Here are some cards arriving these days. Thank you so much all.
Ironbridge Gorge
United Kingdom of Great Britain and Northern Ireland
ỦNESCO site
Date of Inscription: 1986
The Ironbridge Gorge World Heritage property covers an area
of 5.5 km2 (550 ha) and is located in Telford, Shropshire, approximately 50 km
north-west of Birmingham .
The Industrial Revolution had its 18th century roots in the Ironbridge Gorge
and spread worldwide leading to some of the most far-reaching changes in human
history.
The site incorporates a 5 km length of the steep-sided,
mineral-rich Severn Valley from a point immediately west of Ironbridge
downstream to Coalport, together with two smaller river valleys extending
northwards to Coalbrookdale and Madeley.
The Ironbridge Gorge provided the raw materials that
revolutionised industrial processes and offers a powerful insight into the
origins of the Industrial Revolution and also contains extensive evidence and
remains of that period when the area was the focus of international attention
from artists, engineers, and writers. The property contains substantial remains
of mines, pit mounds, spoil heaps, foundries, factories, workshops, warehouses,
iron masters’ and workers’ housing, public buildings, infrastructure, and
transport systems, together with the traditional landscape and forests of the
Severn Gorge. In addition, there also remain extensive collections of artifacts
and archives relating to the individuals, processes and products that made the
area so important.
Today, the site is a living, working community with a
population of approximately 4000 people as well as a world renowned place to
visit. It is also a historic landscape that is interpreted and made accessible
through the work of a number of organisations, in particular, the Ironbridge
Gorge Museum Trust (established in 1967 to preserve and interpret the remains
of the Industrial Revolution within the Ironbridge Gorge) and the Severn Gorge
Countryside Trust (established in 1991 to manage the woodland, grassland and
associated historic structures in the Gorge).
Within the property, five features are highlighted as of
particular interest. It was in Coalbrookdale in 1709 that the Quaker Abraham
Darby I developed the production technique of smelting iron with coke which
began the great 18th century iron revolution. There still remains a high
concentration of 18th and 19th century dwellings, warehouses and public
buildings in Coalbrookdale. In Ironbridge, the community draws its name from
the famous Iron Bridge erected in 1779 by Abraham Darby
III. At the eastern end of Ironbridge stand the remains of two 18th century
blast furnaces, the Bedlam Furnaces, built in 1757. In Hay Brook Valley , south of Madeley, lies a large
open-air museum which incorporates the remains of the former Blists Hill blast
furnaces and Blists Hill brick and tile works. Also of importance is the
spectacular Hay Inclined Plane, which connected the Shropshire
Canal to the Coalport Canal ,
which in turn linked with the River Severn. The small community of Jackfield on
the south bank of the River Severn was important for navigation, coal mining,
clay production, and the manufacture of decorative tiles. Located at the
eastern end of the property and on the north bank of the River Severn,
industrialisation came to Coalport in the late 18th century and the area is
remembered principally for the Coalport China Works.
Parc national Plitvice
Croatia
UNESCO site
Date of Inscription: 1979
The Plitvice
Lakes basin is a
geomorphologic formation of biological origin, a karst river basin of limestone
and dolomite, with approximately 20 lakes, created by the deposition of calcium
carbonate precipitated in water through the agency of moss, algae and aquatic
bacteria. These create strange, characteristic shapes and contain
travertine-roofed and vaulted caves. The carbonates date from the Upper Trias , Juras and Cretaceous Ages and are up to
4,000 m thick. In order to maintain and preserve the natural characteristics of
the lakes, the whole of surface and most of the subterranean drainage system
has to be embraced by extending the original borders of the park. The new areas
comprise layers of karstified limestone with dolomites of Jurassic age.
There are 16 interlinked lakes between Mala
Kapela Mountain
and Pljesevica Mountain . The lake system is divided
into the upper and lower lakes: the upper lakes lie in a dolomite valley and
are surrounded by thick forests and interlinked by numerous waterfalls; the
lower lakes, smaller and shallower, lie on the limestone bedrock and are
surrounded only by sparse underbrush. The upper lakes are separated by dolomite
barriers, which grow with the formation of travertine, forming thus travertine
barriers. Travertine is mostly formed on the spots where water falls from an
elevation, by the incrustation of algae and moss with calcium carbonate. The
lower lakes were formed by crumbling and caving-in of the vaults above
subterranean cavities through which water of the upper lakes disappeared.
The forest, that comprises pure stands of beech at lower
altitudes and mixed stands of beech and fir at higher levels, can also be classified
in terms of underlying strata of dolomite and limestone complexes. The dolomite
communities comprise tertiary pine, hornbeam, spruce and beech-fir forests. The
limestone communities have a smaller number of forest types but cover a larger
area with communities of spruce and fern, spruce in beech, coppiced hornbeam
with sumac, maple and heather. Hydrophytic communities of black alder, grey
ivy, willow, reeds and bulrush communities are found. There are a large mosaic
of meadow communities, depending on altitude, geology soils and other
ecological factors.
The area is fauna-rich, including European brown bear, wolf,
eagle owl and capercaillie. There are records of 126 species of bird, of which
70 breed.
The area was the cradle of the prehistoric Illyrian tribe of
Japuds dating from 1000 BC. The Japudic culture was followed by the Romans and
from the 8th century AD was occupied by Slavs. Archaeological remains include a
prehistoric settlement on the site of the current Plitvice village,
fortifications, Bronze Age tools and ceramics.
Venice
and its Lagoon
Province of Venezia , Veneto Region ,
Italy
UNESCO site
Date of inscription: 1987
Founded in the 5th century AD and spread over 118 small
islands, Venice
became a major maritime power in the 10th century. The whole city is an
extraordinary architectural masterpiece in which even the smallest building
contains works by some of the world's greatest artists such as Giorgione,
Titian, Tintoretto, Veronese and others.
In this lagoon covering 50,000 km², nature and history have
been closely linked since the 5th century when Venetian populations, to escape
barbarian raids, found refuge on the sandy islands of Torcello, Jesolo and
Malamocco. These temporary settlements gradually became permanent and the
initial refuge of the land-dwelling peasants and fishermen became a maritime
power. Over the centuries, during the entire period of the expansion of Venice , when it was obliged to defend its trading markets
against the commercial undertakings of the Arabs, the Genoese and the Ottoman
Turks, Venice
never ceased to consolidate its position in the lagoon.
In this inland sea that has continuously been under threat,
rises amid a tiny archipelago at the very edge of the waves one of the most
extraordinary built-up areas of the Middle Ages. From Torcello to the north to Chioggia to the south,
almost every small island had its own settlement, town, fishing village and
artisan village (Murano). However, at the heart of the lagoon, Venice itself stood as one of the greatest
capitals in the medieval world. When a group of tiny islands were consolidated
and organized in a unique urban system, nothing remained of the primitive
topography but what became canals, such as the Giudecca Canal, St Mark's Canal
and the Great Canal, and a network of small rii that are the veritable arteries
of a city on water.
Source: UNESCO.org
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