Slopes are an important element of a river valley. They determine the specific character of the valley and the attractiveness of its landscape, and influence the type of its development. The Warta valley slopes in the vicinity of Uniejów are asymmetric, with the eastern slope high and steep, at places cut with dry valleys. The article describes a section of the slope 13 km long, its origin and geological structure. It also explains its impact on the micro-climate (including the strength and direction of the wind
Development trends of the modern city imply a reduction in the number of inhabitants in its centre, ...
Valley development through erosional processes typically tends to create symmetrical valleys. Over ...
On upland Triassic sandstone slopes of the western Blue Mountains, nonswamp, sclerophyllous heath (s...
Slopes are an important element of a river valley. They determine the specific character of the vall...
The author describes the relief and geological structure of the Warta valley in its river gap across...
The conditions existing in the Uniejów Basin were favourable to formation of outflow after successiv...
This article is an attempt at presenting environmental changes within the Warta valley during the l...
© Published under licence by IOP Publishing Ltd. The article examines the spatial distributions of a...
Creation or agricultural terraces is one of the main method of anti-erosional protection in the moun...
The nature of the inter-relationship of valley-side slopes and the streams at their base is regarded...
Cultural landscape is a historically formed part of geographical space which emerged as a result of ...
Long distance slope transport has been relatively rarely observed in the Polish lowlands. This study...
Cultural landscape is a historically formed part of geographical space which emerged as a result of ...
This article describes the formation and development of the 1st-order valley network in the postglac...
This Poster is primarily intended as supplementary material to the article (Małka et al., 2022). Thi...
Development trends of the modern city imply a reduction in the number of inhabitants in its centre, ...
Valley development through erosional processes typically tends to create symmetrical valleys. Over ...
On upland Triassic sandstone slopes of the western Blue Mountains, nonswamp, sclerophyllous heath (s...
Slopes are an important element of a river valley. They determine the specific character of the vall...
The author describes the relief and geological structure of the Warta valley in its river gap across...
The conditions existing in the Uniejów Basin were favourable to formation of outflow after successiv...
This article is an attempt at presenting environmental changes within the Warta valley during the l...
© Published under licence by IOP Publishing Ltd. The article examines the spatial distributions of a...
Creation or agricultural terraces is one of the main method of anti-erosional protection in the moun...
The nature of the inter-relationship of valley-side slopes and the streams at their base is regarded...
Cultural landscape is a historically formed part of geographical space which emerged as a result of ...
Long distance slope transport has been relatively rarely observed in the Polish lowlands. This study...
Cultural landscape is a historically formed part of geographical space which emerged as a result of ...
This article describes the formation and development of the 1st-order valley network in the postglac...
This Poster is primarily intended as supplementary material to the article (Małka et al., 2022). Thi...
Development trends of the modern city imply a reduction in the number of inhabitants in its centre, ...
Valley development through erosional processes typically tends to create symmetrical valleys. Over ...
On upland Triassic sandstone slopes of the western Blue Mountains, nonswamp, sclerophyllous heath (s...