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all geography including DSDP/ODP Sites and Legs
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Africa
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Gibraltar
Gibraltar subduction zone is invading the Atlantic
Arc-related high-K magmatism in the Ceuta Peninsula (Internal Rif, Spain): discovery and consequences
CUSTODIAN OF THE GIBRALTAR SKULL: THE HISTORY OF THE GIBRALTAR SCIENTIFIC SOCIETY
Reconstructing chemical weathering during the Lower Mesozoic in the Western-Central Mediterranean area: a review of geochemical proxies
The Alboran domain in the western Mediterranean evolution: the birth of a concept
Spatial Variation of Lg ‐Wave Attenuation in the Iberian Peninsula
BRITISH PIONEERS OF THE GEOLOGY OF GIBRALTAR, PART 3: E. B. BAILEY AND ROYAL ENGINEERS 1943 TO 1953
BRITISH PIONEERS OF THE GEOLOGY OF GIBRALTAR, PART 2: CAVE ARCHAEOLOGY AND GEOLOGICAL SURVEY OF THE ROCK, 1863 TO 1878
BRITISH PIONEERS OF THE GEOLOGY OF GIBRALTAR, PART 1: THE ARTILLERYMAN THOMAS JAMES ( ca 1720–1782); INFANTRYMAN NINIAN IMRIE OF DENMUIR ( ca 1752–1820); and EX-MILITIAMAN JAMES SMITH OF JORDANHILL (1782–1867)
Ground‐Motion Models for Seismic‐Hazard Assessment in Western Iberia: Constraints from Instrumental Data and Intensity Observations
A Dominant Tectonic Signal in High-Frequency, Peritidal Carbonate Cycles? A Regional Analysis of Liassic Platforms from Western Tethys
Structural evolution of the external zones derived from the Flysch trough and the South Iberian and Maghrebian paleomargins around the Gibraltar arc: a comparative study
Evidence for active subduction beneath Gibraltar
Military engineering on the Rock of Gibraltar and its geoenvironmental legacy
Abstract The 400-m-high Rock of Gibraltar is a partly overturned klippe of Early Jurassic dolomitic limestone, notched by raised shorelines and flanked by Quaternary scree breccias and windblown sands. It dominates a narrow 5-km-long peninsula jutting south from Spain at the western entrance to the Mediterranean Sea. Fortified from at least 1160 to World War II successively by the Moors, Spanish, and British, and subjected to 15 major sieges between 1309 and the Cold War of 1947 to 1989, Gibraltar is arguably one of the most densely fortified and fought over places in Europe. Stone walls, bastions, and numerous artillery positions built to enhance the natural defenses of the coastal cliffs now provide a tourist attraction, but constrain development of the modern city. Occasional rockfalls and the need for slope-safety measures are continuing concerns, especially in areas of scree breccia quarried to provide fill for the extension of a Royal Navy harbor between 1893 and 1905 and a Royal Air Force airfield largely between 1941 and 1943. Water supply has posed a problem throughout the history of the fortress, leading to innovative development of rainwater catchment areas on natural slopes, dual potable/sanitary water supplies, and projects to enhance these by cloud condensation or groundwater abstraction, before near total commitment to desalination from 1993. Tunnels and underground chambers are major features of the Rock. Mostly excavated in five phases between 1782 and 1968 to provide access, reservoirs, accommodation, or storage, they now total over 50 km in length, generally unlined. Tunnel integrity is dependent on excavation technique and bedrock characteristics. From the early eighteenth century to recent years, much of the major construction work on Gibraltar was directed and often carried out by Royal Engineers. In 1994, disbandment of 1st (Fortress) Specialist Team RE brought over two centuries of British military engineering on the Rock to an end—and provided a legacy of works and land now largely inherited by civilian bodies responsible to the Gibraltar government.