Hotels in Jordan
Jordan is a nation many people often like to visit to see the history, culture, sports, and tourist attractions of the nation. Some may want to stay at cheap or luxury hotels in the nation. Some may want to stay at large or small hotels in the nation. Some may want to visit hotels that have an impressive reputation. Some may want to stay at hotels with access to parking facilities. Some may want to stay at hotels that have access to quality facilities.

Hotels in the nation of Jordan are often needed for tourists who require short term accommodation.

Jordan (Arabic: al-'Urdunn), officially the Hashemite Kingdom of Jordan, is an Arab country in Southwest Asia spanning the southern part of the Syrian Desert down to the Gulf of Aqaba. It shares borders with Syria to the north, Iraq to the north-east, Israel and the Palestinian territories to the west, and Saudi Arabia to the east and south. It shares control of the Dead Sea with Israel, and the coastline of the Gulf of Aqaba with Israel, Saudi Arabia, and Egypt. Much of Jordan is covered by desert, particularly the Arabian Desert; however the north-western area, with the sacred Jordan River, is regarded as part of the Fertile Crescent. The capital city of Amman is in the north-west.

During its history, Jordan has seen numerous civilizations, including such ancient eastern civilizations as the Sumerian, Akkadian, Babylonian, Assyrian, Mesopotamian, and Persian empires. Jordan was for a time part of Pharaonic Egypt, and spawned the native Nabatean civilization who left rich archaeological remains at Petra. Cultures from the west also left their mark, such as the Macedonian, Roman, Byzantine, and Ottoman Turkish empires. Since the seventh century the area has been under Muslim and Arab cultures, with the exception of a brief period under British rule.

The Hashemite Kingdom of Jordan is a constitutional monarchy with representative government. The reigning monarch is the head of state, the chief executive and the commander-in-chief of the armed forces. The king exercises his executive authority through the prime ministers and the Council of Ministers, or cabinet. The cabinet, meanwhile, is responsible before the elected House of Deputies which, along with the House of Notables (Senate), constitutes the legislative branch of the government. The judicial branch is an independent branch of the government.

Fractures of the earth's surface are evident in the great geological rift that extends southward from the Jordan Valley through the Gulf of Aqaba and the Red Sea, gradually disappearing south of the lake country of East Africa. Although an earthquake prone region, as of early 1989 no severe shocks had been recorded for several centuries.

By far the greatest part of the East Bank is desert, displaying the land forms and other features associated with great aridity. Most of this land is part of the great Syrian (or North Arabian) Desert (see fig. 4). There are broad expanses of sand and dunes, particularly in the south and southeast, together with salt flats. Occasional jumbles of sandstone hills or low mountains support only meager and stunted vegetation that thrives for a short period after the scanty winter rains. These areas support little life and are the least populated regions of Jordan.

The drainage network is coarse and incised. In many areas the relief provides no eventual outlet to the sea, so that sedimentary deposits accumulate in basins where moisture evaporates or is absorbed in the ground. Toward the depression in the western part of the East Bank, the desert rises gradually into the Jordanian Highlands--a steppe country of high, deeply cut limestone plateaus with an average elevation of about 900 meters. Occasional summits in this region reach 1,200 meters in the northern part and exceed 1,700 meters in the southern part; the highest peak is Jabal Ramm at 1,754 meters (though the highest peak in all of Jordan is Jabal Umm al Dami at 1854 meters. It is located in a remote part of southern Jordan). These highlands are an area of long-settled villages. Until about the 1940s, persons living in these villages depended upon rain-fed agriculture for their livelihood.

The western edge of this plateau country forms an escarpment along the eastern side of the Jordan River-Dead Sea depression and its continuation south of the Dead Sea. Most of the wadis that provide drainage from the plateau country into the depression carry water only during the short season of winter rains. Sharply incised with deep, canyonlike walls, whether wet or dry the wadis can be formidable obstacles to travel.

The Jordan River is short, but from its mountain headwaters (approximately 160 kilometers north of the river's mouth at the Dead Sea) the riverbed drops from an elevation of about 3,000 meters above sea level to more than 400 meters below sea level. Before reaching Jordanian territory the river forms Lake Tiberias, the surface of which is 212 meters below sea level. The Jordan River's principal tributary is the Yarmuk River. Near the junction of the two rivers, the Yarmuk forms the boundary between Israel on the northwest, Syria on the northeast, and Jordan on the south. The Az Zarqa River, the second main tributary of the Jordan River, rises and empties entirely within the East Bank.

A 380-kilometer-long rift valley runs from the Yarmuk River in the north to Al Aqabah in the south. The northern part, from the Yarmuk River to the Dead Sea, is commonly known as the Jordan Valley. It is divided into eastern and western parts by the Jordan River. Bordered by a steep escarpment on both the eastern and the western side, the valley reaches a maximum width of twenty-two kilometers at some points. The valley is properly known as the Al Ghawr (the depression, or valley, also seen as Al Ghor).

The rift valley on the southern side of the Dead Sea is known as the Southern Ghawr and the Wadi al Jayb (popularly known as the Wadi al Arabah). The Southern Ghawr runs from Wadi al Hammah, on the south side of the Dead Sea, to Ghawr Faya, about twenty-five kilometers south of the Dead Sea. Wadi al Jayb is 180 kilometers long, from the southern shore of the Dead Sea to Al Aqabah in the south. The valley floor varies in level. In the south, it reaches its lowest level at the Dead Sea (more than 400 meters below sea level), rising in the north to just above sea level. Evaporation from the sea is extreme due to year-round high temperatures. The water contains about 250 grams of dissolved salts per liter at the surface and reaches the saturation point at 110 meters.

The Jordan Rift Valley (Arabic: Al-Ghor or Al-Ghawr) is an elongated depression located in modern-day Israel, Jordan, the West Bank and the Golan Heights. This geographic region includes the Jordan River, Hula Valley, Lake Tiberias and the Dead Sea, the lowest land elevation on Earth.

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Hotels in Jordan

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