the Thermal stream in danii. Negative correlation

you are: the Thermal stream in danii

Negative correlation between a superficial thermal stream and age of a bark, or age of last tektono-thermal event, is applicable and to region discussed here at its comparison with the next board. CHermak and Hurtig notice, that in some areas of Europe higher thermal stream can have negative correlation with capacity of a bark. It is fair and for the Danish region.

As in Denmark surfaces rather powerful series (about 50-100 impenetrable tertiary breeds, here on small depths we can, possibly to make measurement of a thermal stream which will not be broken by water movement are found out near. Such detailed measurements will be spent in the near future. Their results can promote the best understanding of what influence of the temperature variations caused by changes of a climate. For such influence there are while only tentative estimations.