The Red Sea:

To anyone standing on its shore and gazing out across its heavenly waters, the Red Sea may seem to be a mislabeling. Its blueness is eternal and anything less red cannot be fantasized. The Red Sea, where the desert meets the ocean, is truly one of the planet’s most exotic and fascinating natural seascape environments. The Red Sea is located between Asia and Africa. At its most northerly point forms the Sinai Peninsula and stretches over 1000 miles south to join the Indian Ocean, between Ethiopia and Yemen. In the north and west are desert plains, while in the south a mountainous region (2642 meters high), which is part of the mountain range stretching from deep in Saudi Arabia, across the Sinai and then into Nubia of the African continent. The Red Sea holds beneath its crystal blue surface an oasis of living creatures, reefs, and coral formation. Its use as a highway between East and West has attracted man since the beginning of time.

The Red Sea was created by the movement of plates in the Earth’s surface about 30 million years ago. In that time, the Arab peninsula started to part from Africa along a thin break line which was filled by the ocean’s water. However, "Mother Nature" did not stop there. Twenty million years ago another geological movement started. The Arab peninsula which parted from Africa started to move to the north. That movement struck resistance in Turkey and swung to the east, and another break line was formed. This one stretching all the way from the northern part of Israel, through the Jordan valley to the Dead Sea, and finally through the Gulf of Eilat to Ras Mohamad at the southern point of the Sinai. The young age of the Gulf of Eilat is what makes it so deep, 100 meters in Dahab and 1800 meters north of the Straits of Tiran. On the other hand, the old Gulf of Suez is relatively shallow, with an 85 meters maximum depth. The Red Sea is still widening at about one-half inch per year, the rift is the youngest region of continental breakup on the planet, allowing geologists to learn about processes that occurred in the Atlantic and Pacific oceans hundreds of millions of years earlier.