Abstract
A detailed description and engineering-geological characterization are made for the loess-soil series rocks of Zdolbuniv key profile, which represents the main loess, palaeo-soil, and palaeo-cryogenic horizons of the Middle and Upper Pleistocene within the Volyn’ Upland – a classical region of the European loess development. The analysis of the differentiation in the composition and properties of the loess, palaeo-soil, and palaeo-cryogenic horizons imply on their significant difference caused by palaeogeographical conditions of their development and of the dia-genetic metamorphism. Key words: loess, loess-soil series, key profile, fossil soil, palaeo-cryogenesis, engineering-geological properties.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
