The origin of the Oleshkivski Sands significantly influenced the unique landscapes of the place. There is an interesting presumption that the desert was created in the result of the fact that the huge array of continental ice was moving through the ancient valley of the Dnipro river during the ice age. The glacier occasionally came from the north along the Dnipro riverbed and brought hundreds of kilometers of soil mass with it that remained after the ice thawed. This soil formed a natural dam that separated the lakes near the glacier from the lower part of the river bed. When glaciers melted, the water level in these lakes gradually climbed and the dam could not hold against the water pressure and broke down. The huge flow of water moving down from Dnipro to the Black Sea washed away everything on its way. Around the place where Nova Kakhovka is located, the current decreased and trillion tons of sand washed from the banks of the Dnipro, settled to the bottom and created a massive sand area.
Despite the fact that there has always been sand in the valleys of the Dnipro, the human activity strongly contributed to the spread of sands. Especially the active sheep farming conducted here in 18-19 centuries.
Cattle began to destroy the vegetation, thus increasing the size of sand dunes. As well as wind erosion, that has contributed highly to the expanding of the sand area.
Since the late 18th century actions were taken to control the spread of the sand area. Oleshkivski Forestry was created to support such actions. However, in the second half of the 19th century, after the land was given to farmers, forests were severely damaged by irrational use, which led to an increase in the sand dunes. To stop this process, active planting of pine forests, orchards and vineyards began. Therefore, it is correct to define Oleshkivski sands as a semi-desert. Desert is conventionally divided into seven arenas, each with different natural and climatic features.
Like all deserts, it consists of numerous bahrans, about 5 meters high (separate are up to 20 meters high), which move due to the wind. In summer the temperature of the sand reaches 75 ° C, the rains are rare, and sandstorms occur from time to time. Deep under the sand layer, fresh water can be found, but its use is strongly limited, as it is necessary for the desert growth containment. You can find a number of opportunities for active tourism at the Oleshkivski sands: hiking, biking, horseback riding, auto, motorcycle tours and trophy on the sand.
Природні ландшафти, які тут співіснують пліч-о-пліч, дуже різноманітні: піщаний степ з барханами, луки, гаї, болота і озера. Фауна і флора Олешківських пісків також унікальна - деякі рослини і тварин ви не зустрінете більше ніде в світі.