No other place in the world yields the number, concentration and quality of such fossils, nor their accessibility and setting in an attractive and protected landscape.[5] The valley was therefore inscribed on theUNESCOWorld Heritage List in 2005.[2]
The fossils found at the site may not be the oldest but their great concentration in the area and the degree of their preservation is such that even some stomach contents are intact. The presence of fossils of other early animals such as sharks, crocodiles, sawfish, turtles and rays found at Wādī al-Ḥītān makes it possible to reconstruct the surrounding environmental and ecological conditions of the time, adding to its justification to be cited as a Heritage site.[6]
The first fossil skeletons of whales were discovered in the winter of 1902–03.[1] For the next 80 years they attracted relatively little interest, largely due to the difficulty of reaching the area. In the 1980s interest in the site resumed as four wheel drive vehicles became more readily available. Continuing interest coincided with the site being visited by fossil collectors, and many bones were removed, prompting calls for the site to be conserved.
The remains display the typical streamlined body form of modern whales, yet retaining some of the primitive aspects of skull and tooth structure. The largest skeleton found reached up to 21 m in length,[7] with well-developed five-fingered flippers on the forelimbs and the unexpected presence of hind legs, feet, and toes, not known previously in anyarchaeoceti. Their form was serpentine and they were carnivorous. A few of these skeletal remains are exposed but most are shallowly buried in sediments, slowly uncovered by erosion. Wādī al-Ḥītān provides evidences of millions of years of coastal marine life.[6]
Skeletons of basilosaurid whales likeDorudon (featured above) were discovered at the site
Wādī al-Ḥītān is the most important site in the world to demonstrate one of the iconic changes that make up the record of life on Earth: the evolution of the whales. It portrays vividly their form and mode of life during their transition from land animals to a marine existence. It exceeds the values of other comparable sites in terms of the number, concentration and quality of its fossils, and their accessibility and setting in an attractive and protected landscape. Iconic assemblage of fossilized skeletons of Archaeoceti (primitive whales documenting cetacean transition to marine life), sirenians and reptiles, as well as shark teeth from Gehannam Formation (40–41 million years ago).[8] The strata in Wādī al-Ḥītān belongs to MiddleEocene epoch and it contains extensive vertebrate fossils within a 200 km2 (77 sq mi) area. Fossils are present in high numbers and often show excellent quality of preservation. The most conspicuous fossils are the skeletons and bones of whales and sea cows, and over several hundred fossils of these have been documented.[9] Wādī al-Ḥītān (Whale Valley) is unusual in having such a large concentration of fossil whales (1500 marine vertebrate fossil skeletons) in a relatively small area.
The fossils of whales vary from single bones to entire skeletons, and a number of partial skeletons are currently on display in the public part of the park. The two common whales are the largeBasilosaurus, and the smaller (3- to 5-metre)Dorudon.[10] At least two other species are known from rarer remains. The whales possess small hind limbs, that are not seen in modern whales, and a powerful skull with teeth similar to those of carnivorous land mammals.[9]Other mammals are represented by the skeletons of three species ofsirenia or sea cows. These were fully marine like the whales, and likewise show primitive features not seen in modern species and possess teeth that suggest that they grazed on seagrasses and other marine plants.[11] Bones of the primitive elephantMoeritherium have also been recorded.[12]
Fossil reptiles are represented by fossils of crocodiles and sea turtles, and bones of sea snakes have also been recorded. There are many species of bony fish, sharks and rays represented, but most of the fossils are isolated small teeth and these are not often conspicuous. Larger fish fossils include the rostra and pegs ofsawfish; a sawfish rostrum of 1.8 metres long is laid out in the park. Fossil shells are not common in the main whale-bearing rocks, but are very common in other rocks; many fallen rocks can be seen to be full of a wide variety of fossil shells. Disc-shapednummulite fossils are common in places, and often coat the desert floor.A large log is present in the park, and this is full of tubularshipworm fossils. Some fossil seagrasses are also known.[citation needed]
The oldest fossil yet discovered of apelican (dating from the lateEocene) was identified at Wādī al-Ḥītān in 2021.[13]
Eroded stratified sandstone bodies from Wādī al-Ḥītān
The geology of the valley gives rise to the scenery, with wind and water erosion producing spectacular cliffs and buttes.The rocks present at Wādī al-Ḥītān are allMiddle toLate Eocene in age and is composed of three main rock units. TheGehannam Formation comprises open marine mudstones, which are largely present on the flatter ground to the east of the public park. The rock unit that contains most of the whale fossils is theBirket Qarun Formation. This comprises yellowish open marine sandstones that form most of the cliffs and buttes.[6]
The monotony of these sandstones is broken by a white layer full of well-preserved animal burrows (previously thought to be mangrove roots) and a layer of black mudstone above that.[10] When the cliffs of the Birket Qarun Formation are followed to the East, they are replaced by Gehannam Formation mudstones, indicating a change in water depth from shallower to deeper in that direction.[6] The tops of the higher cliffs are within theQasr el Sagha Formation, which comprises dark mudstones alternating with limestones full of shells and represents a lagoonal environment.[6]
Only about 1,000 visitors a year drive into Wādī al-Ḥītān by 4WD because the track is unpaved and crosses unmarked desert sands. For the most part, visitors to Wādī al-Ḥītān are foreigners, who usually camp in the valley on winter weekends. Because Wādī al-Ḥītān is within theWadi El Rayan Protected Area, the same protection management plan restricts visitors to prearranged guided tours along a prescribed trail.Sustainable tourism is beginning to develop and grow in the area, and the 4WD are alternatively being replaced by foot or camel treks.[7]
Since part of Wādī al-Ḥītān was made into a tourist venue, walkways between the main fossils have been laid out and small shelters built. This public park is now regularly visited by tourist groups, and a small camp site is present.
The valley is located behind a mountain known asGaretGohannam "the Mountain of Hell". In the light of the setting sun, the mountain seems ablaze with an eerie red light.[14]
The Egyptian government said that in July 2007 a pair ofcars driven byBelgiandiplomats entered a protected zone in this area and destroyed part of the whale fossil, causing 10 millionUS dollars' worth of damage. The Belgian government alleges no damage was caused by its diplomats.[15] The issue remains unresolved.
^ab"Wadi Al-Hitan (Whale Valley)".UNESCO World Heritage Centre. United Nations Educational, Scientific, and Cultural Organization. Retrieved20 July 2006.
^Mahdy, A.; El-Kheir, G. Abu; Gohar, Abdullah S.; El-Soughier, Maher I. (4 March 2021). "Palaeobiological assessment of some basilosauridarchaeocetes (mammalia, cetacea) and its affinity with recent odontocetes: new insights from Wadi El-Hitan, Fayoum, Egypt".Historical Biology.33 (3):313–322.Bibcode:2021HBio...33..313M.doi:10.1080/08912963.2019.1616292.ISSN0891-2963.S2CID181399367.
^Gingerich, P. D.; Domning, D. P.; Blane, C. E.; Uhen, M. D. (1994). "Late Eocene sea cows (Mammalia, Sirenia) from Wadi Al Hitan in the Fayum Basin, Egypt".Contributions from the Museum of Paleontology.29 (2). University of Michigan:41–67.
^El Adli, Joseph J.; Wilson Mantilla, Jeffrey A.; Antar, Mohammed Sameh M.; Gingerich, Philip D. (2 June 2021). "The earliest recorded fossil pelican, recovered from the late Eocene of Wadi Al-Hitan, Egypt".Journal of Vertebrate Paleontology.41 (1): e1903910.Bibcode:2021JVPal..41E3910E.doi:10.1080/02724634.2021.1903910.S2CID236269386.