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Translation	Verse	Text
King James	Jud 12:5	And the Gileadites took the passages of Jordan before the Ephraimites: and it was so, that when those Ephraimites which were escaped said, Let me go over; that the men of Gilead said unto him, Art thou an Ephraimite? If he said, Nay;

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Word	King James Dictionary - Definition
ART	Are; second person singular.

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Word	Easton Dictionary - Definition
GILEAD	hill of testimony, (Gen. 31:21), a mountainous region east of Jordan. From its mountainous character it is called "the mount of Gilead" (Gen. 31:25). It is called also "the land of Gilead" (Num. 32:1), and sometimes simply "Gilead" (Ps. 60:7; Gen. 37:25). It comprised the possessions of the tribes of Gad and Reuben and the south part of Manasseh (Deut. 3:13; Num. 32:40). It was bounded on the north by Bashan, and on the south by Moab and Ammon (Gen. 31:21; Deut. 3:12-17). "Half Gilead" was possessed by Sihon, and the other half, separated from it by the river Jabbok, by Og, king of Bashan. The deep ravine of the river Hieromax (the modern Sheriat el-Mandhur) separated Bashan from Gilead, which was about 60 miles in length and 20 in breadth, extending from near the south end of the Lake of Gennesaret to the north end of the Dead Sea. Abarim, Pisgah, Nebo, and Peor are its mountains mentioned in Scripture.

Word

Easton Dictionary - Definition

GILEAD

hill of testimony, (Gen. 31:21), a mountainous region east of Jordan. From its mountainous character it is called "the mount of Gilead" (Gen. 31:25). It is called also "the land of Gilead" (Num. 32:1), and sometimes simply "Gilead" (Ps. 60:7; Gen. 37:25). It comprised the possessions of the tribes of Gad and Reuben and the south part of Manasseh (Deut. 3:13; Num. 32:40). It was bounded on the north by Bashan, and on the south by Moab and Ammon (Gen. 31:21; Deut. 3:12-17). "Half Gilead" was possessed by Sihon, and the other half, separated from it by the river Jabbok, by Og, king of Bashan. The deep ravine of the river Hieromax (the modern Sheriat el-Mandhur) separated Bashan from Gilead, which was about 60 miles in length and 20 in breadth, extending from near the south end of the Lake of Gennesaret to the north end of the Dead Sea. Abarim, Pisgah, Nebo, and Peor are its mountains mentioned in Scripture.

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Word	American Tract Society - Definition
JORDAN	The chief river of Palestine, running from north to south, and dividing the Holy Land into two parts, of which the larger and more important lay on the west. There are two small streams, each of which claims to be its source. One of these, near Banias, anciently Caesarea Philippi, issues from a large cave in a rocky mountain side, and flows several miles towards the south-west, where it is joined by the second and larger stream, which originates in a fountain at Tellel-Kady, three miles west of Banias. But besides these, there is a third and longer stream, which rises beyond the northern limit of Palestine, near Hasbeia on the west side of mount Hermon, flows twenty-four miles to the south, and unites with the other streams before they enter the "waters of Merom," now lake Huleh, the Jordan flows about nine miles south-ward to the sea of Tiberias, through which its clear and smooth course may be traced twelve miles to the lower end. Hence it pursues its sinuous way to the south, till its pure waters are lost in the bitter sea of Sodom. Between these two seas, that of Tiberias and the Dead Sea, lies the great valley or plain of the Jordan, 2Ki 25:4 2Ch 4:17. It is called by the Arabs El-Ghor. Its average width is about five miles, but near Jericho it is twelve or fifteen miles. It is terminated on both sides, through its whole length, by hills, which rise abruptly on the western border 1,000 or 1,200 feet high, and more gradually on the east, but twice as high. This valley is excessively not, and except where watered by fountains or rivulets, is sandy and destitute of foliage. It is covered in many parts with innumerable cone-like mounds, and sometimes contains a lower and narrow terrace of similar character, perhaps an eighth of a mile wide. Through this valley the river takes its serpentine course in a channel from fifteen to fifty feet below the general level. Its immediate banks are thickly covered with trees and shrubs, such as the willow, tamarisk, and oleander; and often recede, and leave a larger space for vegetation. In the lower Jordan, the stream is bordered by numerous canebrakes. The thickets adjoining the river were formerly the retreat of wild beasts, which of course would be driven out by a freshet; hence the figure, "He shall come up like a lion from the swelling of Jordan," Jer 49:19 50:44. The channel of the river may be deeper sunk than of old, but even now not only the intervales within the banks are overflowed in spring, but in many places the banks themselves, 1Ch 12:15. Lieutenant Lynch of the United States navy, who traversed the Jordan in 1848, ascertained that, although the distance from the sea of Galilee to the Dead Sea is but sixty miles in a straight line, it is two hundred miles by the course of the river, which has innumerable curves. Its width varies at different points from seventy-five to two hundred feet, and its depth from three to twelve feet. Its volume of water differs exceedingly at different seasons and from year to year. The current is usually swift and strong; and there are numerous rapids and falls, of which no less than twenty-seven are specified by Lieutenant Lynch as dangerous even to his metallic boats. The sea of Tiberias lies 312 (according to Lynch, 653) feet below the level of the Mediterranean, and the Dead Sea 1,316 feet; hence the fall of the Jordan between the two seas is 1,000 feet. The waters of the Jordan are cool and soft, and like the Sea of Galilee, it abounds in fish. It is crossed by a stone bridge, below Lake Huleh, (see GESHUR, GESHURI, GESHURITES;) and the fragments of another, just south of the Sea of Tiberias, still remain. Several fords, available in ordinary season, are mentioned in Scripture, Jud 3:28 12:5 2Sa 17:22-24. Ferryboats were also used, 2Sa 19:17,18,39. See SEA 4. It was during the annual "swelling of the Jordan" that Joshua and the Israelites crossed it, Jos 3:15. Yet the swift and swollen current was arrested in its course, opposite to Jericho; and while the waters below the city rolled on to the4 sea, those above it were miraculously stayed, and left in the river bed a wide passage for the hosts of Israel. Twice afterwards the Jordan was miraculously crossed, by Elijah and Elisha, 2Ki 5:14 6:6. Here, too, our Savior was baptized, Mt 3:13; and this event is commemorated, in the middle of April of each year, by thousands of pilgrims of various sects of nominal Christians, who on a given day, and under the protection of a strong Turkish escort, visit the sacred river, drink and bathe in its waters, and after an hour or two return to Jerusalem. The principal branches of the Jordan are the Yermak, anciently Hieroma, a large stream, and the Jabbok, both on the east. There are several small rivulets and many mountain brooks, which dry up more or less early in the summer. The phrase, "beyond Jordan," usually indicates the east side of the river, but before the conquest by Joshua it meant the west side. At the present day, the Jordan is lost in the Dead sea; but many have supposed that in very ancient times, before the destruction of the cities in the vale of Sodom, the Jordan passed through the Dead Sea and the vale of Siddim, and continued its course southward to the Elanitic Gulf of the Red Sea. The southern end of the Dead Sea is found to be connected with the Elanitic gulf, or gulf of Akaba, by the great valley, called El-Arabah, forming a prolongation of El-Ghor, the valley of the Jordan. See map in EXODUS. The course of this valley is between south and south-southwest. Its length, from the Dead Sea to Akaba, is about one hundred miles in a direct line. From the extremity of the Dead Sea, a sandy plain extends southward between hills, and on a level with the sea, for the distance of eight or ten miles, where it is interrupted by a chalky cliff, from sixty to eighty feet high, which runs nearly across the valley, but leaves at its western end the opening of a valley nearly half a mile wide, which runs up for many miles to the south within the broad and desert valley El-Arabah, upon which it at length emerges, and the water of which it conveys to the Dead Sea. The cliff above referred to, probably the Akrabbim of the Bible, marks the termination of El-Ghor and the commencement of El-Arabah, which is thence prolonged without interruption to Akaba. It is skirted on each side by a chain of mountains; but the streams which descend from these, are in summer lost in their gravelly beds before they reach the valley below; so that this lower plain is in summer entirely without water, which alone can produce verdure in the Arabian deserts and render them habitable. There is not the slightest appearance of a road, or of any other work of human art, in any part of the valley. The opinion that the Jordan formerly traversed this great valley is rendered untenable by the fact that the Dead Sea lies nearly 1,300 feet lower than the Gulf of Akaba, and that most of the intervening region now pours its streams north into the Dead Sea. Of course the Jordan must also have stopped there of old, as it does now, unless, according to the somewhat startling theory of Lieutenant Lynch and others, the Dead sea-and with it, though less deeply, the whole valley to the north and south-sunk down from a higher level into its present deep chasm, perhaps long before that appalling catastrophe from which Lot found refuge in "the mountain," Ge 19:17-28,30. See SEA 3.

Word

American Tract Society - Definition

JORDAN

The chief river of Palestine, running from north to south, and dividing the Holy Land into two parts, of which the larger and more important lay on the west. There are two small streams, each of which claims to be its source. One of these, near Banias, anciently Caesarea Philippi, issues from a large cave in a rocky mountain side, and flows several miles towards the south-west, where it is joined by the second and larger stream, which originates in a fountain at Tellel-Kady, three miles west of Banias. But besides these, there is a third and longer stream, which rises beyond the northern limit of Palestine, near Hasbeia on the west side of mount Hermon, flows twenty-four miles to the south, and unites with the other streams before they enter the "waters of Merom," now lake Huleh, the Jordan flows about nine miles south-ward to the sea of Tiberias, through which its clear and smooth course may be traced twelve miles to the lower end. Hence it pursues its sinuous way to the south, till its pure waters are lost in the bitter sea of Sodom.

Between these two seas, that of Tiberias and the Dead Sea, lies the great valley or plain of the Jordan, 2Ki 25:4 2Ch 4:17. It is called by the Arabs El-Ghor. Its average width is about five miles, but near Jericho it is twelve or fifteen miles. It is terminated on both sides, through its whole length, by hills, which rise abruptly on the western border 1,000 or 1,200 feet high, and more gradually on the east, but twice as high. This valley is excessively not, and except where watered by fountains or rivulets, is sandy and destitute of foliage. It is covered in many parts with innumerable cone-like mounds, and sometimes contains a lower and narrow terrace of similar character, perhaps an eighth of a mile wide. Through this valley the river takes its serpentine course in a channel from fifteen to fifty feet below the general level. Its immediate banks are thickly covered with trees and shrubs, such as the willow, tamarisk, and oleander; and often recede, and leave a larger space for vegetation. In the lower Jordan, the stream is bordered by numerous canebrakes. The thickets adjoining the river were formerly the retreat of wild beasts, which of course would be driven out by a freshet; hence the figure, "He shall come up like a lion from the swelling of Jordan," Jer 49:19 50:44. The channel of the river may be deeper sunk than of old, but even now not only the intervales within the banks are overflowed in spring, but in many places the banks themselves, 1Ch 12:15. Lieutenant Lynch of the United States navy, who traversed the Jordan in 1848, ascertained that, although the distance from the sea of Galilee to the Dead Sea is but sixty miles in a straight line, it is two hundred miles by the course of the river, which has innumerable curves. Its width varies at different points from seventy-five to two hundred feet, and its depth from three to twelve feet. Its volume of water differs exceedingly at different seasons and from year to year. The current is usually swift and strong; and there are numerous rapids and falls, of which no less than twenty-seven are specified by Lieutenant Lynch as dangerous even to his metallic boats. The sea of Tiberias lies 312 (according to Lynch, 653) feet below the level of the Mediterranean, and the Dead Sea 1,316 feet; hence the fall of the Jordan between the two seas is 1,000 feet. The waters of the Jordan are cool and soft, and like the Sea of Galilee, it abounds in fish. It is crossed by a stone bridge, below Lake Huleh, (see GESHUR, GESHURI, GESHURITES;) and the fragments of another, just south of the Sea of Tiberias, still remain. Several fords, available in ordinary season, are mentioned in Scripture, Jud 3:28 12:5 2Sa 17:22-24. Ferryboats were also used, 2Sa 19:17,18,39. See SEA 4.

It was during the annual "swelling of the Jordan" that Joshua and the Israelites crossed it, Jos 3:15. Yet the swift and swollen current was arrested in its course, opposite to Jericho; and while the waters below the city rolled on to the4 sea, those above it were miraculously stayed, and left in the river bed a wide passage for the hosts of Israel. Twice afterwards the Jordan was miraculously crossed, by Elijah and Elisha, 2Ki 5:14 6:6. Here, too, our Savior was baptized, Mt 3:13; and this event is commemorated, in the middle of April of each year, by thousands of pilgrims of various sects of nominal Christians, who on a given day, and under the protection of a strong Turkish escort, visit the sacred river, drink and bathe in its waters, and after an hour or two return to Jerusalem.

The principal branches of the Jordan are the Yermak, anciently Hieroma, a large stream, and the Jabbok, both on the east. There are several small rivulets and many mountain brooks, which dry up more or less early in the summer. The phrase, "beyond Jordan," usually indicates the east side of the river, but before the conquest by Joshua it meant the west side.

At the present day, the Jordan is lost in the Dead sea; but many have supposed that in very ancient times, before the destruction of the cities in the vale of Sodom, the Jordan passed through the Dead Sea and the vale of Siddim, and continued its course southward to the Elanitic Gulf of the Red Sea. The southern end of the Dead Sea is found to be connected with the Elanitic gulf, or gulf of Akaba, by the great valley, called El-Arabah, forming a prolongation of El-Ghor, the valley of the Jordan. See map in EXODUS. The course of this valley is between south and south-southwest. Its length, from the Dead Sea to Akaba, is about one hundred miles in a direct line. From the extremity of the Dead Sea, a sandy plain extends southward between hills, and on a level with the sea, for the distance of eight or ten miles, where it is interrupted by a chalky cliff, from sixty to eighty feet high, which runs nearly across the valley, but leaves at its western end the opening of a valley nearly half a mile wide, which runs up for many miles to the south within the broad and desert valley El-Arabah, upon which it at length emerges, and the water of which it conveys to the Dead Sea. The cliff above referred to, probably the Akrabbim of the Bible, marks the termination of El-Ghor and the commencement of El-Arabah, which is thence prolonged without interruption to Akaba. It is skirted on each side by a chain of mountains; but the streams which descend from these, are in summer lost in their gravelly beds before they reach the valley below; so that this lower plain is in summer entirely without water, which alone can produce verdure in the Arabian deserts and render them habitable. There is not the slightest appearance of a road, or of any other work of human art, in any part of the valley. The opinion that the Jordan formerly traversed this great valley is rendered untenable by the fact that the Dead Sea lies nearly 1,300 feet lower than the Gulf of Akaba, and that most of the intervening region now pours its streams north into the Dead Sea. Of course the Jordan must also have stopped there of old, as it does now, unless, according to the somewhat startling theory of Lieutenant Lynch and others, the Dead sea-and with it, though less deeply, the whole valley to the north and south-sunk down from a higher level into its present deep chasm, perhaps long before that appalling catastrophe from which Lot found refuge in "the mountain," Ge 19:17-28,30. See SEA 3.

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Word	Easton Dictionary - Definition
JORDAN	Heb. Yarden, "the descender;" Arab. Nahr-esh-Sheriah, "the watering-place" the chief river of Palestine. It flows from north to south down a deep valley in the centre of the country. The name descender is significant of the fact that there is along its whole course a descent to its banks; or it may simply denote the rapidity with which it "descends" to the Dead Sea. It originates in the snows of Hermon, which feed its perennial fountains. Two sources are generally spoken of. (1.) From the western base of a hill on which once stood the city of Dan, the northern border-city of Palestine, there gushes forth a considerable fountain called the Leddan, which is the largest fountain in Syria and the principal source of the Jordan. (2.) Beside the ruins of Banias, the ancient Caesarea Philippi and the yet more ancient Panium, is a lofty cliff of limestone, at the base of which is a fountain. This is the other source of the Jordan, and has always been regarded by the Jews as its true source. It rushes down to the plain in a foaming torrent, and joins the Leddan about 5 miles south of Dan (Tell-el-Kady). (3.) But besides these two historical fountains there is a third, called the Hasbany, which rises in the bottom of a valley at the western base of Hermon, 12 miles north of Tell-el-Kady. It joins the main stream about a mile below the junction of the Leddan and the Banias. The river thus formed is at this point about 45 feet wide, and flows in a channel from 12 to 20 feet below the plain. After this it flows, "with a swift current and a much-twisted course," through a marshy plain for some 6 miles, when it falls into the Lake Huleh, "the waters of Merom" (q.v.). During this part of its course the Jordan has descended about 1,100 feet. At Banias it is 1,080 feet above sea-level. Flowing from the southern extremity of Lake Huleh, here almost on a level with the sea, it flows for 2 miles "through a waste of islets and papyrus," and then for 9 miles through a narrow gorge in a foaming torrent onward to the Sea of Galilee (q.v.). "In the whole valley of the Jordan from the Lake Huleh to the Sea of Galilee there is not a single settled inhabitant. Along the whole eastern bank of the river and the lakes, from the base of Hermon to the ravine of Hieromax, a region of great fertility, 30 miles long by 7 or 8 wide, there are only some three inhabited villages. The western bank is almost as desolate. Ruins are numerous enough. Every mile or two is an old site of town or village, now well nigh hid beneath a dense jungle of thorns and thistles. The words of Scripture here recur to us with peculiar force: 'I will make your cities waste, and bring your sanctuaries unto desolation...And I will bring the land into desolation: and your enemies which dwell therein shall be astonished at it...And your land shall be desolate, and your cities waste. Then shall the land enjoy her sabbaths, as long as it lieth desolate' (Lev. 26:31-34).", Dr. Porter's Handbook. From the Sea of Galilee, at the level of 682 feet below the Mediterranean, the river flows through a long, low plain called "the region of Jordan" (Matt. 3:5), and by the modern Arabs the Ghor, or "sunken plain." This section is properly the Jordan of Scripture. Down through the midst of the "plain of Jordan" there winds a ravine varying in breadth from 200 yards to half a mile, and in depth from 40 to 150 feet. Through it the Jordan flows in a rapid, rugged, tortuous course down to the Dead Sea. The whole distance from the southern extremity of the Sea of Galilee to the Dead Sea is in a straight line about 65 miles, but following the windings of the river about 200 miles, during which it falls 618 feet. The total length of the Jordan from Banias is about 104 miles in a straight line, during which it falls 2,380 feet. There are two considerable affluents which enter the river between the Sea of Galilee and the Dead Sea, both from the east. (1.) The Wady Mandhur, called the Yarmuk by the Rabbins and the Hieromax by the Greeks. It formed the boundary between Bashan and Gilead. It drains the plateau of the Hauran. (2.) The Jabbok or Wady Zerka, formerly the northern boundary of Ammon. It enters the Jordan about 20 miles north of Jericho. The first historical notice of the Jordan is in the account of the separation of Abraham and Lot (Gen. 13:10). "Lot beheld the plain of Jordan as the garden of the Lord." Jacob crossed and recrossed "this Jordan" (32:10). The Israelites passed over it as "on dry ground" (Josh. 3:17; Ps. 114:3). Twice afterwards its waters were miraculously divided at the same spot by Elijah and Elisha (2 Kings 2:8, 14). The Jordan is mentioned in the Old Testament about one hundred and eighty times, and in the New Testament fifteen times. The chief events in gospel history connected with it are (1) John the Baptist's ministry, when "there went out to him Jerusalem, and all Judaea, and were baptized of him in Jordan" (Matt. 3:6). (2.) Jesus also "was baptized of John in Jordan" (Mark 1:9).

Word

Easton Dictionary - Definition

JORDAN

Heb. Yarden, "the descender;" Arab. Nahr-esh-Sheriah, "the watering-place" the chief river of Palestine. It flows from north to south down a deep valley in the centre of the country. The name descender is significant of the fact that there is along its whole course a descent to its banks; or it may simply denote the rapidity with which it "descends" to the Dead Sea.

It originates in the snows of Hermon, which feed its perennial fountains. Two sources are generally spoken of. (1.) From the western base of a hill on which once stood the city of Dan, the northern border-city of Palestine, there gushes forth a considerable fountain called the Leddan, which is the largest fountain in Syria and the principal source of the Jordan.

(2.) Beside the ruins of Banias, the ancient Caesarea Philippi and the yet more ancient Panium, is a lofty cliff of limestone, at the base of which is a fountain. This is the other source of the Jordan, and has always been regarded by the Jews as its true source. It rushes down to the plain in a foaming torrent, and joins the Leddan about 5 miles south of Dan (Tell-el-Kady).

(3.) But besides these two historical fountains there is a third, called the Hasbany, which rises in the bottom of a valley at the western base of Hermon, 12 miles north of Tell-el-Kady. It joins the main stream about a mile below the junction of the Leddan and the Banias. The river thus formed is at this point about 45 feet wide, and flows in a channel from 12 to 20 feet below the plain. After this it flows, "with a swift current and a much-twisted course," through a marshy plain for some 6 miles, when it falls into the Lake Huleh, "the waters of Merom" (q.v.).

During this part of its course the Jordan has descended about 1,100 feet. At Banias it is 1,080 feet above sea-level. Flowing from the southern extremity of Lake Huleh, here almost on a level with the sea, it flows for 2 miles "through a waste of islets and papyrus," and then for 9 miles through a narrow gorge in a foaming torrent onward to the Sea of Galilee (q.v.).

"In the whole valley of the Jordan from the Lake Huleh to the Sea of Galilee there is not a single settled inhabitant. Along the whole eastern bank of the river and the lakes, from the base of Hermon to the ravine of Hieromax, a region of great fertility, 30 miles long by 7 or 8 wide, there are only some three inhabited villages. The western bank is almost as desolate. Ruins are numerous enough. Every mile or two is an old site of town or village, now well nigh hid beneath a dense jungle of thorns and thistles. The words of Scripture here recur to us with peculiar force: 'I will make your cities waste, and bring your sanctuaries unto desolation...And I will bring the land into desolation: and your enemies which dwell therein shall be astonished at it...And your land shall be desolate, and your cities waste. Then shall the land enjoy her sabbaths, as long as it lieth desolate' (Lev. 26:31-34).", Dr. Porter's Handbook.

From the Sea of Galilee, at the level of 682 feet below the Mediterranean, the river flows through a long, low plain called "the region of Jordan" (Matt. 3:5), and by the modern Arabs the Ghor, or "sunken plain." This section is properly the Jordan of Scripture. Down through the midst of the "plain of Jordan" there winds a ravine varying in breadth from 200 yards to half a mile, and in depth from 40 to 150 feet. Through it the Jordan flows in a rapid, rugged, tortuous course down to the Dead Sea. The whole distance from the southern extremity of the Sea of Galilee to the Dead Sea is in a straight line about 65 miles, but following the windings of the river about 200 miles, during which it falls 618 feet. The total length of the Jordan from Banias is about 104 miles in a straight line, during which it falls 2,380 feet.

There are two considerable affluents which enter the river between the Sea of Galilee and the Dead Sea, both from the east. (1.) The Wady Mandhur, called the Yarmuk by the Rabbins and the Hieromax by the Greeks. It formed the boundary between Bashan and Gilead. It drains the plateau of the Hauran.

(2.) The Jabbok or Wady Zerka, formerly the northern boundary of Ammon. It enters the Jordan about 20 miles north of Jericho.

The first historical notice of the Jordan is in the account of the separation of Abraham and Lot (Gen. 13:10). "Lot beheld the plain of Jordan as the garden of the Lord." Jacob crossed and recrossed "this Jordan" (32:10). The Israelites passed over it as "on dry ground" (Josh. 3:17; Ps. 114:3). Twice afterwards its waters were miraculously divided at the same spot by Elijah and Elisha (2 Kings 2:8, 14).

The Jordan is mentioned in the Old Testament about one hundred and eighty times, and in the New Testament fifteen times. The chief events in gospel history connected with it are (1) John the Baptist's ministry, when "there went out to him Jerusalem, and all Judaea, and were baptized of him in Jordan" (Matt. 3:6).

(2.) Jesus also "was baptized of John in Jordan" (Mark 1:9).

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Word	King James Dictionary - Definition
NAY	No.

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