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From this result, the solidification front of melt can be decided.
The crystallization kinetics of the metastable melt can be determined by means of differential scanning calorimetry.
Even this massive area of surface melt can be seen as a one-off summer event recurring twice every three centuries.
The melt can be modelled in the system jadeite calcite CO2 and will, on emplacement, form mineral assemblages characteristic of a wide range of alkalic rocks.
By changing this parameter opposite surface temperature gradients in the melt can be obtained, which define opposite thermocapillary stresses.
The νe within the melt can be changed when crystals with different lamellar thickness l are melted.
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This melting can be a problem, particularly if the melting ice starts its life on land.
The magnitude of glacier melting can be seen at the Rongbuk glacier on the northern slope of Mount Everest.
The pronounced reorientation of cross-linked epoxy resin melts can be ascribed to the inter-bonded chains.
This difference in melting can be accounted for by modulating the ablation factor according to debris properties.
Consequently, strain-softening of diblock copolymer melts can be tuned by the weight/volume ratio of the two blocks.
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