Brixham Cave

Brixham Cave. A limestone cavern located on Windmill Hill near the fishing port of Brixham in Devon, it became a pivotal site in 19th-century archaeology. Its systematic excavation between 1858 and 1859 provided crucial evidence for the antiquity of humans, directly challenging prevailing Biblical chronology. The findings from this site played a decisive role in convincing the scientific establishment of the coexistence of early humans with extinct Ice Age fauna.

Discovery and excavation

The cavern was discovered in January 1858 during quarrying operations on the land of a local merchant. Recognizing its potential, the geologist Hugh Falconer promptly visited and helped organize a committee to fund a meticulous investigation. The excavation was entrusted to the schoolmaster and geologist William Pengelly, who employed a revolutionary grid system to record the precise three-dimensional location of every find. This committee included prominent figures like Joseph Prestwich and Charles Lyell, whose prior work on the Somme River valley had begun to shift scientific opinion. The rigorous methodology, supervised by these leading minds of the Royal Society and the Geological Society of London, ensured the stratigraphic integrity of the discoveries was beyond reproach.

Archaeological significance

The primary significance of the site lies in its role as a catalyst for the acceptance of human antiquity. Before its excavation, the dominant view, influenced by scholars like William Buckland, was that human fossils found with extinct animals were intrusive. The undisputed stratigraphic sequence at this location demonstrated that flint tools were sealed within the same undisturbed layers as the bones of long-vanished creatures like the woolly rhinoceros. This evidence was presented at a famous 1859 meeting of the British Association for the Advancement of Science, where Charles Darwin's On the Origin of Species was also about to be published. The convergence of these ideas fundamentally altered the understanding of prehistory and provided a deep temporal context for human evolution.

Stratigraphy and dating

The stratigraphy of the cave deposits was clearly defined during the excavation. A dense layer of stalagmite floor sealed the lower archaeological layers, proving they had not been disturbed in recent times. Beneath this floor were strata containing both Palaeolithic flint handaxes and a rich assemblage of Pleistocene animal bones. While the original investigations provided relative dating through stratigraphic association and faunal correlation, modern techniques have since provided absolute dates. The site is now understood to belong primarily to the Middle Palaeolithic, associated with Neanderthal occupation during the last glacial period. Comparisons with other dated sequences in Europe, such as those at Kent's Cavern and Creswell Crags, have helped refine its chronological placement.

Faunal remains

The cave yielded an extensive and well-preserved collection of Pleistocene mammal bones, offering a snapshot of the local environment during the Ice Age. The fauna was dominated by cold-adapted species, including woolly mammoth, woolly rhinoceros, reindeer, and cave bear. Also present were remains of cave hyena, lion, and various bovids. This Mammoth steppe assemblage indicated a cold, open grassland environment prevailing in Devon at the time. The bones showed clear evidence of human activity, including cut marks from butchering and fractures for marrow extraction, alongside gnawing marks from predators like hyenas, illustrating the complex taphonomy of the site.

Relationship to other sites

The findings here were immediately and deliberately compared to other key European sites to build a consensus. Joseph Prestwich and John Evans famously traveled to Abbeville and Amiens in France to examine the discoveries of Jacques Boucher de Perthes in the Somme River gravels, using the evidence from Devon to validate those claims. It forms a critical part of a network of British Palaeolithic caves, including the nearby Kent's Cavern and the caves of the Cheddar Gorge. Its legacy is directly linked to the establishment of the science of archaeology and the systematic exploration of other important sites like Boxgrove Quarry and Swanscombe Heritage Park.

Category:Caves of Devon Category:Archaeological sites in Devon Category:Paleolithic sites in England Category:History of archaeology