(160 m.) "Wolf's-Throat" (Vovche horlo), with three great rocks; the small Javlena Sabora, three dangerous "Robber Rocks" (Kameni Rosbiyniki), and two granite precipices, Stovli (Pillars), and we come into the Zaporog country (Zaporoze).
Here the Dnieper valley widens and numerous islands appear in the stream. The upper ones, for example, Khortizia and Tomakivka, which were once the site of the first Zaporog Sich, are high, rocky, and overgrown with forest. Further south the steep left-hand valley slope recedes far from the river and the so-called Veliki Luh begins. It is a labyrinth of flat forest and reed-covered alluvial islands, river branches, old river beds, lakes and swamps. Here were located the hunting and fishing grounds of the Zaporog Cossacks; here was their dwelling place, wonderfully fortified by nature and surrounded by an inaccessible wilderness of forests and waters, and the center of their military state; of the century-old oaks of the Veliki Luh, the Zaporogs built their ships, in order to pay their daring visits to the lord of Islam in his own capital. But the glorious days are past, the warlike life and activity has disappeared, and strange colonists, whom the Russian Government has sent here to settle, now occupy the ground on which the second Ukrainian state originated.
From the many-branched mouth of the Konka (also named Kinska voda) the Dnieper River turns toward the southwest, which direction it retains until it disembogues into the sea. From this point on, the river nowhere flows in a single bed; an enormous number of side arms branch off from the main arm or unite with it. The broad river valley, whose right bank continues to be high and rocky for a time, is taken up by the plavni formation and winds like a broad band of freshly growing verdure thru the steppe, which stretches out dry and golden-brown in the hot midsummer. After receiving, as its last tributary, the stepperiver Inhuletz, it empties with nine arms into its liman, below Kherson. Of these arms only two are navigable for larger vessels, and the immense Dnieper liman is at most only 6 meters deep. The river brings down great masses of sand and mud, and fills up its liman so rapidly that strenuous dredging is necessary, in order to make it possible for small sea-vessels to reach the harbor of Kherson.
The Dnieper River brings the Black Sea, on the average, 2000 cu. m. of water per second. It is navigable, even for large river boats, along a stretch of 1900 km." The ice-cover lasts 100 days at Kiev; 80 days in the lower part of its course.
The tributaries of the Dnieper are very numerous and important; their total length is over 13,000 km. Of those on the right, the Pripet River is the most important. It gathers in all the waters of the Polissye and is the typical river of that district. Its length exceeds 650 km. Rising in the northern spurs of the Volhynian Plateau, very close to the course of the Buh, it immediately reaches the Polissian Plain and becomes a navigable river over 50 m. wide and about 6 m. deep. In the main axis of the Polissian basin the Pripet turns eastward and becomes about 100 m. wide. The incline of the river is very slight, the number of turns and river arms enormous. Between swampy woods and moors the river forms labyrinths of delicate, intricate waterways and stagnant pools. Near Mosir, where the river turns to the southeast, its width reaches 450 m., its depth 10 m. Of quite the same type are the tributaries of the Pripet: the Turia, Stokhod, Stir with the Ikva, the Horin with the Sluch, the Ubort and the Uz on the right; the Pina Yasiolda, Sluch and Ptich on the left. All of them are navigable along great stretches. The remaining right-hand tributaries of the Dnieper, the Teterev and the Irpen, have the Polissian character only near their mouth, otherwise they are purely plateau rivers with rocky beds. The Teterev is able to transport rafts of logs, while the other rivers of the Dnieper Plateau, as for example, the Ross (altho greater than the Teterev) and the Tiasmin, are entirely unfit for navigation, as a result of their rocky beds and their small volume in summer. The last large Dnieper tributary, the steppe-river Inhulez, altho barely 100 km. shorter than the Pripet, is, for the same reasons, only capable of carrying logs in the last 150 km. of its much-twisted course.