is Brownhills Common, a 100-acre (0.40 km²) heathland which once formed part of Cannock Forest (also known as "Canke Wood").
Although the forest was felled in the 15th and 16th centuries, the spread of heather and the grazing of sheep led to the creation of a huge area of heathland.
The area was affected by mine workings but has now returned to a more natural state and lizards and dragonflies may be observed.
The area now supports various habitat types, with the heathland mixing with marshy grassland, with scattered scrub and pools.
In 1926, when ownership of the Common was transferred to the local Council, a large area of barren land at the eastern end, closest to the town, was landscaped, with new trees planted.
Lying south of the Common, Birch Coppice is a large area of predominantly oak and birch woodland, which, although crossed by a now-dismantled railway line, mostly escaped the destruction caused to other wooded areas by mining and other industry.

To the south, Brownhills is separated from the nearby village of Clayhanger by Clayhanger Common, which is designated a Site of Special Scientific Interest and considered "one of the best wetland sites in the county".
In 2007, a new £445,000 bridge was erected across the canal at Brownhills, providing pedestrian, disabled and cycling access to the Common and to the village of Clayhanger beyond.
To the east lies the village of Stonnall and a large area of green belt land.

The geology of Brownhills comprises mainly red clay marl overlying Triassic sandstone and deposits of coal.
The town is on several fault lines, the main one being the Vigo Fault, a branch of the larger Eastern Boundary Fault, which runs from Birmingham to Rugeley.
On the western side of the fault, in the area of Brownhills Common, the marl is over 1,000 feet (305 m) thinner than on the eastern side, bringing the coal seams significantly closer to the surface.
The presence of the faults and the effects of mining mean that subsidence has been a major problem in the area for many years.

The land within the town is made up of approximately 62% greenspace, 18% domestic gardens, 7% roads, 4% domestic buildings, 3% non-domestic buildings and 6% other uses.
Since the 19th century, trade in Brownhills has been centred on the High Street.
As the canal and Clayhanger Common lie immediately to the south of the High Street, the town's housing areas are mainly to the north and at the eastern and western ends of the town.
Brownhills has 5,152 residential dwellings, of which 47% are semi-detached houses.
Selling prices for all types of property within the town have risen significantly since 2000; in August 2007 the average selling price was £137,600, compared to £59,596 in 2000, a rise of 131%.
The Aldridge and Brownhills Housing Trust owns and manages those properties formerly owned as council houses by Walsall Council.

In the West Midlands, the warmest time of the year is July and August, when maximum temperatures average around 21 °C (70 °F); the coolest months are January and February, when minimum temperatures average around 1 °C (39 °F).
The area's average maximum and minimum temperatures are almost exactly in line with the national average.
The average annual rainfall is about 676 millimetres (27 in), the wett
Brownhills is located at 52°38′49.20″N 1°55′58.80″W on the edge of Cannock Chase and lies mostly at a height of approximately 150 metres (492 ft) above sea level, although there is a sharp incline to nearly 180 metres (590 ft) at the eastern end of the town. The highest point of Cannock Chase, standing at 244 metres (801 ft) above sea level, lies approximately 4 miles (6 km) from the town. Although a small river called Crane Brook flows slightly to the east of Brownhills, the only significant bodies of water in the area are human-made, namely the canal and the 3 km² (1.2 sq mi) reservoir Chasewater, which lies to the north, between Brownhills and Cannock Chase. The reservoir was constructed in the 18th century and reshaped by reclamation schemes as recently as the 1970s.
Immediately to the west of the town is Brownhills Common, a 100-acre (0.40 km²) heathland which once formed part of Cannock Forest (also known as "Canke Wood"). Although the forest was felled in the 15th and 16th centuries, the spread of heather and the grazing of sheep led to the creation of a huge area of heathland. The area was affected by mine workings but has now returned to a more natural state and lizards and dragonflies may be observed. The area now supports various habitat types, with the heathland mixing with marshy grassland, with scattered scrub and pools. In 1926, when ownership of the Common was transferred to the local Council, a large area of barren land at the eastern end, closest to the town, was landscaped, with new trees planted. Lying south of the Common, Birch Coppice is a large area of predominantly oak and birch woodland, which, although crossed by a now-dismantled railway line, mostly escaped the destruction caused to other wooded areas by mining and other industry.
To the south, Brownhills is separated from the nearby village of Clayhanger by Clayhanger Common, which is designated a Site of Special Scientific Interest and considered "one of the best wetland sites in the county". In 2007, a new £445,000 bridge was erected across the canal at Brownhills, providing pedestrian, disabled and cycling access to the Common and to the village of Clayhanger beyond. To the east lies the village of Stonnall and a large area of green belt land.
The geology of Brownhills comprises mainly red clay marl overlying Triassic sandstone and deposits of coal. The town is on several fault lines, the main one being the Vigo Fault, a branch of the larger Eastern Boundary Fault, which runs from Birmingham to Rugeley. On the western side of the fault, in the area of Brownhills Common, the marl is over 1,000 feet (305 m) thinner than on the eastern side, bringing the coal seams significantly closer to the surface. The presence of the faults and the effects of mining mean that subsidence has been a major problem in the area for many years.
The land within the town is made up of approximately 62% greenspace, 18% domestic gardens, 7% roads, 4% domestic buildings, 3% non-domestic buildings and 6% other uses. Since the 19th century, trade in Brownhills has been centred on the High Street. As the canal and Clayhanger Common lie immediately to the south of the High Street, the town's housing areas are mainly to the north and at the eastern and western ends of the town. Brownhills has 5,152 residential dwellings, of which 47% are semi-detached houses. Selling prices for all types of property within the town have risen significantly since 2000; in August 2007 the average selling price was £137,600, compared to £59,596 in 2000, a rise of 131%. The Aldridge and Brownhills Housing Trust owns and manages those properties formerly owned as council houses by Walsall Council.
In the West Midlands, the warmest time of the year is July and August, when maximum temperatures average around 21 °C (70 °F); the coolest months are January and February, when minimum temperatures average around 1 °C (39 °F). The area's average maximum and minimum temperatures are almost exactly in line with the national average. The average annual rainfall is about 676 millimetres (27 in), the wett
Brownhills