by the officers of the Palestine Exploration Fund. A good deal of
work has been done by individual travellers, but the material for
a full description of its physical character is as yet lacking. Two
great rivers, the Yarmuk (Hieromax) and the Zerka (Jabbok),
divide Eastern Palestine into three sections, namely Hauran
(Bashan, q.v.) with the Jaulan west of it; Jebel Ajlun (Gilead,
q.v.); and the Belk’a (the southern portion of Gilead and the ancient
territory of the tribe of Reuben). The latter extends southward
to the Mojib, which, as we have already seen, is the southern
boundary of Eastern Palestine.
It is a matter of dispute whether Hauran should be included within Palestine proper, accepting its definition as the “ancient Hebrew territory.” It is a large volcanic region, entirely covered with lava and other igneous rocks. Two remarkable rows of these run in lines from north to south, through the region of the Jaulan parallel to the Ghor, and from a long distance are conspicuous features in the landscape. The soil is fertile, and there are many remains of ancient wealth and civilization scattered over its surface. South of the Yarmuk the formation is Cretaceous, Hauran basalt being found only in the eastern portion. That region is much more mountainous than Hauran. South of the Zerka the country culminates in Jebel ‛Osha, a peak of Jebel Jil‛ad (“the mountain of Gilead”), 3596 ft. high. From this point southward the country assumes the appearance which is familiar to those who have visited Jerusalem an elevated plateau, bounded on the west by the precipitous cliffs known as the mountains of Moab, with but a few peaks, such as Jebel Shihan (2781 ft.) and Jebel Neba (Nebo, 2643 ft.), conspicuous above the level of the ridge by reason of superior height.
Geology.—The oldest rocks consist of gneiss and schist, penetrated by dikes and bosses of granite, syenite, porphyry and other intrusive rocks. All of these are pre-Carboniferous in age and most of them probably belong to the Archean period. They are generally concealed by later deposits, but are exposed to view along the eastern margin of the Wadi Araba, at the foot of the plateau of Edom. Similar rocks occur also at one or two places in the desert of et-Tih, while towards the south they attain a greater extension, forming nearly the whole of Sinai and of the hills on the east side of the Gulf of Akaba. These ancient rocks, which form the foundation of the country, are overlaid unconformably by a series of conglomerates and sandstones, generally unfossiliferous and often red or purple in colour, very similar in character to the Nubian sandstone of Upper Egypt. In the midst of this series there is an inconstant band of fossiliferous limestone, which has been found in the Wadi Nasb and at other places on the southern border of et-Tih, and also along the western escarpment of the Edom plateau. The fossils include Syringopora, Zaphrentis, Productus, Spirifer, &c., and belong to the Carboniferous. The sandstone which lies below the limestone is also, no doubt, of Carboniferous age; but the sandstone above is conformably overlaid by Upper Cretaceous beds and is generally referred to the Lower Cretaceous. No unconformity, however, has yet been detected anywhere in the sandstone series, and in the absence of fossils the upper sandstone may represent any period from the Carboniferous to the Cretaceous. The Upper Cretaceous is represented by limestones with bands of chert, and contains Ammonites, Baculites, Hippurites and other fossils. It covers by far the greater part of Palestine, capping the table-lands of Moab and Edom, and forming most of the high land between the Jordan and the Mediterranean. It is overlaid towards the west by similar limestones, which contain nummulites and belong to the Eocene period; and these are followed near the coast by the calcareous sandstone of Philistia, which is referred by Hull to the Upper Eocene. Lava flows of basic character, belonging to the Tertiary period, cover extensive areas in Jaulan and Hauran; and smaller patches occur in the land of Moab and also west of the Jordan, especially near the Sea of Gennesareth. Of Recent deposits the most interesting are the raised beaches near the coast and the terraces of the Jordan-Araba depression. The latter indicate that at one period nearly the whole of this depression was filled with water up to a level somewhat above that of the Mediterranean.
The geological structure of the country is very simple in its broad features, but of exceptional interest. In general the stratified deposits lie nearly flat and in regular conformable succession, the lowest resting upon the floor of ancient crystalline rocks. There is, however, a slight dip towards the west, so that the newest deposits lie near the coast. Moreover, along the eastern side of the Jordan-Araba valley there is a great fault, and on the eastern side of this fault the whole series of rocks stands at a much higher level than on the west. Consequently, west of the Jordan almost the whole country is formed of the newer beds (Upper Cretaceous and later), while east of the Jordan the older rocks, sometimes down to the Archean floor, are exposed at the foot of the plateau. The western margin of the valley is possibly defined by another fault which has not yet been detected; but in any case it is clear that the great depression owes its extraordinary depth to faulting. A line of depressions of similar character has been traced by E. Suess as far south as Lake Nyasa.[1]
Climate.—Palestine belongs to the sub-tropical zone: at the summer solstice the sun is ten degrees south of the zenith. The length of the day ranges from ten to fourteen hours. The great variety of altitude and of surface characteristics gives rise to a considerable number of local climatic peculiarities. On the maritime-plain the mean annual temperature is 70° F., the normal extremes being about 50° to about 90°. The harvest ripens about a fortnight earlier than among the mountains. Citrons and oranges flourish, as do, melons and palms: the latter do not fruit abundantly, but this is less the fault of climate than of carelessness in fertilization. The rainfall is rather lower than among the mountains. In the mountainous regions the mean annual temperature is about 62°, but there is a great range of variation. In winter there are often several degrees of frost, though snow very rarely lies for more than a day or two. In summer the thermometer occasionally registers as much as 100° in the shade, or even a degree or two more: this however is exceptional, and 80°-90° is a more normal maximum for the year. The rainfall is about 28 in., sometimes less, and in exceptional years as much as 10 in. in excess of this figure has been registered. The vine, fig and olive grow well in this region. The climate of the Ghor, again, is different. Here the thermometer may rise as high as 130°. The rainfall is scanty, but as no civilized person inhabits the southern end of the Jordan valley throughout the year, and it has hitherto proved impossible to establish self-registering instruments, no systematic meteorological observations have been taken. In Eastern Palestine there is even a greater range of temperature; the loftier heights are covered in winter with snow. The thermometer may range within twenty-four hours from freezing-point to 80°.
The rainy season begins about the end of November, usually with a heavy thunderstorm: the rain at this part of the year is the “former rain” of the Old Testament. The earth, baked hard by the summer heat, is thus softened, and ploughing begins at once. The wettest month, as indicated by meteorological observation, is January; February is second to it, and December third; March is also a very wet month. In April the rains come to an end (the “latter rains”) and the winter crops receive their final fertilization. The winter crops (barley and wheat) are harvested from April to June. The summer crops (millet, sesame, figs, melons, grapes, olives, &c.) are fertilized by the heavy “dews” which are one of the most remarkable climatic features of the country and to a large extent atone for the total lack of rain for one half the year. These crops are harvested from August to October.
Water Supply.—Notwithstanding the long drought, it must not be supposed that Palestine is a waterless country, except in certain districts. There are very few spots from which a spring of some sort is not accessible. Perennial streams are, and in the recent geological ages always have been, rare in the country. The whole face of the land is pitted with ancient cisterns; indeed, many hillsides and fields are on that account most dangerous to walk over by night, except for those who are thoroughly familiar with the landmarks. These cisterns are bell-shaped or bottle-shaped excavations, with a narrow circular shaft in the top, hollowed in the rock and lined with cement. Besides these, more ambitious works are to be found, all now more or less ruined, in various parts of the country (see Aqueducts: Ancient). Such are the aqueducts, of which remains exist at Jericho, Caesarea and other places east and west of the Jordan; but especially must be mentioned the enormous reservoirs known as Solomon’s Pools, in a valley between Jerusalem and Hebron, by which the former city was supplied with water through an elaborate system of conduits. Many of these aqueducts, as well as countless numbers of now leaky cisterns, could with but little trouble be brought into use again, and would greatly enhance the fertility of the country. The most abundant springs in Palestine are the sources of the Jordan at Banias and at Tell el-Kadi. A considerable number of springs in the country are brackish, being impregnated with chemicals of various kinds or (when near a town) with sewage. The latter is the case of the Virgin’s Fountain (Ain Umm ed-Daraj), which is the only natural source of water in the neighbourhood of Jerusalem.
Hot springs are found in various parts of the country, especially at El-Hamma, about 1 m. south of Tiberias, where the water has a temperature of 140° F. This is still used for curative purposes, as it was in the days of Herod, but it is neglected and dirty. The spring of the Zerka Ma‛in (Calirrhoe) has a temperature of 142° F. There are also hot sulphur springs on the west side of the Dead Sea. Those of El-Hamma, below Gadara, are from 104° to 120° F. in temperature.
Fauna.—It has been calculated that about 595 different species of vertebrate animals are recorded or still to be found in Palestine—about 113 being mammals (including a few now extinct), 348 birds (including 30 species peculiar to the country), 91 reptiles and 43 fishes. Of the invertebrata the number is unknown, but it must be enormous. The most important domestic animals are the sheep and the goat; the breed of oxen is small and poor. The camel, the horse and the donkey are the draught animals; the flesh of the first
- ↑ See Lortet, La Mer Morte (Paris, 1877); E. Hull, Mount Seir, Sinai and Western Palestine (London, 1885); and Memoir on the Geology and Geography of Arabia Petraea, Palestine, and adjoining Districts (London, 1886).
