Terminology

The word “Palestine” is derived from the name of one of the Sea Peoples (Heb. pelishtim) who migrated to the southern coastal region of the Fertile Crescent from one or more of the coastal regions of the Mediterranean (see Philistines).

The word “Palestine” has at times been used to refer to an area as small as this southwestern coastal region (functioning at times as a synonym for “Philistia”) and as large as the land on both sides of the Jordan River, including the Negev in the south.

Most English versions of the Bible do not mention “Palestine,” although in the KJV the Hebrew word peleshet (usually rendered “Philistia” or “Philistines”) is translated as “Palestina” in Exod. 15:14; Isa. 14:29, 31 and as “Palestine” in Joel 3:4.

Other designations of this region within the Scripture include “Canaan” (Gen. 10:19; Josh. 22:9), “the land” (Gen. 13:17; Josh. 2:1), “the land of Canaan” (Gen. 17:8; Num. 13:2), “the land of the Hebrews” (Gen. 40:15), “the land . . . promised on oath” (Gen. 50:24; Deut. 6:23), in various combinations and order “the land of the Canaanites, Hittites, Amorites, Hivites, Periz-zites, Jebusites, and Girgashites” (Exod. 3:17; 13:5; 23:23), “the Lord’s land” (Josh. 22:19), “the land of Israel” (1 Sam. 13:19; Ezek. 47:18), and “Trans-Euphrates,” which was “beyond the river” from the perspective of those in Persia (Ezra 4:10; Neh. 2:7). Compare also “the tribes of Israel” (2 Sam. 24:2; Ezek. 47:13), “Israel and Judah” (2 Sam. 5:5; 2 Chron. 30:6), and “from Dan to Beersheba” (Judg. 20:1; 1 Kings 4:25).

In the NT, this territory is usually designated by reference to the provinces of Judea and Galilee (Matt. 2:22; John 7:1), which sometimes are mentioned with the Decapolis (Matt. 4:25) and Samaria (Acts 9:31; cf. Luke 3:1).

Boundaries and Size

Boundaries. Palestine is in the southwestern portion of the Fertile Crescent (i.e., western Iraq, Syria, Lebanon, Jordan, and Israel). It is located northeast of the Nile River basin and west-southwest of the basins of the Tigris and Euphrates rivers.

Generally speaking, it is bounded by Lebanon to the north, the Mediterranean Sea (= the Sea, the Great Sea, or the western sea) on the west, Wadi el-Arish (= the river of Egypt, the Wadi of Egypt) in the southwest, the Sinai Peninsula in the south, and the Transjordan in the east (Gen. 15:18; Num. 34:3–7, 11–12; Deut. 1:7; 11:24; 34:2; Josh. 1:4; 11:16; 2 Kings 24:7). When the Transjordan is considered part of Palestine (cf. Deut. 34:1), the eastern boundary is the Syrian (Syro-Arabian) Desert. In several biblical texts the northeast boundary of this region is “the great river, the Euphrates” (Gen. 15:18; Deut. 1:7; 11:24; Josh. 1:4; 1 Chron. 5:9; cf. 2 Sam. 8:3).

Size. Because of fluidity in the use of the term “Palestine,” it is difficult to speak precisely of the land area designated by it. Palestine west of the Jordan River is about six thousand square miles, similar to the land area of the state of Hawaii.

A description of “the whole land” viewed by Moses included both the Negev and Gilead, part of the Transjordan (Deut. 34:1–3). In the OT, the Negev is regularly included as one of the regions of the land on the west side of the Jordan (Deut. 1:7; Josh. 10:40; 11:16; Jer. 17:26). The unity of the land on both sides of the Jordan is reflected in texts that focus on Israel’s inheritance of land (Deut. 3:12–17), cities of refuge (Num. 35:14; Josh. 20:7–8), and military victories (Josh. 12:1–8; 24:8–13).

The land area of Palestine increases considerably if one includes these areas, for the Transjordan region is about 4,000 square miles, while the Negev is about 4,600 square miles.

Topographical Regions

Frequent seismic activity, the rising and falling of the landmass, and deposits from the inundation and withdrawal of seas produced seven topographical regions current in Palestine.

Coastal plain. The coastal plain is the fertile terrain bordering the Mediterranean, though the coastline itself consists of beaches, sand dunes, wetlands, and rock cliffs.

The southern portion of the coastal plain was once inhabited by the Philistines (with the coastal cities of Gaza, Ashkelon, and Ashdod). Moving north of the Yarkon River, we pass through the marshy Plain of Sharon and the Dor Plain. In the north, hills rise near Carmel and extend west to the central highlands. North of the Carmel range lie the Acco Plain, the Asher Plain, and the coastlands of Phoenicia (including Tyre and Sidon).

Hill country. The hill country is located between, and runs parallel to, the coastal plain on the west and the Jordan Valley on the east. The hills, ridges, plateaus, and valleys of the hill country are the setting for most of the OT narratives.

The hill country is bisected by the Jezreel Valley, which runs east-west from the Jordan Valley to the Bay of Acco (Haifa Bay), north of Carmel.

The hill country south of the Jezreel Valley is called “the central highlands,” which consist of the rough and rocky hills of Samaria in the north (such as Mount Gerizim and Mount Ebal) and the more arid (and, historically, less populated) Judean hill country in the south. The highest hills of this area exceed three thousand feet.

In Scripture the southern hill country (or portions of it) is called “the hill country of Judah/Judea” (Josh. 11:21; Luke 1:39) and “the hill country of Bethel” (Josh. 16:1; 1 Sam. 13:2), while the northern (Samarian) hill country (or portions of it) is called “the hill country of Israel” (Josh. 11:21), “the hill country of Naphtali” (Josh. 20:7), and, most frequently, “the hill country of Ephraim” (Josh. 17:15; Judg. 2:9; 1 Kings 4:8).

The hill country north of the Jezreel Valley consists of two parts, Lower and Upper Galilee, divided by the fault through which runs Wadi esh-Shaghur. Lower Galilee has fertile basins and hills about two thousand feet above sea level. Farther north is Upper Galilee, with hills averaging about three thousand feet. It forms a transition to the mountains of Lebanon, which lie to the north.

The Shephelah (“lowland” or “piedmont”) is the region of gentle and rolling hills between five hundred and one thousand feet above sea level between the Judean hill country and the coastal plain. These hills formerly were covered with sycamore trees and provided Judeans with protection against an attack from the west.

Jezreel Valley. The Jezreel Valley is often equated with the Plain of Esdraelon, though some distinguish the fault basin (Esdraelon) from the rift valley (Jezreel).

On its west side, this fertile plain begins north of Carmel at the coast, moving east to the Jordan Valley. The central highlands lie to the north (Galilee) and south (Samaria) of this plain.

The fertile soil of this low-lying basin was valued for farming. Traders and armies regularly passed through this great plain, and it was often the place of military conflict (cf. Judg. 6:33; 1 Sam. 29:1, 11; Hos. 1:5).

Jordan Valley. The Jordan Valley (also known as the Jordan Rift Valley or the Dead Sea Rift) begins near the base of Mount Hermon in the north (9,232 feet). Moving south, the rift continues to the Hula Valley, through which the Jordan River flows to the Sea of Galilee (Sea of Gennesaret, Lake Kinnereth). The Sea of Galilee is about twelve miles long and five miles wide, located within an area of hills and valleys.

The Jordan River meanders south, flowing through a deep gorge and falling three thousand feet before coming to the Dead Sea (also called “the Sea of the Arabah” [Deut. 4:49; Josh. 3:16] and “the Salt Sea” [Num. 34:3, 12; Josh. 15:2, 5 ESV, NASB]), the lowest place on earth. At its lowest point, the Dead Sea is more than 2,600 feet below sea level.

The Jordan Valley rises as one continues south from the Dead Sea (forty-eight miles long and eight miles wide) through the arid Arabah (cf. Isa. 33:9; Zech. 14:10) to the Gulf of Aqaba.

The term “Arabah” is generally used to refer to the extension of the rift south of the Dead Sea, though at one time in the history of ancient Israel it referred to a region that included the Jordan Valley between the Sea of Galilee and the Dead Sea, on both the east (Deut. 3:17; Josh. 12:1–3) and the west (Deut. 11:30; Josh. 11:2; Ezek. 47:8) sides of the Jordan River.

Transjordan. The Transjordan region is located east of the Jordan Valley and west of the Syrian (Syro-Arabian) Desert. Three major rivers run across this region, each moving from east to west. The Yarmouk (Yarmuk) and the Jabbok (Zarqa) rivers empty into the Jordan River, while the Arnon River (Wadi el-Mujib) flows into the Dead Sea.

In ancient Israel, regions of the Transjordan, from north to south, included Bashan (Karnaim), north of the Yarmuk River; Gilead, south of the Yarmuk; Ammon, the region of modern-day Amman, southeast of Gilead; Moab, south of the Arnon River; and Edom, south of Wadi el-Hesa (Zered River [cf. Num. 21:12; Deut. 2:13–14]).

The capture of the territory belonging to Sihon between the Jabbok and the Arnon rivers was a significant event in the history of ancient Israel (Num. 21:24; Josh. 12:1–2).

Although the Transjordan is often excluded from “Palestine,” there were times in biblical history when the land on both sides of the Jordan was considered a unit. For example, “the other half of Manasseh, the Reubenites and the Gadites” received their tribal inheritance east of the Jordan (cf. Josh. 13:8–32). They inhabited Bashan, Gilead, and the land of the Amorites (cf. Deut. 3:12–17; 34:1; Judg. 20:1).

According to 2 Sam. 8, David established control over Moab (vv. 2, 12), the Beqaa Valley (“along the Euphrates River” [v. 3 GW]), Aram (v. 6; vv. 12–13 MT), Ammon and Amalek (v. 12), and Edom (v. 14; vv. 12–13 LXX, Syriac; cf. 1 Chron. 18:2–13).

In Scripture, the central Transjordan hill country is sometimes called “the hill country of Gilead” (Gen. 31:21, 23, 25; Deut. 3:12). The southern elevated region in Edom is called “the hill country of Seir” (Gen. 36:8–9; Deut. 2:5).

Negev. The Negev (Negeb) is shaped like an inverted triangle with its peak at the southern city of Eilat (Elath) near the biblical Ezion Geber (cf. 1 Kings 9:26). It is bounded on the north by the Judean hill country, on the west by Sinai, and on the east by the Arabah Valley (which lies along the rift south of the Dead Sea).

The Negev is an extremely dry area, with the most rain found in the northern (twelve inches annually) and western (ten inches annually) sections, and the least in the Arabah Valley (two inches annually). It is a place of sand dunes, rocky desert, and brown hills that increase in height as one moves toward Sinai.

Although the Negev is described as “a land of hardship and distress, of lions and lionesses, of adders and darting snakes” (Isa. 30:6), it was also a place of wells and springs, in addition to cities and towns such as Beersheba (Josh. 15:21–32; 2 Sam. 24:7).

Sinai peninsula. The Sinai peninsula is about twenty-three thousand square miles. It consists primarily of plains, plateaus, and hills (the highest of which is Jebel Yiallaq, at 3,656 feet), with a coastline along the Mediterranean of 145 miles.

The longest river in the region is the Wadi el-Arish, which runs 155 miles northward from central Sinai to the Mediterranean.

Israel’s activities in the Desert of Sinai are often mentioned in the Pentateuch (e.g., Exod. 19:1–2; Num. 1:1; 9:5).

The Desert of Sinai is distinguished from the Desert of Sin (Exod. 16:1) and the Desert of Paran (Num. 10:12). Other arid areas within the Sinai Peninsula include the Desert of Zin (Num. 34:3), the Desert of Shur (Exod. 15:22), and the Desert of Etham (Num. 33:8).

Climate

The climate of Palestine consists of a dry and hot season from June to August and a wet season from mid-October to mid-April. It is common for the wet season to consist of two distinct periods of heavy rain, one at the beginning and one toward the end of this period (cf. “spring and autumn rains” [Deut. 11:14; Joel 2:23; James 5:7]).

Two transitional seasons of about six weeks each bridge the wet and the dry seasons. One occurs between early September and the end of October, the other between early April and the middle of June.

Average temperatures throughout the region range from 46.5–55 degrees (Fahrenheit) in January (both the coldest and the wettest month in Palestine) to 71.5–93 degrees in August.

Most rainfall in Palestine occurs as cyclonic storm systems (about twenty-five each year) bring warm air from North Africa eastward over the Mediterranean, clashing with cooler air from Europe and Asia. As clouds move over the land, precipitation falls heaviest on the west side of the hills, leaving the east side of the hills with less rain.

Typically, rainfall is heaviest in the northern areas of Palestine, the regions closest to the Mediterranean, and in the Transjordan. The area around the Dead Sea is extremely dry, with evaporation exceeding precipitation. In contrast, the northern highlands have forty inches of annual rainfall.

In Palestine, precipitation can also take the form of both snow (cf. 2 Sam. 23:20; Prov. 25:13) and, in a significant way, dew (cf. Judg. 6:37–40; Song 5:2). Dew provides moisture for agriculture especially in the coastal plain, the central highlands, and the Jezreel Valley.

During the transitional seasons, desiccating winds (sometimes called sirocco winds) bring warm desert air from the east (and at times from the south), raising the temperature and lowering the relative humidity throughout Palestine. These winds often bring fine dust from the desert. The effects are most onerous in the Jordan Valley. References to an east wind in Scripture are common (Gen. 41:6; Hos. 13:15; Jon. 4:8; see also “south wind” in Job 37:17; Luke 12:55).

Roads

Two major highways passed through Palestine: “the Way of the Sea,” or Via Maris (cf. Isa. 9:1; Matt. 4:15), and “the King’s Highway” (cf. Num. 20:17; 21:22).

The Way of the Sea moved north from Egypt through the coastal plain, heading east through the Jezreel Valley. From this point it branched out in three directions: northwest through Phoenicia, north toward Damascus, and east to join with the King’s Highway.

The King’s Highway was a Transjordanian route passing from the Gulf of Aqaba in the south (cf. Deut. 2:8) through Edom, Moab, Gilead, and Bashan to Damascus in the north.

Merchants and armies used these highways to pass through Palestine, while local traffic often used east-west roads to move throughout the area.