From Academic Kids

Denehole (alternatively Dene hole or Dene-hole) is the name given to certain caves or excavations in England, which have been popularly supposed to be due to the Danes or some other of the early northern invaders of the country. The common spelling Dane hole is adduced as evidence of this, and individual names, such as Vortigerns Caves at Margate, and Canutes Gold Mine near Bexley, naturally follow the same theory. The word, however, is probably derived from the Anglo Saxon den, a hole or valley. The lack of evidence found in them has led to long arguments as to their function.



The general outline of the formation of these caves is invariably the same. The entrance is a vertical shaft some 3 ft. (1m) in diameter falling, on an average, to a depth of 60 ft (20m). The depth is regulated, obviously, by the depth of the chalk from the surface, but, although chalk could have been obtained close at hand within a few feet, or even inches, from the surface, a depth of from 45 to 80 ft., or more, is a characteristic feature. It is believed that dene-holes were also excavated in sand, but as these would be of a perishable nature there are no available data of any value.

Footholds were cut into the sides of the shaft to allow the miners to climb in and out. The shaft, when the chalk is reached, widens out into a domed chamber with a roof of chalk some 3 ft. thick. The walls frequently contract somewhat as they near the floor. As a rule the main chamber is between 16 to 18 ft. in height, beneath each shaft. From this excessive height it has been inferred that the caves were not primarily intended for habitations or even hiding-places. In most cases, between two and four sub-chambers are present, excavated laterally from the floor level, the roof being supported by pillars of chalk left standing.


There are many underground excavations in the south of England, also found to some extent in the Midlands and the north, but true dene-holes are found chiefly in those parts of Kent and Essex along the lower banks of the Thames. With one exception there are no recorded specimens farther east than those of the Grays Thurrock district, situated in Hangmans Wood, on the north, and one near Rochester on the south side of the river. Isolated specimens have been discovered in various parts of Kent and Essex, but the most important groups have been found at Grays Thurrock, in the districts of Woolwich, Abbey Wood and Bexley, and at Gravesend. Those at Bexley and Grays Thurrock are the most valuable still existing. It is generally found that the tool work on the roof or ceiling is rougher than that on the walls, where an upright position could be maintained


Pliny the Elder wrote about British chalk extraction in 70AD and archaeological evidence shows that at least some of the deneholes were being exploited during prehistory. Casts taken of some of the pick-holes near the roof show that, in all probability, they were made by bone or horn picks. And numerous bone picks have been discovered in Essex and Kent. These pick-holes are amongst the most valuable data for the study of dene-holes, and have assisted in fixing the date of their formation to pre-Roman times. Very few relics of antiquarian value have been discovered in any of the known dene-holes which have assisted in fixing the date or determining the uses of these prehistoric excavations. Chretien de Troyes has a passage on underground caves in Britain which may have reference to dene-holes, and tradition of the 14th century treated the dene-holes of Grays as the fabled gold mines of Cunobeline (or Cymbeline) of the 1st century.

In 1225 Henry III gave every man the right to sink a marl pit on his own land and it seems that spreading chalk on the fields was a common practice in the Middle Ages. This appears to have continued into the nineteenth century and it is tempting to attribute deneholes to the need for chalk.

Vortigerns Caves at Margate are possibly dene-holes which have been adapted by later peoples to other purposes; and excellent examples of various pick-holes may be seen on different parts of the walls.

Local tradition in some cases traces the use of these caves to smugglers, and, when it is remembered that illicit traffic was common not only on the coast but in the Thames as far up the river as Barking Creek, the theory is at least tenable that these ready-made hiding-places, difficult of approach and dangerous to descend, were so utilized.


By the end of the nineteenth century, three purposes were suggested for which dene-holes may have been originally excavated:

  • as hiding-places or dwellings
  • storehouses for grain.
  • drawwells for the extraction of chalk for agricultural uses

For several reasons it is unlikely that they were used as habitations, although they may have been used occasionally as hiding-places. Other evidence has shown that it is equally improbable that they were used for the extraction of chalk. Silos, or underground storehouses, are well known in the south of Europe and Morocco. It has been suggested that the grain was stored in the ear and carefully protected from damp by straw. A curious smoothness of the roof of one of the chambers of the Gravesend twin-chamber dene-hole has been put forward as additional evidence in support of this theory.

Since the 1950s the theory that they were ancient chalk mines has gained acceptance This was formerly thought unlikely as it was reasoned that chalk could have been obtained outcropping close by. J.E.L. Caiger worked in Kent excavating, surveying and researching deneholes and concluded that they were excavated in prehistoric, Roman, medieval and even post-medieval times in order to produce a supply of unpolluted chalk to spread on fields for the purposes of marling. By excavating a narrow shaft, the miners used up as little of the productive agricultural land as possible. He suggested various other practical issues which supported his ideas including that open cast chalk extraction would require moving the material further than necessary and that shallower chalk deposits have much of their minor mineral content leached out by groundwater.

One other theory has been advanced, viz, that the excavations were made in order to get flints for implements, but this is quite impossible, as a careful examination of a few examples will show.

Further references

  • Essex Dene-holes by T.V. Holmes and W Cole; The Archaeological Journal (1882); the Transactions of the Essex Field Club; Archaeologia Cantiana. &c.;
  • Deneholes by F. W. Reader, in Old Essex, ed. A. C. Kelway (1908).
  • F.C.J. Spurrell's paper 'Deneholes and Artificial Caves with Vertical Entrances', published in the Archaeological Journal for 1881 and 1882.

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