The
main landforms of the province of Trabzon, south, east-west direction
along the watershed areas of the mountains, in the bosom of their main
stream, gradually descending towards the north and the hilly areas
introduced in the field with important external factor is that the
current şekillenlenmeyi Solakli, Yomra, Degirmendere, Greenhouse,
Kalenima, formed by river valleys and deltas, such as Folder.
Geological
formation, Upper Cretaceous stratigraphy from bottom to top in terms of
fat, added intermediate volcanic sedimentary series, the conglomerate,
fabric, marl, upper Miocene marine clay and lime stone and the series,
gravelly, sandy, silty and clayey, sandy gravel with quaternary fatty
terrace fills, silty, clayey, clayey river and coastal sediment shaped.
The valleys and hills, Rivers and Lakes
Valleys
formed by rivers, especially the arms and the second-order streams,
where the side sections very dardırlar involved in them. This feature is
dominated by the majority of the site. Character of the area's humid
climate, watersheds, and more freight transport is a fast-flowing,
deep-abrasive played a major role. Which is vulnerable to wear tuff,
agglomerate and limestone buildings, on the one hand konsekant vertical
erosion accelerated in the arms perpendicular to develop "V"-shaped
valleys formed, on the other hand, this also occurred on the slopes of
the valleys and slopes of the secondary arms thoroughly slaugh increased
their discharge activity. So today, in the field of vaccine dantritik
drainage system consists of the valley descending towards the sea, sat a
uniform. Even though you have moved into a small area of erosion
debris near the base of valley slopes, the accumulation of low-,
low-sloping plains formed part. At the same time suitable for carrying
any of these areas.
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