Wadi Al-Hitan (Whale Valley)

Wadi Al-Hitan

Location: 150 km South-west of Cairo Map

 

Description of Wadi Al- Hitan

Wadi Al- Hitan or a Whale Valley ( وادي الحيتان) is situated some 150 km South West of Cairo. It is famous fo numerous fossils of ancient whales that are found here. Wadi Al- Hitan or Valley of the Whales is famous for full skeletons of whales that once swam here then this part of Africa was submerged under the sea. Evolution of a land based animal to a marine mammal is easily traceable by the fossils that are spread all around the region. It is no surprise that this part of Egyptian desert is named UNESCO World Heritage Site. Its isolation from most of human settlement gave chance to scientists discover and describe many whale species of Archaeocetes suborder. Known to palaeontologists as Dorudon Atrox, this ancient ancestor of modern whales is commonly found in the area. While its body shows characteristics of a marine animal, it still keeps its rudimentary hind limbs as well as skull and tooth design of a land animal.

 

Geology

Around 40 million years ago, during the Eocene, the Tethys Ocean was located here for around two million years. Then tectonic forces raised the terrain and the sea was pushed back. The remains of the sea creatures were embedded in sediments.

Today you can discover the fossilized skeletons of primitive whales, shark teeth, shells and corals as well as other traces of past marine life in the eight square kilometer area. Fossilized mangrove roots from that era can also be found. These finds allow a reconstruction of the paleoecology, i.e. the living conditions of that time.

The whale skeletons are of particular interest - a total of 250 specimens have been discovered so far. These are remains of the genera Basilosaurus (“king lizard”) and Dorudon atrox. The first bones of Basilosaurus were found in the USA in 1830 and were mistakenly thought to be the remains of a reptile. However, the English anatomist Richard Owen recognized that it was a mammal and suggested renaming it tozeuglodon (“yoke tooth”). But according to the principle of priority, the older name applies, although “Zeuglodon” remained a frequently used synonym. The Wadi al-Hitan is therefore also called “Wadizeuglodon”.

These fossils can be used to prove the origin of whales from land animals. The fossils still have remnants of the hind legs, but they already have the streamlined shape that is adapted to aquatic life.

Around a dozen of the best locations for finding whale spines are marked and secured by ropes to the left and right of the marked path. Other bones are buried under mounds of earth or rubble, so you should neither climb nor drive over these piles.

 

Fossils

In the valley, among the fossils that emerged from the erosion of the sandstones formed from the ancient seabed, over 500 skeletons of archaeocetes, complete or partial, have been documented and three different species of these ancient cetaceans have been identified.

The largest specimen is a Basilosaurus isis 21 meters long, a carnivorous cetacean with serrated teeth, hind limbs equipped with fingers and a tapered body like modern whales. The remains of these hidden limbs testify to the evolution of cetaceans from terrestrial to marine life forms. During the 2015 excavation campaign, the first and only known complete skeleton of Basilosaurus isis was found, 18 meters long, thanks to which it was possible to observe for the first time the tail equipped with spines (as in a thagomizer). Inside the specimen still preserved, in correspondence with the stomach, the remains of the last meal: crabs, sawfish and a small cetacean. Next to the skeleton, the presence of numerous shark teeth testifies to how the carcass was partially devoured after death and reflects the abundance of these species at the time.

Numerous skeletons of Dorudon atrox were also found, archaeocetes up to 5 meters long, half of which were very young, which suggests that the area represented a usual place for the birth of young, favored by the shallow waters located along the southern coasts of the Tethys Ocean. Some skulls of Dorudon atrox hatchlings show bite marks from a large predator, probably Basilosaurus isis.

A third species of archaeocete is represented by the Ancalecetus simonsi, of comparable size to the Dorudon atrox, of which only a partial skeleton has been found.

The presence of fossil finds of other marine animals including three primitive species of sirenids, remains of Moeritherium, an ancestor of the elephant, crocodiles, sharks, sawfish, rays, bony fish, turtles and sea snakes, allows us to reconstruct the ecological and environmental conditions of the area at the time of the evolution of the archaeocetes.

The fossils also include numerous invertebrates: nummulites, molluscs, gastropods, echinoids, bivalves and crabs.

 

Tourism

There are only 1,000 visitors a year who travel to Wādī al-Ḥītān by 4WD as the track is not asphalted and crosses desert sands. For the most part, visitors to Wādī al-Ḥītān are foreigners who usually frequent the valley during winter weekends. Because Wādī al-Ḥītān is within the Wādī al-Rayān protected area, the site's conservation program funnels visitors along a prescribed route. Sustainable tourism is starting to develop and grow in the area, while visits on board four-wheel drive vehicles are alternatively replaced by walks on foot or on dromedaries.

Since part of Wādī al-Ḥītān has been transformed into a tourist site, some walkways have been placed to connect the places where the main fossils are found and small shelters have also been built. This public park is now regularly visited by tourist groups and there is also a small campsite.

The valley lies behind a mountain, known as Qārat Gahannam (Arabic قارة)‎?, Qārat) means "hill" or "mountain" and Gahannam, Arabic ﺟﻬﻨﻢ‎?, means "hell", so Qārat Gahannam means " mountain of hell". In the light of the sunset, the mountain seems to be ablaze with a frightening red light.

The Egyptian government said that in July 2007 two cars driven by Belgian diplomats entered a protected zone in this sector and this caused US$10 million in damage to the fossils. The Belgian government declared, however, that no damage was caused by its diplomats. The problem still remains unsolved.