vrijdag 6 november 2015

Republic of Korea, Royal Tombs of the Joseon Dynasty

The Royal Tombs of the Joseon Dynasty form a collection of 40 tombs scattered over 18 locations. Built over five centuries, from 1408 to 1966, the tombs honoured the memory of ancestors, showed respect for their achievements, asserted royal authority, protected ancestral spirits from evil and provided protection from vandalism. Spots of outstanding natural beauty were chosen for the tombs which typically have their back protected by a hill as they face south toward water and, ideally, layers of mountain ridges in the distance. Alongside the burial area, the royal tombs feature a ceremonial area and an entrance. In addition to the burial mounds, associated buildings that are an integral part of the tombs include a T-shaped wooden shrine, a shed for stele, a royal kitchen and a guards’ house, a red-spiked gate and the tomb keeper’s house. The grounds are adorned on the outside with a range of stone objects including figures of people and animals. The Joseon Tombs completes the 5,000 year history of royal tombs architecture in the Korean peninsula.


United Kingdom, Castles and Town Walls of King Edward in Gwynedd

The castles of Beaumaris and Harlech (largely the work of the greatest military engineer of the time, James of St George) and the fortified complexes of Caernarfon and Conwy are located in the former principality of Gwynedd, in north Wales. These extremely well-preserved monuments are examples of the colonization and defence works carried out throughout the reign of Edward I (1272–1307) and the military architecture of the time.


Australia, Macquarie Island

Macquarie Island (34 km long x 5 km wide) is an oceanic island in the Southern Ocean, lying 1,500 km south-east of Tasmania and approximately halfway between Australia and the Antarctic continent. The island is the exposed crest of the undersea Macquarie Ridge, raised to its present position where the Indo-Australian tectonic plate meets the Pacific plate. It is a site of major geoconservation significance, being the only place on earth where rocks from the earth’s mantle (6 km below the ocean floor) are being actively exposed above sea-level. These unique exposures include excellent examples of pillow basalts and other extrusive rocks.