Soil cover of a bog array on the western slope of the Northern Basseg

The soils of the marsh massif on the slope of the Northern Basseg mountain are studied. It is established that from the center of the marsh massif to the periphery of the thickness of the peat decreases. In connection with this, a number of subtypes of soils have been diagnosed in the transect of the "center-margin": peat oligotrophic gley silty-peat - gleyzem coarse-humus - humus-gley coarse-humus ferruginous.