VOLCANIC ERUPTIONS AND GEOLOGICAL FORMATION

Posted on 27th Nisan 2008 by admin in Cappadocia

Mount Erciyes, Hasandagi and Golludag were active volcanoes in the geological periods. Alongside with many other volcanoes, eruptions of these volcanoes started in the Early Miocene (10 million years ago) and have continued until the present day.

 

The lava produced by these volcanoes, under the Neogene lakes, formed a layer of tufa on the plateaus, which varied in hardness and was between 100 and 150m thick. Other substances in the layer are ignimbrite, soft tufa, tufa, lahar, ash, clay, sandstone, marn, basalt and other agglomerates.

Plateaus, having been essentially shaped with the lava from the bigger volcanoes, were continuously altered with the eruptions of smaller volcanoes. Starting in the Early Pliocene Period, the rivers in the area, especially Kizilirmak (the Red River), and local lakes contributed to the erosion of this layer of tufa stone, eventually giving the area its present day shape.

Fascinating Curves
Another characteristic feature of the area is the sweeping curves on the sides of the valleys, formed by rainwater. The array of colors seen on some of the valleys is due to the difference in heat of the lava layers. Such patterns can be seen in Uchisar, Cavusin/ Güllüdere, Goreme/ Meskendir, Ortahisar/Kizilçukur and Pancarlik valleys.

Formation of Fairy Chimneys

Posted on 26th Nisan 2008 by admin in Cappadocia

The interesting rock formations, known as “fairy chimneys”, have been formed as the result of the erosion of this tufa layer, sculpted by wind and flood water, running down on the slopes of the valleys. Water has found its way through the valleys creating cracks and ruptures in the hard rock. The softer, easily erodable material underneath has been gradually swept away receding the slopes and in this way, conical formations protected with basalt caps have been created.

 

The fairy chimneys with caps, mainly found in the vicinity of Urgup, have a conical shaped body and a boulder on top of it. The cone is constructed from tufa and volcanic ash, while the cap is of hard, more resistant rock such as lahar or ignimbrite. Various types of fairy chimneys are found in Cappadocia. Among these are those with caps, cones, mushroom like forms, columns and pointed rocks.

Fairy chimneys are generally found in the valleys of the Uchisar- Ürgüp-Avanos triangle, between Urgup and Sahinefendi, around the town of Cat in Nevsehir, in the Sogani valley in Kayseri, and in the village of Selime in Aksaray.

Cappadocia Modern tourism

Posted on 17th Nisan 2008 by admin in Cappadocia

The area is a famous and popular tourist destination, as it has many areas with unique geological, historic and cultural features.

The region is southwest of the major city Kayseri, which has airline and railroad service to Ankara and Istanbul.

The Cappadocia region is largely underlain by sedimentary rocks formed in lakes and streams, and ignimbrite deposits erupted from ancient volcanoes approximately 9 to 3 million years ago (late Miocene to Pliocene epochs). The rocks of Cappadocia near Göreme eroded into hundreds of spectacular pillars and minaret-like forms. The volcanic deposits are soft rocks that the people of the villages at the heart of the Cappadocia Region carved out to form houses, churches, monasteries. Göreme became a monastic center between 300-1200 AD. First period settlement in Göreme reaches to the Roman period from Christianity. Yusuf Koç, Ortahane, Durmus Kadir and Bezirhane churches in Göreme, houses and churches carved into rocks till to Uzundere, Bağıldere and Zemi Valley carries the mystical side of history today. The Göreme Open Air Museum is the most visited site of the monastic communities in Cappadocia and is one of the most famous sites in central Turkey. It is a complex comprising more than 30 rock-carved churches and chapels containing some superb frescoes, dating from the 9th to the 11th centuries.

Cappadocia History

Posted on 16th Nisan 2008 by admin in Cappadocia

Cappadocia was known as Hatti in the late Bronze Age, and was the homeland of the Hittite power centred at Hattusa. After the fall of the Hittite Empire, with the decline of the Syro-Cappadocians (Mushki) after their defeat by the Lydian king Croesus in the 6th century, Cappadocia was left in the power of a sort of feudal aristocracy, dwelling in strong castles and keeping the peasants in a servile condition, which later made them apt for foreign slavery. It was included in the third Persian satrapy in the division established by Darius, but long continued to be governed by rulers of its own, none apparently supreme over the whole country and all more or less tributary to the Great King.

After bringing the Persian Empire to an end, Alexander the Great met with great resistance in Cappadocia. He tried to rule the area through one of his commanders named Sabictus, but the ruling classes and people resisted and declared Ariarathes, a Persian aristocrat, as king. This sent a message to Alexander that not all Persians would submit to his rule. Ariarthes I (332 - 322 BC) was a successful ruler, and extended the borders of the Cappadocian Kingdom as far as the Black Sea. The kingdom of Cappadocia lived in peace until the death of Alexander, when the kingdom fell, in the general partition of the empire, to Eumenes. His claims were made good in 322 BC by the regent Perdiccas, who crucified Ariarathes; but in the dissensions which brought about Eumenes’s death, the son of Ariarathes recovered his inheritance and left it to a line of successors, who mostly bore the name of the founder of the dynasty.

Under Ariarathes IV, Cappadocia came into relations with Rome, first as a foe espousing the cause of Antiochus the Great, then as an ally against Perseus of Macedon. The kings henceforward threw in their lot with the Republic as against the Seleucids, to whom they had been from time to time tributary. Ariarathes V marched with the Roman proconsul Publius Licinius Crassus Dives Mucianus against Aristonicus, a claimant to the throne of Pergamon, and their forces were annihilated (130 BC). The imbroglio which followed his death ultimately led to interference by the rising power of Pontus and the intrigues and wars which ended in the failure of the dynasty.

The Cappadocians, supported by Rome against Mithridates VI of Pontus, elected a native lord, Ariobarzanes, to succeed (93 BC); but in the same year Armenian troops under Tigranes the Great (Tigran) entered Cappadocia, dethroned king Ariobarzanes and crowned Gordios as the new client-king of Cappadocia, thus creating a buffer zone against the encroaching Romans.[3] It was not until Rome had deposed the Pontic and Armenian kings that the rule of Ariobarzanes was established (63 BC). In the civil wars Cappadocia was now for Pompey, now for Caesar, now for Antony, now against him. The Ariobarzanes dynasty came to an end and a certain Archelaus reigned in its stead, by favour first of Antony and then of Octavian, and maintained tributary independence until AD 17, when the emperor Tiberius, on Archelaus’ death in disgrace, reduced Cappadocia at last to a Roman province. Much later it was a region of the Byzantine Empire.

Cappadocia contains several underground cities (see Kaymaklı Underground City), largely used by early Christians as hiding places before they became a legitimate religion. The Cappadocian Fathers of the 4th century were integral to much of early Christian philosophy. It also produced, among other people, another Patriarch of Constantinople, John of Cappadocia, who held office 517–520. For most of the Byzantine era it remained relatively undisturbed by the conflicts in the area, first with the Sassanid Empire and later against the Islamic expansion led by Arabs.

Cappadocia shared an always changing relation with the neighbouring Armenia, by that time a region of the Empire. The Arab historian Abu Al Faraj purports the following about Armenian settlers in Sivas, during the 10th century: “Sivas, in Cappadocia, was dominated by the Armenians and their numbers became so many that they became vital members of the imperial armies. These Armenians were used as watch-posts in strong fortresses, taken from the Arabs. They distinguished themselves as experienced infantry soldiers in the imperial army and were constantly fighting with outstanding courage and success by the side of the Romans in other words Byzantine”.[4] As a result of the Byzantine military campaigns, the Armenians spread into Cappadocia and eastward from Cilicia into the mountainous areas of northern Syria and Mesopotamia. This immigration was increased further after the decline of the local imperial power and the establishment of the Crusader States following the 4th Crusade. Cappadocia became part of the Armenian Kingdom of Cilicia, a state formed in the 12th century by Armenian refugees fleeing the Seljuk invasion of Armenia and a close ally of the Crusaders.

Following the Battle of Manzikert in 1071, various Turkish clans under the leadership of the Seljuks began settling in Anatolia. With the rise of Turkish power in Anatolia, Cappadocia slowly became tributary to the Turkish states that were established to the east and to the west, and some of the population converted to Islam. By the end of the early 12th century, Anatolian Seljuks had established their sole dominance over the region. With the decline and the fall of the Konya-based Seljuks in the second half of the 13th century, they were gradually replaced by the Karaman-based Beylik of Karamanoğlu, who themselves were gradually succeeded by the Ottoman Empire over the course of the 15th century. Cappadocia remained part of the Ottoman Empire for the centuries to come, and remains now part of the modern state of Turkey. A fundamental change occurred in between when a new urban center, Nevşehir, was founded in the early 18th century by a grand vizier who was a native of the locality (Nevşehirli Damat İbrahim Pasha), to serve as regional capital, a role the city continues to assume to this day.

In the meantime many former Cappadocians had shifted to a Turkish dialect (written in Greek alphabet, Karamanlıca), and where the Greek language was maintained (Sille, villages near Kayseri, Pharasa town and other nearby villages), it became heavily influenced by the surrounding Turkish. This dialect of Greek is known as Cappadocian Greek. Following the 1923 population exchange between Greece and Turkey, the language is now only spoken by a handful of the former population’s descendants in modern Greece.