Not really because the Dead Sea valley is really small.
Had to find a full page without politic or tourist info.
Here some 'copy-paste'
It is even more difficult to find pictures other than people floating in the water. But, i will find some and post links
The Dead Sea is the final link of the chain of rivers and lakes that lies in the valley of the Jordan. Taking its rise on the southern slopes of Mt. Hermon, the Jordan in its southern course first spreads out into Lake Merom, emerging from which it flows into the Lake of Tiberias, whence it descends into the Dead Sea. To convey a proper idea of the size and shape of the Dead Sea travellers often compare it to the Lake of Geneva. The resemblance between the two is striking in almost every particular. The great lake of the Holy Land is forty-seven miles long and about ten miles across at its widest part. Its area is approximately 360 square miles. The surface of the water is 1292 feet below the level of the Mediterranean, which is only a few miles to the west. This extraordinary feature alone singles out the Dead Sea from all other bodies of water. A low-lying peninsula about ten miles wide, called el-Lisan, "the tongue", which runs out from the south-eastern shore to within three miles of the opposite shore, divides the sea into two unequal parts. The northern and larger part is very deep, reaching at one point a depth of 1310 feet. The southern bay is, on the contrary, very shallow, averaging hardly a depth of thirteen feet. In two places it is possible to cross from the peninsula to the opposite shore by means of two fords
The water in the Dead Sea is salt. Every day the Jordan and other affluents pour into it over six and one half million tons of fresh water. There is, however, no outlet to the ocean, and the sole agent whereby this increase is disposed of is evaporation. The power of the sun's rays in this great pit is, however, so intense that save for a small fluctuation between the wet and dry seasons, the level of the sea does not change, despite the great volume that is added to it. In the water that remains after evaporation solid matters make up 26 per cent of the whole; 7 per cent being chloride of sodium (common salt), the rest being chiefly chlorides of magnesium, calcium, and derivatives of bromium. The chloride of magnesium gives the water a very loathsome taste; the chloride of calcium an oily appearance. The specific gravity of the water is 1.166. The presence of so much salt explains well the weird name of the sea, since save for a few microbes, no organic life can exist in it. Even fish from the ocean perish when put into it. The human body will not sink below the surface. Bathing, however, in the Dead Sea can hardly be styled a pleasure, as the water is very irritating to the skin and eyes. There is, it need hardly be said, no foundation for the statement sometimes made, that birds cannot fly across the water, as occasionally sea-birds can be seen resting on its surface. From time to time large quantities of bitumen rise to the surface from the bottom. Bitumen is also found along the shores and is referred to in Genesis (xiv, 10) where it speaks of the puteos multos bituminis — "many pits of slime". This feature caused the ancients to speak of the sea as the "Lake of Asphalt
The Dead Sea has an area of 1,050 km˛, with a length of 76 km, and a maximum width of 16 km. Maximum depth is 396 metres. The Dead Sea is geologically part of the Rift Valley system.
The surface of the Dead Sea, 408 m (1,340 ft) below sea level as of 1996, is the lowest water surface on earth. The lake is 80 km (50 mi) long and has a maximum width of 18 km (11 mi); its area is 1,020 sq km (394 sq mi). The Dead Sea occupies a north portion of the Great Rift Valley. On the east the high plateau of Moab rises about 1,340 m (about 4,400 ft) above the sea; on the west the plateau of Judea rises to half that height. From the eastern shore a peninsula juts out into the lake. To the south of this peninsula the lake is shallow, less than 6 m (less than 20 ft) deep; in the north it reaches its greatest depth of 399 m (about 1,309 ft) below surface level, and 799 m (about 2,621 ft) below sea level.