UA DE EN ES FR IT NL PL BY PT
the European climate
pt es fr it nl pl by ua de en
sections
  • Two-dimensional anomalies of heat conductivity
  • the Analysis of a superficial thermal stream
  • Explosive tectonics and a thermal field evropy
  • the Thermal stream and an arrangement of ruptures
  • the Thermal stream, capacity of a bark
  • Value of researches of a thermal stream
  • Geothermal data on bolgarii
  • the Thermal stream in velikobritanii
  • geotermija vengrii
  • the Field of a thermal stream in territory gdr
  • Measurements of a thermal stream frg
  • the Preliminary card of a thermal stream gretsii
  • the Thermal stream in danii
  • Konduktivnyj a thermal stream in islandii
  • Temperature a gradient in ispanii
  • the Thermal stream in italii
  • the Preliminary card of a thermal stream gretsii. The south review

    you are: the Preliminary card of a thermal stream gretsii

    Beginning the review from the south, we can see, that in some places of southern area a thermal stream below the normal. It is a little to the north around an active volcanic arch there is only one gauging. Nevertheless, existence of natural thermal displays and thermal measurements in the boreholes drilled for geothermal researches, show a high gradient and, thus, a high thermal stream.

    ) Susaki, near Corinth, - we find hot superficial displays (solfatary and mofety) with temperatures to 41 °s and plentiful newest modern adjournment of salt. In the drilled chinks the maximum temperature 73 °s on depth of 145 m.

    ) Egina - thermal sources with temperature to 26 °s.

    ) Methane - the temperature of sources to 41 °s, fumaroly during the newest time, a volcano with noted eruption, in two drilled chinks on depth of 65 m is received temperature to 32 °s.

    ) Melos - are known fumaroly with temperatures to 102 °s, the hot earths with temperatures to 75 °s and it is a lot of freaticheskih explosive craters. Temperature measurements in 68 boreholes by depth to 80 m and in two deep chinks are spent: in chink MZ-1 depth of 1101 m the temperature in a face is equal 310 °s, in chink МА-1 depth of 1163 m - 308 °s.

    ) Kimolos (group of Melos) - thermal sources with temperature to 59,5 °s; temperature in superficial chinks to 40 °s.

    ) Santorin (the Shooting gallery) - active vulkanizm, fumaroly and some thermal sources with temperatures to 52 °s.

    ) Nisiros - hot sources (to 48,5 °s), fumaroly with temperatures to 100 °s, in superficial boreholes of temperature to 100 °s, it is a lot of freaticheskih explosive craters with noted activity where on rather small depths it is possible to assume temperature of an order 250 °s.

    ) Plaits: hot sources with temperatures to 45,5 °s.

    For the central area of Aegean sea is available three measurements of a thermal stream. Now while it is difficult to explain, why a thermal stream near island Chios much more above average value. Obviously, presence of the numerous volcanic centres more or less young age and numerous hot sources (the maximum temperature to 87 °s on island Lesbos) to the east and the north from a place where measurement is executed, prove the received value.


    sections
  • Two-dimensional anomalies of heat conductivity
  • the Analysis of a superficial thermal stream
  • Explosive tectonics and a thermal field evropy
  • the Thermal stream and an arrangement of ruptures
  • the Thermal stream, capacity of a bark
  • Value of researches of a thermal stream
  • Geothermal data on bolgarii
  • the Thermal stream in velikobritanii
  • geotermija vengrii
  • the Field of a thermal stream in territory gdr
  • Measurements of a thermal stream frg
  • the Preliminary card of a thermal stream gretsii
  • the Thermal stream in danii
  • Konduktivnyj a thermal stream in islandii
  • Temperature a gradient in ispanii
  • the Thermal stream in italii
  • las secciones
  • las anomalías Bidimensionales de la termoconductividad
  • el Análisis del flujo superficial térmico
  • la tectónica Explosiva y el campo térmico evropy
  • el flujo Térmico y la disposición de las rupturas
  • el flujo Térmico, la potencia kory
  • el Significado de las investigaciones del flujo térmico
  • los datos Geotérmicos por bolgarii
  • el flujo Térmico en velikobritanii
  • la Geotermia vengrii
  • Paul del flujo térmico en el territorio gdr
  • las Medidas del flujo térmico frg
  • la tarjeta Preliminar del flujo térmico gretsii
  • el flujo Térmico en danii
  • Konduktivnyj el flujo térmico en islandii
  • De temperatura el gradiente en ispanii
  • el flujo Térmico en italii
  • les paragraphes
  • dvumernye les anomalies de la conductibilité de la chaleur
  • l'Analyse du flux de chaleur superficiel
  • la tectonique Explosive et le champ thermique evropy
  • le Flux de chaleur et la disposition des ruptures
  • le Flux de chaleur, la capacité de l'écorce
  • la Signification des études du flux de chaleur
  • les données Géothermiques selon bolgarii
  • le Flux de chaleur à velikobritanii
  • la Géothermie vengrii
  • Paul du flux de chaleur sur le territoire gdr
  • les Mesures du flux de chaleur frg
  • la carte Préalable du flux de chaleur gretsii
  • le Flux de chaleur à danii
  • Konduktivnyj le flux de chaleur à islandii
  • De température le gradient à ispanii
  • le Flux de chaleur à italii