In order to explain you the way the Petrified Forest in Lesvos was created thousands years ago, it is important to talk first about volcanoes. 

Eyrudice and Georgia from Greece created a presentation about volcanoes: 

VOLCANOES_georgia euridiki.pptx

Manolis, Stratos and Eyripides created the presentation :

VOLCANOES AND EARTHQUAKES.pptx

Stratoula and Anna-Maria created the presentation : 

What is a Volcano_Stratoula_Anna_Maria.ppt

You can add informations to the collaborative presentation using the following link:  What is a volcano? 

Kula Divlit Volcanic Park

Kula Divlit Volcanic Park is located in the eastern part of Kula-Salihli Geopark, northeast of Kula town center. Kula divlit volcanic park contains all the characteristic landforms formed due to advanced volcanic activities in the 3rd phase of Kula volcanism. It is possible to observe Kula divlit slag cone and lava flow, parasitic cones, spatter cones, lava tunnels and ditches in the park area. There are 1 walking path (approximately 2.7 km in length) and wooden bridges and 1 bicycle track (approximately 34.8 km in length) that allow geosites to be visited. Volcanism in Kula Region can be summarized as follows; Kula region is one of Turkey's youngest volcanic area. Volcanism, which started in the Late Pliocene approximately 2 million years ago, continued until the historical periods and took place in three phases.Kula region is one of Turkey's youngest volcanic area. Volcanism, which started in the Late Pliocene approximately 2 million years ago, continued until the historical periods and took place in three phases.

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