Konduktivnyj a thermal stream in islandii. Data on southwest islandii

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Data across southwest, southern and east Iceland will well enough be co-ordinated with theoretical curves. On the other hand, gradients for northwest Iceland it is considerable above the settlement. The considerable maximum of a gradient is allocated in northern part of peninsula Snaj-fedlsnes and in a gulf the Brejdi-fjord. In the western part of northern Iceland other high values of gradients are noticed also, that also is shown on the diagramme. The explanation for these high values in northwest Iceland is necessary, possibly to search in existence of the certain died off axis of growth which settled down, apparently, along the Brejdi-fjord maximum. Such assumption proves to be true and sinklinalnoj structure of a tertiary basalt complex on either side of from this maximum. Not clearly, however, as this died off axis to the northeast from the Brejdi-fjord proceeds.