the Preliminary card of a thermal stream gretsii. Northern part egejskogo the seas

you are: the Preliminary card of a thermal stream gretsii

In northern part of Aegean sea there are some sites with the raised values, in other places the thermal stream is close to average value. We have united aforementioned values of a thermal stream and have allocated positive anomaly which precisely coincides with area along a break corresponding to the North Egejsky trench.

Further to the north, in continental Greece, two areas with values of a thermal stream above an average have been found out. The first settles down in the central Macedonia where two measurements have shown the raised values. In this area numerous thermal sources, intensive tectonic activity, a mineralization, and also vulkanizm which age was defined as late pliotsen - plejstotsen are shown. Other area settles down to the north from Kavaly where there are considerable thermal displays. This positive anomaly will be co-ordinated with similar anomaly in Bulgaria.

At last, one more area with a superfluous thermal stream has been established between a northeast part of the central Greece and southern edge of the Fessalijsky hollow where dumps along which numerous thermal sources settle down, as is known, are widely developed. As an example it is possible to mention thermal sources of Thermopylae which are most known, and sources Edipsos in the island Euboea northwest where the heat makes 78 °s. In this area there is a number of insignificant displays young vulkanizma (late pliotsen - plejstotsen).

In the western Greece the thermal stream much more low or comes nearer to average value.