Saudi Arabia travel entertainment .........
Saudi Arabia covers approximately four fifths of the area of the Arabian Peninsula, which can be described as a rectangular plateau gradually sloping eastwards till reaching sea level at the Persian Gulf.
Saudi Arabia covers approximately four fifths of the area of the Arabian Peninsula, which can be described as a rectangular plateau gradually sloping eastwards till reaching sea level at the Persian Gulf.
The main topographical features are as follows:

The Sarawat or Sarat mountain range runs parallel to the Red
Sea coast beginning near the Jordanian border until the southern
coast of Yemen,
gradually increasing in height southwards. It is largely made up of barren
volcanic rock, especially in the south, and sandstone in the north, but it is
also interspersed with ancient lava fields and fertile valleys. As one moves
further south towards Yemen,
the barren landscape gradually gives way to green mountains and even woodlands,
the result of being in the range of the monsoons. In Saudi
Arabia, the range is commonly known as the Hejaz,
though the southernmost part of the range is known as 'Aseer. In the foothills
of the Hejaz lies the holy city of Makkah,
and approximately 400 km north of Makkah in an oasis between two large lava
fields lies the other holy city of Madinah.
West of the Sarawat or Hejaz mountain
range is a narrow coastal plain known as Tihama, in which the country's second
largest city, Jidda, is located.
East of the Hejaz lies the elevated
plateau known as Najd, a sparsely populated area of
desert steppe dotted with small volcanic mountains. To the east of Najd-proper
lies the Tuwaig escarpment, a narrow platau running 800 kms from north to south.
Its top layer is made of limestone and bottom layer of sandstone. Historically
rich in fresh groundwater and criscrossed with numerous dry riverbeds (wadis), the
Tuwaig range and its immediate vicinity are dotted with a constellation of
towns and villages. In the middle, nestled between a group of wadis, is the
capital city, Ar-Riyadh.
Further east from the Tuwaig plataeu and parallel to it is a
narrow (20-100 km) corridor of red sand dunes known as the Dahana desert, which
separates the "Central Region" or "Najd"
from the Eastern Province.
The heavy presence of iron oxides gives the sand its distinctive red appearance.
The Dahana desert connects two large "seas" of sand dunes. The
northern one is known as the Nufuud, approximately the size of Lake
Superior, and the southern is known as "the Empty
Quarter," so-called because it covers a quarter of the area
of the Peninsula. Though essentially uninhabitable, the
edges of these three "seas of sand" make for excellent pastures in
the spring season, but even the bedouin almost never attempted to cross the Empty
Quarter.
North of the Nufud desert lies a vaste desert steppe, traditionally
populated mainly by nomadic bedouins with the exception of a few oasis such as
Al-Jof. This region is an extension of the Iraqi and Syrian deserts (or vice
versa). After a rainy season, these barren, rocky steppes can yield lush
meadows and rich pastures.
The eastern province is largely barren except that it
contains two oases resulting from springs of ancient fossil water. These are
the oases of Al-Qateef on the Gulf coast and Al-
Hasa (or Al-Ahsa) further inland. Next to Qatif lies the
modern metropolitan area of Dammam, Dhahran and Al-Khobar


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