Sutton Coldfield, United Kingdom

Near to Langley Mill Farm is Fox Hollies, where archaeological surveys have uncovered flints dating from the New Stone Age. Amongst the finds in the area were flint cores and a flint scraper, which had been retouched with a knife. The presence of flint cores suggest that the site was used for tool manufacture and that a settlement was nearby. Additionally, a Bronze Age burnt mound was also discovered in the area.

In his History of Birmingham, published in 1782, William Hutton describes the presence of three mounds adjacent to Chester Road on the extremities of Sutton Coldfield (although now outside the modern boundaries of the town). The site, southwest of Bourne Pool (named "Bowen Pool" by Hutton), is called Loaches Banks and was mapped as early as 1752 by Dr. Wilks of Willenhall. Hutton interpreted the earthworks as a Saxon fortification but further archaeological work led Dr. Mike Hodder, now the Planning Archaeologist for Birmingham City Council, to believe that the site was an Iron Age hill-slope enclosure. Centuries of agriculture on the land has severely affected the visibility of the features, with the earthworks now only apparent in aerial photography.

Further evidence of pre-Roman human habitation are preserved in Sutton Park. A major fire in the park in 1926 revealed six more mounds near Streetly Lane, excavations of which uncovered charred and cracked stones within them and pits below the two largest mounds. Although their date of origin is unknown, claims they were of Bronze Age origin were disproved. The mounds are now covered in rough heathland. The area around Rowton's Well has been the source of many archaeological discoveries such as flint tools, and in the 18th century, worked timbers were discovered near the well, suggesting a possible Iron Age timber trackway built across wet land, similar to others discovered elsewhere in the country. A burnt mound was also discovered in New Hall Valley.

The presence of Romans in the area is most visible in Sutton Park, where a 1.5-mile (2.4 km) long preserved section of Icknield Street passes through. Whilst the road ultimately connects Gloucestershire to South Yorkshire, locally, the road was important for connecting Metchley Fort in Edgbaston with Letocetum, now Wall, in Staffordshire. The road is most visible from near to the pedestrian gate on Thornhill Road (OS Grid Reference SP 08759 98830), where the 8 m (26 ft) wide bank that formed the road surface is most prominent. Excavations at the road have showed that it was made from compacted gravel, never having a paved surface. Along each side are intermittent ditches, marked by Roman engineers, and beyond these are hollows where gravel was excavated to make the road surface. At least three Roman coins have been found along the course of Icknield Street through Sutton Park, as well as a Roman pottery kiln elsewhere in the town.

Next to the Iron Age property at Langley Brook, the remains of a timber building and field system were discovered. Pottery recovered from this site was dated to the second and third century, indicating the presence of a Roman farmstead.

Upon the Roman withdrawal from Britain to protect the Roman Empire on the continent in the fifth century, the area of Sutton Coldfield, still undeveloped, passed into the Anglo Saxon kingdom of Mercia. It is during this period that it is believed Sutton Coldfield may have originated as a hamlet, as a hunting lodge was built at Maney Hill for the purpose of the Mercian leaders. The outline of the deer park that it served is still visible within Sutton Park, with the ditch and bank boundary forming the western boundary of Holly Hurst, then crossing Keepers Valley, through the Lower Nuthurst and continuing on south of Blackroot Pool. Due to the marshy ground at Blackroot Valley, a fence was probably constructed to contain the deer, and the ditch and bank boundary commence again on the eastern side, on towards Holly Knoll.

This became known as Southun or Sutton; "ton" meaning the town stead to the south of Tamworth, the capital of Mercia. Middleton is situated between the two. "Coldfield" denotes an area of land on the side of hill that is exposed to the weather.

Sutone, as the manor became known, was held by Edwin, Earl of Mercia, during the reign of Edward the Confessor. Upon the death of Edwin in 1071, the manor and the rest of Mercia passed into the possession of the Crown, then ruled by William the Conqueror, resulting in Sutton Chase becoming a royal forest.

The manor of Sutone was mentioned in the Domesday Book of 1086, where it was rated at eight hides, making it larger than all surrounding villages in terms of cultivated land.