In classical times the peak had 25 quarries on the south slope at elevations between 2 500 and 3 300 feet 760 and 1000 m.
Pentelic marble quarry.
2 5 pentelic marble is divided into 3 units distinguishable by δ 13 c and δ 18 o values.
The chief summit about 10 miles 16 km northeast of athens athína is kokkinarás 3 632 feet 1 107 m which yields white pentelic marble on its north slope.
The company is located at prosotsani drama greece.
Marble was called at the time as white stone or pentelic hymettus or parian stone and apart from the quarries of paros and naxos that were already famous since the archaic era the exploitation of the pentelicus quarry began in the classical era.
These quarries are self owned and located at dionyssos attica.
Quarrying here began more than 100 years ago.
Marble is a metamorphic rock composed of recrystallized carbonate minerals most commonly calcite or dolomite marble is typically not foliated although there are exceptions in geology the term marble refers to metamorphosed limestone but its use in stonemasonry more broadly encompasses unmetamorphosed limestone.
Other articles where pentelic marble is discussed.
They produce the world renowned dionyssos pentelicon marble.
In classical times the peak had 25 quarries on the south slope at elevations between 2 500 and 3 300 feet 760 and 1000 m.
This area drama kavala thassos is widely known for producing almost 50 of the total greek white marble semi white marble production.
Pentelic marble was quarried during the golden age of pericles 5th century b c.
These provided excellent marble for most of the buildings and sculptures of athens in the 5th.
δ 13 c and δ 18 o values have been used to precisely match marbles from the acropolis to their source quarries.
Topalidis marble granite is a greek white marble manufacturer with own quarries and has been in the greek stone industry for years.
Marble is commonly used for sculpture and as a building material.
Pentelic marble from the quarries at penteli north of athens is a fine grained calcitic marble.
S a the company solely responsible for its exploitation.
It is fine grained with sporadic calcitic fossil clasts.
Pentelic marble is calcitic in composition with quartz as an accessory mineral.
It is white with a golden tinge.
In athens and supplied thousands of cubic metres of material used to construct the athens acropolis monuments and in the creation of all the great classical hellenistic and roman statues.
The quarry region is at dionysos of attica at dionyssovouni site and has the same chemical composition and texture as the renowned since antiquity pentelic marble.
1 107 m which yields white pentelic marble on its north slope.
