RAVINES AND LANDSLIDES OF THE UFA “PENINSULAR”

V. I. Baryshnikov; V. G. Kamalov

doi:10.15356/0435-4281-2016-1-30-36

RAVINES AND LANDSLIDES OF THE UFA “PENINSULAR”

V. I. Baryshnikov, V. G. Kamalov

https://doi.org/10.15356/0435-4281-2016-1-30-36

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Abstract

The Ufa “Peninsular” since active development is experiencing a shortage of land resources due to intensive dissection of Perm massive, on which the city is situated due to constant expansion of the latter. Structuralgeomorphological analysis, using remote sensing materials, field investigations, and drilling data have shown that Permian gypsum, limestone and sandy-clay rocks composing the territory, are divided by vertical and horizontal crustal deformations into blocks of different sizes. As a result, the rock mass was deconsolidated, which caused the
intensifi cation of the formation of ravines and landslides.

Keywords

овраг, оползень, карст, космоснимок, тектоника

About the Authors

V. I. Baryshnikov

Bashkir State University, Ufa
Russian Federation

V. G. Kamalov

ООО “Архстройизыскания”, Уфа
Russian Federation

References

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Review

For citations:

Baryshnikov V.I., Kamalov V.G. RAVINES AND LANDSLIDES OF THE UFA “PENINSULAR”. Geomorfologiya. 2016;(1):30-36. (In Russ.) https://doi.org/10.15356/0435-4281-2016-1-30-36