About terraces on the shore of the Teriberskaya Bay of the Barents Sea (the Kola Peninsula)

• Published in: Vestnik MGTU
• Main Authors: Neradovsky Yu. N., Miroshnikova Ya. A., Companchenko A. A., Chernyavsky A. V.
• Format: Article in Journal/Newspaper
• Language: Russian
• Published: Murmansk State Technical University 2022
• Subjects: terraces; arctic coast of the barents sea; kola peninsula; teriberka; transformation of the shores; террасы; арктическое побережье баренцева моря; кольский полуостров; териберка; трансформация берегов; General Works; A; Arctic; Barents Sea; Kola Peninsula; Teriberskaya
• Online Access: https://doi.org/10.21443/1560-9278-2022-25-1-38-49; https://doaj.org/article/4b72f0c2f0064b24a83c46790c3a2ad7

The paper considers the results of the study of modern terraces on the coast of the Lodeyny Peninsula in the Barents Sea. According to field observations, decoding of space and geodetic maps and volumetric modeling, signs of three terraces have been identified. Two terraces having a rear seam, a cliff, a brow and horizontal platforms have been studied in more detail. The rear seams are located at 7 and 30 m, and the edges at 10 and 40 m above the sea level. The third terrace is confined to the level of 40–60 m, and has not been studied in detail. According to estimates, the first two terraces were formed about 3,300 and 6,000 years ago respectively. The 1st terrace characterizes the period of slow land rise by 10 m, at the speed up to 3 mm/year, which began about 3,300 years ago and continues to the present. It is characterized by a uniform sea retreat of about 15 mm/year. The erosion products of this terrace are common in the lateral zone and represent modern marine sediments, including beaches forming a new terrace. The 2nd terrace characterizes to the dynamics of rapid land rise by 30 m at a speed of about 11 mm/year, which occurred in the period from 6,000 to 3,300 years ago. The erosion products of this terrace are most common on the coast and are found at a distance of 100 m to 2–3 km from the shore. It is assumed that the speed of movement of the coastline during the retreat of the sea was different and reached up to 900 mm/year. According to the authors, preliminary data indicate the instability of the territory and the manifestation of block movements, which may have a negative impact on the development of infrastructure.