Grotte De Rosée
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The ''Grotte de Rosée'' (Cave of Rosée) is located near
Éhein Éhein ( wa, Éhin) is a village of Wallonia and a district of the municipality of Neupré, located in the province of Liège, Belgium. It was a municipality until the fusion of the Belgian municipalities in 1977. Caves The rock has many caves, ...
in the municipality of
Engis Engis (; wa, Indji) is a municipality of Wallonia located in the province of Liège, Belgium. On 1 January 2006 Engis had a total population of 5,686. The total area is 27.74 km² which gives a population density of 205 inhabitants per km ...
, in Belgium. It has been classified as
Wallonia Wallonia (; french: Wallonie ), or ; nl, Wallonië ; wa, Waloneye or officially the Walloon Region (french: link=no, Région wallonne),; nl, link=no, Waals gewest; wa, link=no, Redjon walone is one of the three regions of Belgium—alo ...
's ''patrimoine immobilier exceptionnel de la Région wallonne'' ('exceptional heritage of Wallonia'), and can be visited only by accredited scientists. It houses a set of
concretions A concretion is a hard, compact mass of matter formed by the precipitation of mineral cement within the spaces between particles, and is found in sedimentary rock or soil. Concretions are often ovoid or spherical in shape, although irregular ...
which is unique in Belgium.


Location

The cave is located in
Éhein Éhein ( wa, Éhin) is a village of Wallonia and a district of the municipality of Neupré, located in the province of Liège, Belgium. It was a municipality until the fusion of the Belgian municipalities in 1977. Caves The rock has many caves, ...
, along the valley of the creek Engihoul, bordered by the road "of the 36 turns", in a
syncline In structural geology, a syncline is a fold with younger layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. A synclinorium (plural synclinoriums or synclinoria) is a large syncline with superimpose ...
formed in the
limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...
of Visean, near ''carrière du Lion'', the "Lion's quarry".


Discovery and designation

The ''Grotte de Rosée'' was discovered in July 1906, following a fire pit in a quarry belonging to the baron Jacques de Rosée. Workers then used the cavity, which appeared as a vertical chimney, to pour hundreds of wheelbarrows of rubble into.E. Van den Broeck, E.-A. Martel et Ed. Rahir, ''Les cavernes et les rivières souterraines de la Belgique étudiées spécialement dans leurs rapports avec l'hydrologie des calcaires et avec la question des eaux potables'', T. II ''Les calcaires carbonifériens du bassin de Dinant et coup d'œil sur le bassin de Namur'', H. Lamertin, Bruxelles, 1910, p.53 à 66 des Annexes. On 15 September, a serious exploration was initiated by A. Vandebosch, supervisor at ''Concasseur des Arwis'', and his friend Ernest Doudou. At the bottom of the chimney (about 12 feet long), they discovered a huge room, a domain "much more reserved to fairies and sylphs than to be trodden by the brutal foot of man", according to Doudou; they named that room "the Crystal Palace". Based on a proposal by E. Van den Broeck, who soon visited the place, the cave was named by the owner, who in turn allowed researchers to investigate it, and protected access to it. The exploration proved to dangerous that the workers refused to continue, leaving the work to the scientists Cosyns, Doudou, and Colette.


Description

The ''Grotte de Rosée'' consists of a vast network of rooms, corridors and galleries sometimes parallel, sometimes perpendicular, which intersect on several levels, punctuated by wells, chimneys,
siphon A siphon (from grc, σίφων, síphōn, "pipe, tube", also spelled nonetymologically syphon) is any of a wide variety of devices that involve the flow of liquids through tubes. In a narrower sense, the word refers particularly to a tube in a ...
, tunnels, etc. It is partially covered by an underground stream. The most impressive room is the ''Crystal Palace'' with its
giant's kettle A giant's kettle, also known as either a giant's cauldron, moulin pothole, or glacial pothole, is a typically large and cylindrical pothole drilled in solid rock underlying a glacier either by water descending down a deep moulin or by gravel r ...
s and domes, waterfalls
stalactite A stalactite (, ; from the Greek 'stalaktos' ('dripping') via ''stalassein'' ('to drip') is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble an ...
s, and
stalagmite A stalagmite (, ; from the Greek , from , "dropping, trickling") is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically ...
s, the main candle being 2.8 m high with a diameter of 60 cm, snowy regions, and across space a shower of
hyaline A hyaline substance is one with a glassy appearance. The word is derived from el, ὑάλινος, translit=hyálinos, lit=transparent, and el, ὕαλος, translit=hýalos, lit=crystal, glass, label=none. Histopathology Hyaline cartilage is ...
crystalline tubes, 5 cm diameter for heights ranging from 1 to 2 m and,
fistula A fistula (plural: fistulas or fistulae ; from Latin ''fistula'', "tube, pipe") in anatomy is an abnormal connection between two hollow spaces (technically, two epithelialized surfaces), such as blood vessels, intestines, or other hollow or ...
s, crystal wands all hollow and containing water. Other eccentric crystallization, formed by capillarity in the most diverse forms (draperies, hooks, buckles, screws, etc..). exist in large numbers, reminiscent of the corals or strange flowers. In the second room, there are also quirky and stalactites concretions like swords. Further west, the cave offers view of stalagmites and draperies red currant and even stalagmites.


Classification as exceptional heritage

The ''Grotte de Rosée'' is classified, with the cave Lyell (named after
Charles Lyell Sir Charles Lyell, 1st Baronet, (14 November 1797 – 22 February 1875) was a Scottish geologist who demonstrated the power of known natural causes in explaining the earth's history. He is best known as the author of ''Principles of Geolo ...
; both are in fact two parts of the same site), ''patrimoine immobilier exceptionnel de la Région wallonne'' (exceptional heritage of Wallonia), under "underground site exceptional," by order of 8 July 1977.Fiche de la Région wallonne
/ref> It is accessible only to researchers due to the fragility of many concretions and because the opening to tourists and recreational cavers also would result in a change in the natural balance of the biotope, by changes in temperature and light, trampling of clay and nutrient that benefit some species, taking into account that the study of this fauna is still very little progress in this cave.


References


Sources

*This page has been initially translated from '' Grotte de Rosée'' on the French Wikipedia, under CC-BY-SA license. See the /fr.wikipedia.org/w/index.php?title=Grotte_de_Ros%C3%A9e&action=history list of authors {{DEFAULTSORT:Grotte de Rosee Limestone caves Rosee Landforms of Liège Province