History of the Terms Palestine and Canaan. The term Palestine, originally applied to the home of Israel's foes, the Philistines, was used by the Greeks as a designation of southern Syria, exclusive of Phœnicia. The Greek historian Herodotus was the first to employ it in this extended sense. The Romans used the same term in the form Palestina and through them the term Palestine has become the prevailing name in the western world of the land once occupied by the Israelites and their immediate neighbors on the east and west. The history of the older name Canaan (Lowland) is similar. In the Tell el-Amarna Letters, written in the fourteenth century B.C., Canaan is limited to the coast plains; but as the Canaanites, the Lowlanders, began to occupy the inland plains the use of the term was extended until it became the designation of all the territory from the Mediterranean to the Jordan and Dead Sea valley. It does not appear, however, to have ever been applied to the east-Jordan land.
Bounds of Palestine. Palestine lies between the eastern shore of the Mediterranean Sea and the Arabian desert. Its northern boundary is the southern slope of Mount Hermon and the River Litany, as it turns abruptly to flow westward into the Mediterranean. Palestine begins where the Lebanons and Anti-Lebanons break into a series of elevated plateaus. Its southern boundary is the varying line drawn east from the southeastern end of the Mediterranean a little south of the Dead Sea at the point where the hills of Judah and the South Country descend to the desert. Palestine therefore lies between 33° 30' and 31° north latitude and 34° and 37° east longitude. Its approximate width is about a hundred miles and its length from north to south only about a hundred and fifty miles. It is, therefore, about the size of the State of Vermont.
Geological History. The geological history of Palestine is somewhat complex, but exceedingly illuminating. The underlying rock is granite. This is now almost completely concealed by later layers of sandstone (which appears in Edom and the east-Jordan), dolomitic and nummulitic limestone and marl. During the earlier geological periods the land was entirely covered by the waters of the sea. Probably at the close of the Pliocene period came the great volcanic upheaval which gave to Syria and Palestine their distinctive character. It left a huge rift running from north to south throughout Syria. This rift is represented to-day by the valley between the Lebanons and its continuation, the valley of the Jordan and Dead Sea. Further south it may be traced through the Wady Arabah and the Gulf of Akaba. This vast depression is the deepest to be found anywhere on the earth's surface. The same great volcanic upheaval gave to the mountains along the western coast their decided northern and southern trend and the peculiar cliff-like structure which characterizes their descent to the western shore. Through the centuries frequent and severe earthquakes have been felt along the borders of this ancient rift, and they are still the terror of the inhabitants, even as in the days of the Hebrew prophets.
Alluvial and Sand Deposits. Until a comparatively late geological period the sea came to the foot of the mountains. The coast rose gradually and has later been built up by the process of erosion that has cut down the mountains, especially on the western side, where the rainfall was heaviest. The plains along the shore have thus been enriched by vast alluvial deposits. Very different was the deposit of Nile sediment, which was blown in from the sea by the western winds, leaving a wide border of yellow sand along the coast of Palestine.
General Divisions. Palestine is sharply divided by nature into four divisions or zones, which extend in parallel lines from north to south.[(1)][1] Along the Great Sea lie the narrow coast plains which broaden in the south into the plains of Sharon and Philistia. The second zone is the central plateau, with hills three to four thousand feet in height in the north, which sink by stages to the large Plain of Esdraelon. South of this great plain lie the fertile hills of Samaria which in turn merge into the stern hills of Judah. These again descend into the low, rocky, rolling hills of the South Country. The third zone is the Jordan and Dead Sea valley which begins at the foot of Mount Hermon and rapidly sinks, until at the Dead Sea it is one thousand two hundred and ninety-two feet below the surface of the ocean. The fourth zone includes the elevated plateaus which extend east of the Jordan and Dead Sea out into the rocky Arabian desert.
Variety in Physical Contour. The first striking characteristic of Palestine is the great variety in physical contour, climate, flora, and fauna to be found within its narrow compass of less than fifteen thousand square miles. Coast plains, inland valleys, elevated plateaus, deep, hot gorges, and glimpses of snow-clad mountains are all included within the closest possible bounds. In a journey of from two to three days the traveller from west to east passes from the equable, balmy climate of the Mediterranean coast to the comparatively cold highlands of the central plateau and then down into the moist, tropical climate of the hot Jordan and Dead Sea valley. Thence he mounts the highlands of Gilead or Moab, where the sun beats down hot at noonday, while the temperature falls low at night and deep snows cover the hilltops in winter. The hills of the central plateaus, covered with the trees of the temperate zone, overhang the palms and tropical fruit trees of the coast plains and Jordan valley.
Effects of this Variety. The different zones touch each other closely, and yet their wide differences in physical contour, climate, flora and fauna constitute invisible but insuperable barriers and produce fundamentally diverse types of life and civilization. To-day, as in the past, inhabitants of cities, tent dwellers, merchants, and peasants live in this narrow land within a few miles, yet separated from each other by the widest possible difference in culture and manner of life. The character of the land made impossible a closely knit civilization. It could never become the centre of a great world-power. It was rather destined to be the abode of many small tribes or nations, with widely differing institutions and degrees of culture. The great variety of scenery, climate, and life, however, made Palestine an epitome of all the world. It was pre-eminently fitted to be the home of a people called to speak a vital message in universal terms to all the races of the earth. Its striking contrasts and its marvellous beauty and picturesqueness also arrested the attention of primitive men and explain the prominence of nature worship among the early inhabitants of Palestine and the large place that its rocks, brooks, hills and meadows occupy in Israel's literature.
Openness to the Arabian Desert. The second marked peculiarity of Palestine is its openness to the desert. As Principal Smith has aptly said, Palestine "lay, so to speak, broadside on to the desert." With its comparatively fertile fields, it has proved a loadstone that for thousands of years has attracted the wandering Arabian tribes. These came in, however, not as a rule in great waves, but as families, or small tribes. Up through the South Country they penetrated the hills of Judah. There in time they learned to cultivate the vine, although they still retained their flocks. East of Moab and Gilead the arable land merges gradually into the rocky desert and the Arabs to-day, as in the past, claim as their own all the land to the Jordan and Dead Sea valley, except where the settled population successfully contests their claim by arms. Palestine, therefore, has always been powerfully influenced by the peculiar life and centralized government and fierce rivalry between tribes and petty peoples—these are but a few of the characteristics of Palestine's history that are primarily due to its openness to Arabia.
Absence of Navigable Rivers and Good Harbors. Palestine, on the other hand, is shut off from close commercial contact with other peoples. No great waterway invited the trader and warrior to go out and conquer the rest of the world. Instead, in the early periods when men depended chiefly upon communication by river or sea, Palestine shut in its inhabitants and tended to develop an intensive rather than an extensive civilization. Its one large river, the Jordan, flows, not into the ocean, but into a low inland sea, whose only outlet is by evaporation. The coast line of Palestine is also characterized by the lack of a single good harbor. At Joppa, at the northwestern end of Carmel, and at Tyre the otherwise straight shore line curves slightly inland; but at each of these points there is no natural protection from the severe western gales. The Phœnicians, shut in by the eastern mountains, dared the perils of the deep; but to the early peoples of Palestine the Great Sea was, on the whole, a barrier rather than an invitation to commerce and conquest.
Incentives to Industry. The physical characteristics of Palestine were well fitted to develop active, industrious inhabitants. The constant pressure on their borders by Arabs, who could be held back only by a strong, organized civilization, was a powerful spur. The natural division of the land among independent and usually hostile races made eternal activity and watchfulness the price that must be paid for life and freedom. Popular tradition, based on a fact that pre-eminently impresses every traveller in the land to-day, states that the fabled Titan, who was sent to scatter stones over the face of the earth, distributed them equally over Europe and Africa, but that when he came to Asia and was passing through Syria, his bag broke, depositing its contents on Palestine. Throughout most of its territory the rich soil can be cultivated only as the stones are gathered either in huge heaps or fences. The fertility of the plains can be utilized only as the waters of the mountain brooks are used for irrigation. It is, therefore, a land that bred hardy men, strong of muscle, resourceful, alert, and, active in mind and body.