Situation and Bounds of the Plain of Esdraelon. The Plain of Esdraelon is the last of the great terraces by which the Lebanons descend on the south to the sea-level. The plain itself lies only about two hundred feet above the level of the Mediterranean and to the east sinks toward the Jordan to below the sea-level. Its shape is that of an equiangular triangle. Its base lies close under the northeast side of Mount Carmel and is twenty miles long running from Tell el-Kasis to Jenîn. Its northern line runs along the foot of the Nazareth hills for fifteen miles to a point opposite Mount Tabor. The eastern boundary, from Tabor to Jenîn is also about fifteen miles in length but less regular. Moreh or Little Hermon and Mount Gilboa jut out into the plain, which sends down toward the Jordan two broad valleys, of which the most important is the plain of Jezreel to the north of Gilboa.[(10)] The watershed between these two plains is near the modern village of Zerin which stood not far from the ancient Jezreel.
Plain of Jezreel. The Plain of Jezreel extends like a great broad valley almost due east for about fifteen miles until it reaches the Jordan. Through it runs the Nahr Jalûd with its perennial parallel streams. Where the Plain of Jezreel joins the low-lying Jordan valley stands the guardian of the gateway, the town of Beisan, which represents the ancient Bethshean, later known as Scythopolis. This Plain of Jezreel, together with the narrow valley through which the Kishon now finds its way to the Mediterranean, completes the link between the Great Sea and the Jordan Valley and for a brief space separates the hills of Galilee from those of Samaria.
Water Supply and Fertility of the Plain of Esdraelon. Originally the Plain of Esdraelon appears to have been a shallow inland lake. Viewed from the top of Mount Gilboa it appears to be completely shut in by a circle of mountains on the north, west, and south.[(11)] Its elevation toward the east is so slight and its outlets to the east and west so imperfect that during the rainy season much of it is practically a morass. Into it drain the waters from the surrounding hills. Some of the drainage is on the surface, but most of it is underground, with the result that at many points on the plain rushing springs pour forth their waters, which run for a time as a dashing brook and then sink again into the porous soil. Springs of this character are found especially on the northeastern and southern sides of the plain. Some of them ultimately send their scattered waters down the Plain of Jezreel to the Jordan, but more of them find their outlet through the low, muddy Kishon, which, with many turnings, ploughs its way through the middle of the Plain of Esdraelon to the shadow of Mount Carmel and then finds a narrow outlet into the Mediterranean past the Galilean foot-hills, which here are scarcely one hundred yards from the spurs of Mount Carmel. As a result of its peculiar position and formation, the Plain of Esdraelon is one of the best watered areas in all Palestine. In certain places, indeed, it suffers from an excess of water. Its loamy, basaltic soil is also richly fertile and its alluvial deposits are free from stone. By nature it is fitted to be the great grain field of central Palestine. The hills that jut out into this garden land were naturally the first centres of a developed agricultural civilization. Here on the southern border are found the large mounds which were once the sites of teeming Canaanite cities.
Central and Commanding Position. The Plain of Esdraelon, like the Plain of Sharon, was a great highway of the nations. Through the broad valleys which lead into it came from every quarter the invaders, whether for peaceful or violent conquest, for here all the important roads converged. On its western border ran the great coast road from Egypt to Phœnicia. The eastern branches of the road also entered the plain from the south through three different avenues. The one was through the valley which led from the Plain of Sharon to the southeastern end of Mount Carmel. Still more direct and easy was the approach through northwestern Samaria along the Wady Arah, past the famous old fortress of Megiddo. The third was farther east along the broad Plain of Dothan to Engannim, the present Jenîn, and thence along the eastern side of the Plain of Esdraelon. These highways in turn connected with those which ran past Mount Tabor to the populous cities on the Lake of Gennesaret and thence to Damascus and the East. Another important artery of trade ran along the wide, level Plain of Jezreel, past Bethshean that guarded its eastern gateway[(12)] to the Jordan and thence northward to Damascus or directly eastward to Gilead and the desert (cf. chap. IX).
Importance of the Plain in Palestinian History. The Plain of Esdraelon was both the door and the key to Palestine. Through it came the ancient conquerors to possess the land. The Midianites in the days of Gideon were but a part of that ever-advancing Arab horde, which surged up through the Plain of Jezreel whenever the government of central Palestine was weak. On its gently sloping hills from the days of Thotmes III to Napoleon were waged the great battles that determined the possession of the land. Here, under the leadership of Deborah, the Hebrews fought the valiant fight that left them masters of Canaan and free to pass over the barrier of plain that had hitherto kept apart the tribes of the north from those of the south.
V
THE HILLS OF SAMARIA AND JUDAH
Character of the Hills of Samaria. The hills of Samaria and Judah are the southern extension of the central plateau of Palestine, and yet, like Galilee and Esdraelon they constitute an independent natural unit. No sharply defined boundary separates them; rather the one gradually merges into the other. The heights of Samaria and Judah are commonly called mountains and the term is not entirely inappropriate when applied to the range as a whole; but the individual peaks are in reality little more than rounded hills. None of them rise over three thousand four hundred feet above the sea-level. The highest rest upon elevated plateaus, so that only two or three of them convey the impression of towering height and majesty that is ordinarily associated with the word mountain. Rather they are a chain of hills which, viewed from the shore of the Mediterranean or from the heights east of the Jordan, give the impression of a bold mountain range. This is especially true as one looks up toward them from the deep depression of the Jordan and Dead Sea valley, for they completely fill the western horizon. The water=*shed lies on the eastern side of the range. The result is that the western hills have been worn down into gradually descending terraces; while on the east the deep Jordan valley is exceedingly abrupt, becoming more so in the south. At certain points the descent is over twenty-eight hundred feet in nine miles, and down by the western side of the Dead Sea there is often an almost sheer fall of between fifteen hundred and three thousand feet.