Salt Sea in Smiths Bible Dictionary

the usual and perhaps the most ancient name for the remarkable lake which to the western world is now generally known as the Dead Sea. I. Names.-- (1) The Salt Sea, Ge 14:3 (2) Sea of the Arabah (Authorized Version "sea of the plain," which is found in De 4:49 ); (3) The East Sea Joe 2:20 (4) The sea, Eze 47:8 (5) Sodomitish Sea, 2 Esdras; (6) Sea of Salt and Sea of Sodom, in the Talmud; (7) The Asphaltic Lake, in Josephus; (8) The name "Dead Sea" appears to have been first used in Greek by Pausanias and Galen, and in Latin (mare mortuum) by Justin xxxvi. 3,6, or rather by the older historian Trogus Pompeius (cir. B.C. 10), whose work he epitomized. (9) The Arabic name is Bahr Lut, the "Sea of Lot." II Description. --The so-called Dead Sea is the final receptacle of the river Jordan, the lowest and largest of the three lakes which interrupt the rush of its downward course. It is the deepest portion of that very deep natural fissure which runs like a furrow from the Gulf of Akabah to the range of Lebanon, and from the range of Lebanon to the extreme north of Syria. Viewed on the map, the lake is of an oblong form, of tolerably regular contour, interrupted only by a large and long peninsula which projects from the eastern shore near its southern end, and virtually divides the expanse of the water into two portions, connected by a long, narrow and somewhat devious passage. Its surface is from north to south as nearly as possible 40 geographical or 46 English miles long. Its greatest width is about 9 geographical or 10 1/2 English miles. Its area is about 250 geographical square miles. At its northern end the lake receives the stream of the Jordan; on its eastern side the Zurka Ma'in (the ancient Callirrhoe, and possibly the more ancient en-Eglaim), the Mojib (the Arnon of the Bible), and the Beni-Hemad; on the south the Kurahy or el-Ahsy; and on the west that of Ain Jidy. The depression of its surface, and the depth which it attains below that surface, combined with the absence of any outlet, render it one of the most remarkable spots on the globe. The surface of the lake in May, 1848, was 1316.7 feet below the level of the Mediterranean at Jaffa. Its depth, at about one third of its length from the north end, is 1308 feet. The water of the lake is not less remarkable than its other features. Its most obvious peculiarity is its great weight. Its specific gravity has been found to be as much as 12.28; that is to say, a gallon of it would weigh over 12 1/4 lbs., instead of 10 lbs., the weight of distilled water. Water so heavy must not only be extremely buoyant, but must possess great inertia. Its buoyancy is a common theme of remark by the travellers who have been upon it or in it. Dr. Robinson "could never swim before, either in fresh or salt water," yet here he "could sit, stand, lie or swim without difficulty." (B.R.i.506.) The remarkable weight of the water is due to the very large quantity of mineral salts which it holds in solution. Each gallon of the water, weighing 12 1/4 lbs., contains nearly 3 1/3 lbs. of matter in solution --an immense quantity when we recollect that seawater, weighing 10 1/4 lbs. per gallon, contains less than 1/2 a lb. Of this 3 1/2 lbs. nearly 1 lb. is common salt (chloride of sodium), about 2 lbs. chloride of magnesium, and less than 3 a lb. chloride of calcium (or muriate of lime). The most usual ingredient is bromide of magnesium, which exists in truly extraordinary quantity. It has been long supposed that no life whatever existed in the lake; but recent facts show that some inferior organizations do find a home even in these salt and acrid waters. The statements of ancient travellers and geographers to the effect that no living creature...