Філоненко, Ю. М.Ю. М.ФілоненкоБездухов, О. А.О. А.Бездухов2026-01-072026-01-072017Філоненко Ю. М., Бездухов О. А. Особливості мікрорельєфу боліт і заболочених ділянок Чернігівщини. Фізична географія та геоморфологія. 2017. Вип. 4 (88). С. 50-54.УДК 551.4(477)https://ir.library.knu.ua/handle/15071834/9494Проаналізовано особливості виникнення та розміщення окремих елементів мікрорельєфу поверхні боліт і заболочених ділянок на території Чернігівської області. Зокрема, досліджено такі форми рельєфу, як купини, міжкупинні зниження, пасма, мочари та горбки. Охарактеризовано їх генезис, морфологічні і морфометричні особливості, а також щільність розташування у межах боліт і заболочених ділянок на дослідженій території.Regardless of significant human impact as a result of conducted large-scale works on land development in 1960-1970, swamp complexes of Chernihiv region mainly saved the initial character of their surface. Hummocks and hollows (low-lying areas between hummocks) are the most widespread and numerous microrelief forms of swamps and wetlands of Chernihiv region. Their origin is connected with uneven vegetation cover density and peculiarities of peat accumulation. The investigated hummocks and the majority of hollows on the chosen key areas are the result of phytogenic accumulation and only a small part of them was formed due to the influence of denudation processes (mainly because of erosion and sometimes due to the impact of big ungulates). The majority of hummocks has the same internal structure. The top layer with the thickness of 3-5 (in some cases 7-8) cm is made up by fresh turf. Below the top layer, there is a layer, which is the first stage of peat formation. The location of hummocks in swamps and wetlands is almost always chaotic. The investigated hummocks had the average height of 15-20 cm, while their diameter was approximately 25-30 cm. Hummocks with bigger height are much less frequent. In some areas in the north of Chernihiv region (Ripky, Koriukivka, Snovsk and some other raions) there are also bottom-hole-strand and strand-bottom-hole-small-lake complexes having the area of several tens (sometimes hundreds) of m². The key role in formation of these relief forms belongs to biogenic processes, which are closely related to other factors of swamp microrelief formation (hydrological, thermal, mechanical, gravitational, fluvial and so on). Except for hummocks, hollows, ridges and bottom holes of wetlands occurring in swamps there are also some small humps, which are formed mainly by tree trunks raisings. It should be mentioned that the surface of swamps and wetlands and some of their microrelief forms are subjected to considerable changes due to the impact of fires.ukкупинаболотопоширеннянаноулоговинамікропасмомочаринагорбокформи рельєфущільністьплощаhummockswampspreadnano-hollowmicroridgebottom hole of wetlandhumprelief formsdensityareaСтаття