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The article presents some results of working out the methodology for monitoring the state of frozen rocks, which are conducted as part of observations at the Zvenigorod biological station. One of the methods of presenting experimental data on the dynamics of the temperature regime and the thickness of the active layer over a 3-year period of field observations is also considered. The presented data can serve to verify the predictive numerical simulation of these processes at the Zvenigorod Biological Station of Lomonosov Moscow State University. This makes it possible to use this methodology for assessing the thermal state of frozen grounds and the stability of foundations and buildings and linear constructions located on them in the conditions of the North and mountainous territories. Therefore, the presented methodology can serve as a good help for monitoring and preventing the destruction of the observed structures in the conditions of climate warming.