Introducing Trabzon Province 14

One of the geomorphological elements of the province of Trabzon in the mass movements. These are based on the size of landslides, earth flows and soliflüksiyondur. Trabzon province is extremely important in shaping the basic reason for the formation of mass movements of soil structure. The lavas and tuffs are the dominant materials are slit and their bodies because of the cracks are more or less water conduction. Although still common in the tuffs contain pores large extent. Receive more precipitation in the region is quite hot and humid fact, decomposite cause rocks to the depths, while the overall slope, slopes of 25 ° - 30 ° on the fact that the total rainfall in the months and year-end values ​​in the specific amounts to reach close to the mass movements are encouraged. To date, the most important of landslides that have occurred; Çaykara-Grand Mosque (1929, 146 dead), Greenhouse (1949), Macka-Catak (1988, 63 dead), Sındıran (1990) and King and Poplar Landslide.

Macka Macka's in the northwest of the village as an example akmalarında Ormanüstü soil slopes of the foothills overlooking the creek and south of the pitches can be a little more.

The valley slopes are very steep and the slope Soliflüksiyonu and hamlets with the plateau.

FLORA

The vertical dimension of the field variable in all seasons in temperate and rainy climate, the vegetation of different species, gave rise to generations of vegetation of different species. Accordingly, 0-300 m. yükseltilerinden psöudomaki infiltrate into the Mediterranean plant species (persimmon, maple, boxwood, cherry laurel, laurel, prekanta, medlar, juniper tar, strawberry ... etc.) showing distribution of elements, circles close to the shore from the broad-leaved forests located in the skirt (alder, chestnut, oak species , ash, linden, common hazel, white willow, poplar, east, such as Plane Tree ...), on the floor leaves a large wide-dominated mixed coniferous forests (European chestnut, common alder, hornbeam, common hazel, eastern horn, oak, maple , rowan, ÇİTLENBİK, laurel, purple flowered rhododendron, beech, spruce and fir) and also above the forests dominated by conifers (pine, spruce, rhododendron, and some of the purple flowering shrub species) shows that distribution.