The Sinai Peninsula, with
a surface area of 61.000 km2 (200 km E –W, 380 km N-S), connects
the two continents Africa and Asia . It is surrounded on 3 sides
by sea. On the North the Mediterranean Sea, on the East the Gulf
of Aqaba, on the West the Gulf of Suez and the Suez Channel.
|
History
Because of its position
the Sinai has since early times been a transit corridor between
Egypt and Palestine and between the Empires of Africa and Asia .
It was the route for Islamic pilgrims to Mecca, the trade route
between Africa and Asia, and also a route for Crusaders. The most
important route was the Via Maris, following the Mediterranean coastline.
Along this route many archaeological finds have been made. The pilgrims
to Mecca used a different route: the Darb el Hagg, which is now
the road from Taba to Suez. |
Of course the Sinai wasn't only a
thorough way. From the Stone Age people were living in the Sinai.
Remnants have been found of an ancient nomadic people (called the
Timna), Nabateans (whose capital was Petra in Jordan ), and Etruscans.
In Pharaonic times the Sinai was of importance due to copper and
turquoise mining. The Exodus, most probably having taken place during
the reign of Ramsis II or Merenptah (1298 – 1230 BC) was to place
Sinai on the map for pilgrims of the 3 religions (Muslims, Jews,
Christians), but mainly for Christians. Many settled down in the
area of St. Katherine and Feran for longer or shorter period.
|
Geology
Geologically Sinai is a
young formation of the earth's crust. 40 million years ago (late
Eocene) an enormous fault movement formed the great African Rift
Valley and the Red Sea with its 2 gulfs. The peninsula became separated
from the Arab o-Nubian massif. The peninsula is a tilted plate in
the earth's crust that slopes downward to the North and is uplifted
in the South. A drive across the Sinai is a journey through its
geological history (from 1 billion years to the present):
|
 |
In the south erosion
uncovers ancient formations. The high mountain area shows the oldest
history on earth for erosion has exposed the roots of the mountain:
Precambrian rocks rose as melted magma 1000 million years ago.
Further to the north, quaternary
sandstone formations are broken up by numerous outcroppings of limestone
from the Tertiary and Eocene period, which also makes up the Tih
Plateau.
Along the Mediterranean
coast the landscape consists mostly of sand dunes and quaternary
deposits (ancient riverbeds and fossil beaches formed by the changing
sea level during the glacial and interglacial periods). North western
winds have driven sand from the Sahara across the Mediterranean
Sea thus forming sand dunes 25-50 km wide. |
People and Environment
Sinai's real desert inhabitants
are the Bedouins who wander through the desert as nomads or semi-nomads.
The term Bedouin is not a name for a specific people but characterises
a way of life, the Arabic word Bedawi means desert inhabitant. Nowadays,
Bedouins are not the only inhabitants of the Sinai. Mainy due to
tourism more and more non-bedouins come to work and live in the
Sinai. Under the increasing influence of foreign neighbours and
tourism most of the Bedouins give up the traditional way of life.
|
|
Bedouins were originally
camel breeders and nomads. The Bedouins were well adapted to desert
life, knowing where to find water in which period of time, which
plants are edible, have medicinal purposes, are poisonous or are
intoxicating and where these plants can be found.
But due to influences from
outside Bedouin life is changing and they are not as much one with
the desert. |
Water can be bought,
pick-up trucks are exchanged for camels, and camels are only used
for tourist treks. Also the knowledge of plants and their use disappears.
Tourism has become one of the important means of living for many
Bedouins. What the Bedouins have kept is the craving for freedom
and independency.
Bedouins are divided into
tribes according to their different origins, but all claiming to
go back to the 12 sons of Ishmael, the son of Abraham. An exception
is the Jabaliya tribe from the St Katherine area. Their ancestors
were brought to the Sinai by Emperor Justinian in the 6th Century
from Romania and Alexandria to build and protect the Monastery.
At present there are 6
tribes in South Sinai , each claiming a certain area.
|
Flora & Fauna
Soil and Climate determine
the occurrence and spread of plant & animal species. In total
there are approximately 900 plant species in the Sinai, including
34 endemic species found only in the Sinai. |
The small number
of species is a direct consequence of the harsh climate of the
Sinai: minimal rainfall, high day temperatures, extreme variation
between day and night temperatures, strong winds. The plants
consequently have large root systems ( some up to 35 m or more),
small thick leaves to minimize evaporation, water storage systems
(many plants are shaped to collect sand, building there own
little sand dunes).
Observation of flora
and fauna make clear that the Sinai is a genuine land bridge
between Africa and Eurasia . Here plant species from 4 major
neighbouring regions mix. Most belong to the Sahara-Arabian
region. From Africa comes for example the acacia and caper bush.
Only a few species from the Mediterranean are found.
|
|
The Sinai has an interesting
mixture of fauna:
From the Palearctic region:
wolves, foxes, ibexes, dormice, partridges and rock doves
From tropical Africa :
grackle, bulbul, sun bird, rock hyrax and in former times the ostrich.
Leopards, only recently extinct as well as hyenas and jackals crossed
the land bridge to Asia. |
Marine Life
Like every living thing
coral makes demands on its environment and if one major condition
is not met it will not be able to survive.
Warm, clear, sun flooded,
nutrient poor seawater (water temp. not less than 18 - 20 º
C), and a hard seabed are some of these conditions for coral life.
|
| In the Red Sea and the Gulf of Aqaba
these conditions are met. A deep rift ( dept 1800 m) split the old
basement complex in the Red Sea and the Gulf of Aqaba , creating a
hard bottom surface for corals. In the Gulf of Suez on the other hand
the sea is shallow (max. dept 80 m) and sand covers any young coral
growth. |
|
Coral reefs constitute
of the richest eco-systems on earth. But like elsewhere the coral
reefs along the coast of the Sinai are being threatened.
Climate change, a growing
tourist industry (and thus a growing pressure of recreational diving
and a growing influx of nutrient rich sewage water) and over-fishing
along and on the reef: All these factors together give the reef
little time to recuperate. Don't forget that coral grows only a
few centimetres a year!
|
Climate
The Sinai is a desert environment
therefore there is little rainfall throughout the year. Most rain
falls inland in the winter and spring months. The air humidity is
low, so even the extreme heat in the summer is bearable. Along the
coast, mainly in Dahab and El Tor there is on most days a cool breeze
from the sea. In Sharm el Sheikh the wind usually comes from overland,
bringing a warm desert wind. |
St Katherine high mountain
region:
- Best in spring and autumn;
- Summer is hot but bearable,
the evenings are cool
- Winter is very cold, especially
at night
|
Tips
for travelers:
Inland desert:
-
Best in
spring, autumn and winter (the nights can be very cold
in winter)
-
Summer
is too hot. Even the Bedouins move to the coast in the
summer
|
Coast:
- Spring, autumn and winter
perfect. The water temperature is around 19 º C in
the winter, 24 º in summer
- Summer is hot but the sea
is always nearby for a cooling dip
|
|
|
| |