Genista Caves

Last updated
Genista Cave
LocationWindmill Hill, Gibraltar
Coordinates 36°07′02″N5°20′52″W / 36.11733°N 5.34768°W / 36.11733; -5.34768

The Genista Caves are a series of caves located under Windmill Hill in the British Overseas Territory of Gibraltar. Fossils of various mammals and human remains were discovered here in the mid-1860s. [1] The name of the caves is a play on words based on Captain Frederick Brome's name, who discovered them.

History

Captain Frederick Brome excavated Genista I Cave in the 1860s. Brome’s investigations were so thorough that they prompted scientists of the calibre of Hugh Falconer and George Busk, secretaries of the Royal Society and the Linnean Society respectively, to visit Gibraltar in search of the breccias. [2] Brome had taken up the appointment of Governor of the Military Prison on Windmill Hill, an ancient wave-cut platform at the southern end of Gibraltar where a system of fissure caves, known as the Genista Caves are situated. The largest and most important is Genista I which was discovered by Brome. He used his prisoners to excavate this deep fissure which yielded large quantities of bone some of which are thought to be the oldest found in Gibraltar. The fauna included brown bear, wild cat, lynx, leopard, spotted hyena, horse, narrow-nosed rhinoceros, wild boar, red deer, aurochs and ibex. [3]

The exploration of the caves commenced as a result of a decision taken in 1862 to enlarge the boundaries of the military prison and to construct a large water tank. According to George Busk (1868):

“Within the enclosed space (for the water tank), and close to the south-east angle, an excavation was made for the proposed tank. This excavation led to the discovery of the first and most important of the series of caves on the Windmill Hill Plateau, which it is to be hoped will be known to all time by the name which has been given to them, in allusion and in honour of their discoverer and explorer.”

Busk was humorously referring to Genista as the Latin name of the broom, a Mediterranean shrub, as a play of words with Brome. Brome obtained the Secretary of State’s approval, at his suggestion, to employ prisoners on the new works and their construction and he kept a close supervision over what was going on. He clearly had great vision and intuition when it came to caves. He described the first time he found the fissure which was to lead to the discovery of Genista I like this:

“On removing the earth from this space, which varied from two to four feet in depth, an irregular surface of compact limestone presented itself; in which the only fissure visible was an open vertical one about six feet long and five inches wide, between two large blocks of limestone; the disturbed state and the peculiar position of these masses appeared to me, with the fissure, to be remarkable, and I drew the attention of Lieutenant Buckle, RE, in charge of the works, to them, who observed that ‘it was merely one of those fissures in which the Rock of Gibraltar abounded.’ Labour was directed to quarry out the limestone to the required depth for the tank, and, about the end of February, after blasting out a proportion of solid rock at a depth of nine feet from the original surface, a few bones were found in the bottom of a small fissure, under some dark mould; they were lying without order in all directions, and mostly fractured. [3]

He was a thorough researcher and gained the respect of the scientists of the day with whom he corresponded. Busk, for example, wrote thus:

“Fortunately when the excavations on Windmill Hill were commenced, an accomplished and distinguished officer, fully alive to the importance of science, was in command of the fortress; and it was equally fortunate that the subsequent explorations were carried out by an observer so able, energetic and vigilant as Captain Frederick Brome, at that time Governor of the Prison. These operations, which were continued from April 1863 to December 1868, have of necessity required an amount of labour, and involved sometimes a degree of responsibility which it is not very easy to over-estimate. But this labour and responsibility have been ungrudgingly and most disinterestedly given and incurred by Captain Brome, who, with the aid of prisoners and their warders under his command, has in those five years conducted with surprising success an amount of difficult exploration never before equalled, and made collections in the public interest of unrivalled value.” [3]

Brome also discovered Genista II which was a smaller cave. Genista III and Genista IV followed and all showed some evidence of habitation but Genista four was very inaccessible and was thought be a place of refuge rather than a place to live as its entrance was forty feet down from the summit on a cliff face of the Rock of Gibraltar. Most of the Genista floors are covered in stalagmites and investigators found human remains, pottery and broken bones. One possibility is that the caves were used as a place to live but after being abandoned they were reused as burial places. [4]

The excavations revealed the bones of a large number of what are now locally extinct animals including lynx, leopard, hyena, rhinoceros and aurochs. They had evidently fallen through fissures in the surface and perished. Unfortunately the cave entrance was later lost or destroyed when a large magazine was built directly overhead at the end of the 19th century. [5]

Related Research Articles

<span class="mw-page-title-main">Wookey Hole Caves</span> Series of limestone caverns in Somerset county, England

Wookey Hole Caves are a series of limestone caverns, a show cave and tourist attraction in the village of Wookey Hole on the southern edge of the Mendip Hills near Wells in Somerset, England. The River Axe flows through the cave. It is a Site of Special Scientific Interest (SSSI) for both biological and geological reasons. Wookey Hole cave is a "solutional cave", one that is formed by a process of weathering in which the natural acid in groundwater dissolves the rocks. Some water originates as rain that flows into streams on impervious rocks on the plateau before sinking at the limestone boundary into cave systems such as Swildon's Hole, Eastwater Cavern and St Cuthbert's Swallet; the rest is rain that percolates directly through the limestone. The temperature in the caves is a constant 11 °C (52 °F).

<span class="mw-page-title-main">Zhoukoudian Peking Man Site</span> Cave complex and archaeological site in China

Zhoukoudian Peking Man Site (周口店北京人遗址), also romanized as Choukoutien, is a cave system in suburban Fangshan District, Beijing. It has yielded many archaeological discoveries, including one of the first specimens of Homo erectus, dubbed Peking Man, and a fine assemblage of bones of the giant short-faced hyena Pachycrocuta brevirostris.

<span class="mw-page-title-main">Kirkdale Cave</span> Cave in North Yorkshire, England

Kirkdale Cave is a cave and fossil site located in Kirkdale near Kirkbymoorside in the Vale of Pickering, North Yorkshire, England. It was discovered by workmen in 1821, and found to contain fossilized bones of a variety of mammals not currently found in Great Britain, including hippopotamuses, elephants and cave hyenas.

<span class="mw-page-title-main">St. Michael's Cave</span> Caves in Gibraltar

St. Michael's Cave or Old St. Michael's Cave is the name given to a network of limestone caves located within the Upper Rock Nature Reserve in the British Overseas Territory of Gibraltar, at a height of over 300 metres (980 ft) above sea level. According to Alonso Hernández del Portillo, the first historian of Gibraltar, its name is derived from a similar grotto in Monte Gargano near the Sanctuary of Monte Sant'Angelo in Apulia, Italy, where the archangel Michael is said to have appeared.

<span class="mw-page-title-main">Risovača Cave</span> Cave and archaeological site in Serbia

Risovača Cave, is situated at the very entrance of the town of Aranđelovac in central Serbia around 17 m (56 ft) above the Kubršnica river valley. It is one of the most important archaeological sites of the Paleolithic in Serbia besides the Gradac Cave near Kragujevac. Its discovery confirmed the assumed existence of the Paleolithic culture south of the Sava-Danube line and provided new information on the life of prehistoric humans in Europe.

<span class="mw-page-title-main">King Arthur's Cave</span>

King Arthur's Cave is a limestone cave at the foot of a low cliff at the north-western end of Lord's Wood in The Doward, near Symonds Yat, Herefordshire, about four miles northeast of Monmouth, in the Wye Valley. The cave entrance lies about 285 feet above the River Wye on a hill, with a double interconnected entrance and two main chambers. It is protected as a nature reserve under the Herefordshire Nature Trust. There is evidence that the cave was occupied by man during the Upper Palaeolithic era, and flint tools and woolly mammoth bones have been unearthed within and around the caves.

<span class="mw-page-title-main">Martin's Cave</span>

Martin's Cave is a cave in the British Overseas Territory of Gibraltar. It opens on the eastern cliffs of the Rock of Gibraltar, below its summit at O'Hara's Battery. It is an ancient sea cave, though it is now located over 700 feet (210 m) above the shore of the Mediterranean Sea. It is only accessible because Martin's Path was constructed.

<span class="mw-page-title-main">Poca Roca Cave</span> Cave in the British Overseas Territory of Gibraltar

Poca Roca Cave is a cave in the British Overseas Territory of Gibraltar.

Cave S is a limestone cave in the British Overseas Territory of Gibraltar. It is located on the eastern side of the Rock of Gibraltar, near Holy Boy's Cave. Human remains were found in the cave in 1910 that did not appear to be of a modern man.

<span class="mw-page-title-main">Goat's Hair Twin Caves</span> Cave in the British Overseas Territory of Gibraltar

The Goat's Hair Twin Caves are in the British Overseas Territory of Gibraltar.

Judge's Cave is a cave in the British Overseas Territory of Gibraltar. Human remains dated to the late prehistoric period have been unearthed in the cave.

<span class="mw-page-title-main">Leonora's Caves</span> Limestone cave system in the British Overseas Territory of Gibraltar

Leonora's Caves is a limestone cave system in the British Overseas Territory of Gibraltar. They are located within Old St. Michael's Cave.

Genista Battery is an artillery battery in the British Overseas Territory of Gibraltar.

<span class="mw-page-title-main">Neanderthals in Gibraltar</span>

The Neanderthals in Gibraltar were among the first to be discovered by modern scientists and have been among the most well studied of their species according to a number of extinction studies which emphasize regional differences, usually claiming the Iberian Peninsula partially acted as a “refuge” for the shrinking Neanderthal populations and the Gibraltar population of Neanderthals as having been one of many dwindling populations of archaic human populations, existing just until around 42,000 years ago. Many other Neanderthal populations went extinct around the same time.

<span class="mw-page-title-main">Windmill Hill (Gibraltar)</span> A pair of plateaux

Windmill Hill or Windmill Hill Flats is one of a pair of plateaux, known collectively as the Southern Plateaux, at the southern end of the British Overseas Territory of Gibraltar. It is located just to the south of the Rock of Gibraltar, which descends steeply to the plateau. Windmill Hill slopes down gently to the south with a height varying from 120 metres (390 ft) at the north end to 90 metres (300 ft) at the south end. It covers an area of about 19 hectares, though about 6 hectares at the north end is built over. The plateau is ringed to the south and east with a line of cliffs which descend to the second of the Southern Plateaux, Europa Flats, which is itself ringed by sea cliffs. Both plateaux are the product of marine erosion during the Quaternary period and subsequent tectonic uplift. Windmill Hill was originally on the shoreline and its cliffs were cut by the action of waves, before the ground was uplifted and the shoreline moved further out to the edge of what is now Europa Flats.

<span class="mw-page-title-main">Mladeč caves</span> Cave complex and archaeological site in the Czech Republic

The Mladečské Caves are a cave complex in the municipality of Mladeč in the Czech Republic. It is located in the Třesín National Nature Monument within the Litovelské Pomoraví Protected Landscape Area.

<span class="mw-page-title-main">Ash Hole Cavern</span> Cave in Brixham, Devon, England

Ash Hole Cavern is a limestone cave system in Brixham, Devon, England. There is evidence of human habitation since Neolithic times, and archaeological excavations have been conducted, with several artefacts found. It has been a scheduled monument since 1966.

<span class="mw-page-title-main">Pešturina</span> Cave and archaeological site in Serbia

Pešturina is a cave in the municipality of Niška Banja in southeast Serbia. It is located southwest of Jelašnica and 20 km (12 mi) southeast of Niš. Artifacts from the Middle and Upper Paleolithic periods were discovered since the archaeological excavations began in 2006. The remains, identified as the Mousterian culture, were dated from 111,000 BP+ 5,000 to 39,000 BP + 3,000, which makes Pešturina one of the latest surviving Neanderthal habitats. The cave has been nicknamed the "Serbian Atapuerca".

<span class="mw-page-title-main">Windmill Hill Cavern</span> Cave and archaeological site in Devon, England

Windmill Hill Cavern is a limestone cave system in the town of Brixham, Devon. It was discovered in 1858 and later excavated by a team led by the geologist William Pengelly, who found proof that humans co-existed with extinct British fauna.

Dream Cave is a natural limestone cavern located near Wirksworth in Derbyshire, England. It was discovered by lead miners in 1822 and was found to contain the almost complete skeletal remains of a woolly rhinoceros and other large mammal bones. These remains were acquired by the geologist William Buckland and are now housed in Oxford Museum.

References

This article uses freely licensed text generously shared by underground-gibraltar.com
  1. "On the fossil contents of the Genista cave, Gibraltar". Quarterly Journal of the Geological Society. Archived from the original on 21 February 2013. Retrieved 17 January 2013.
  2. Busk, G.; Falconer, H. (1 January 1865). "On the Fossil Contents of the Genista Cave, Gibraltar". Quarterly Journal of the Geological Society. 21 (1–2): 364–370. doi:10.1144/GSL.JGS.1865.021.01-02.35. S2CID   131067735 . Retrieved 18 January 2013.
  3. 1 2 3 Genista Caves, Underground-Gibraltar.com, accessed 8 January 2013
  4. Boyd Dawkins, W (February 2009). Echo Library. Echo Library. p. 205. ISBN   9781848301870.
  5. "Captain Frederick Brome and Genista I Cave, Gibraltar". Gibraltar Museum Caving Unit. Retrieved 28 June 2013.