The Birket Qarun lake, also known by its ancient name, Lake Moeris, Wadi El Hitan, and Wadi El-Rayan.
2 Days
8
A private car/minibus
Wadi Rayan and Wadi Hitan with an overnight stay under the starry sky in the Western Desert.
is an ancient lake in the northwest of the Fayum Oasis, 80 km southwest of Cairo,
In prehistoric times, Egypt was home to a freshwater lake, estimated to have had a surface area ranging from 1,270 km² to 1,700 km².
And It continues to exist today as a smaller saltwater lake called Birket Qarun.
The lake and surrounding area is a protected area and has been designated a Ramsar site since 2012. It is a source for tilapia and other fish from the area.
The prehistoric mammal Moeritherium was found in this area. When the Mediterranean Sea became a hot,
dry cavity was towards the end of the messianic salinity crisis in the late Miocene,
During that time, Faiyum was a dry basin, and the Nile River flowed along its bottom through a gorge estimated to be 2,400 meters deep or deeper, where Cairo is located today.
Wadi El-Hitan is located in the Wadi El Rayan Reserve, which spans an area of 1,759 square kilometers in the Fayoum Governorate.
It is located at a distance of 150 kilometers from Cairo, Egypt.
In the whale valley, 10 complete whale structures were discovered, which had inhabited that region approximately 40 million years ago.
as they were part of a great ocean encompassing North Africa.
And that’s not all, also sea turtles, sawfish, and crabs.
And these are the most active places of the ecosystems and there was plenty of food and shelter for the smaller animals.
But fossilized mangrove roots have also been found here. That means that here in this part of the sea it was an offshore line.
To make it easier for them and so that they could move more effectively in the water
but changes to the skeleton have also occurred under water.
This is clearly visible in fossils, especially of Basilosaurus-Isis. He was busy with this development.
Wadie Rayn The Wadi El-Rayan valley is an area of 1759 km2 of which 113 km2 is the dominant water body
of the Wadi El Rayan Lakes.
And It is located about 65 km southwest of Fayum City and 80 km west of the Nile River.
The Wadi Rayan has been utilized for the creation of artificial lakes from agricultural waste, resulting in the establishment of a reserve comprising the two separate Wadi El Rayan lakes.
The reserve consists of a 50.90 km2.
And higher lake and a 62.00 km2 lower lake.
And with waterfalls between the two Among the springs are three sulfur springs on the south side of the lower lake, with extensive sand dunes.
Gabal Manqueer Al Rayan, situated in the south and southeast of the springs, harbors marine fossils and archaeological remnants. These significant remains can be discovered in the vicinity of the renowned Wadie Rayn waterfalls, which hold the distinction of being the largest waterfalls in Egypt.
Gabal Madwera, located near the lower lake, is notable for its vast expanse of dune formations. The vegetation in this area comprises a diverse array of 13 species of perennial plants, along with a few specimens of Calligonum comosum and Zygophyllum album.
Tickets to the monuments for children
– Children up to 6 years old free.
– Children from 6 to 12 years of age pay from 50%
All prices are subject to change.
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Lake Moeris is an ancient lake located in the northwest of the Fayum Oasis, 80 km southwest of Cairo, Egypt. In prehistory, it was a freshwater lake, with an estimated surface area of 1,270 km² to 1,700 km². It persists today as a smaller saltwater lake called Birket Qarun. The surface of the lake is 43 meters below sea level and covers approximately 202 square kilometers The lake and its surrounding area are a protected area and have been designated as a Ramsar site since 2012. It is a source of tilapia and other local fish species. In this area, the prehistoric mammal Moeritherium was found. When the Mediterranean Sea was a hot, dry basin towards the end of the Messinian salinity crisis in the late Miocene, Faiyum was a dry basin and the Nile flowed through it at the bottom of a canyon 2400 meters deep or more, where Cairo now stands. After the Mediterranean Sea became inundated at the end of the Miocene, the Nile canyon became a sea arm that extended further inland than Aswan. Over the course of geological time, that sea arm gradually filled with silt and became the Nile Valley. Eventually, the bed of the Nile Valley became sufficiently silted up to allow the overflowing Nile to inundate the Fayum basin, creating a lake. The lake was first recorded around 3000 BCE, around the time of King Narmer, but for the most part, it would only be filled during high water. The lake was bordered by Neolithic settlements, and the city of Shedet grew up in the south, where higher ground created a ridge.
In 2300 BCE, the waterway from the Nile to the natural lake was widened and deepened to create a canal now known as the Bahr Yussef.
This project was initiated by Amenemhat III. This canal emptied into the lake. This was intended to serve three purposes: controlling the floods of the Nile, regulating the water level of the Nile during dry seasons, and providing irrigation to the surrounding area. There is evidence that ancient Egyptian pharaohs of the twelfth dynasty used the natural lake of Fayum as a reservoir to store excess water for use during dry periods. Near the lake are the remains of the oldest known paved road in the world, the Lake Moeris Quarry Road, which helped transport basalt blocks from a nearby quarry to the lake, from where they could be shipped to the Giza Necropolis. The American Society of Civil Engineers has included it in the list of historic landmarks for civil engineering. The immense hydraulic works undertaken by the ancient Egyptian pharaohs of the twelfth dynasty to transform the lake into a vast water reservoir gave the impression that the lake was an artificial excavation, as described by geographers and travelers in classical antiquity. The lake was eventually abandoned because the nearest branch of the Nile diverted from it around 230 BCE. Shrunk. The name Moeris is a Greek version of the Egyptian mer-wer, meaning 'great canal'. Amenemhat III, who initiated this project, was also known as Moeris. In ancient Egypt, the lake was also alternatively referred to as 'the lake,' 'pure lake,' and 'Osiris' lake. During the Middle Kingdom, the entire area around the lake was often referred to as Mer-wer as well. Similarly, the Late Egyptian word Piom, meaning 'sea,' originally limited to the Moeris Lake, was used to refer to the city of Crocodilopolis, which is still the capital of Fayum but is now called Al-Fayum.
Wadi El-Hitan is located in the Wadi El Rayan Reserve, covering an area of 1759 square kilometers in the Fayum Governorate, at a distance of 150 km from Cairo, Egypt. In the Whale Valley, 10 complete whale structures were found, which lived in that region approximately 40 million years ago, as they were part of a vast ocean that encompassed North Africa. In 2005, Wadi El-Hitan was designated as a UNESCO World Heritage Site and was chosen by UNESCO as one of the best archaeological sites in the ancient world for whale fossils. Wadi El-Hitan is so special because over 400 skeletons of whales and sea cows have been found here. And that's not all, also sea turtles, sawfish, and crabs. These were the most active sites of the ecosystems, and there was plenty of food and protective spaces for the smaller animals here. Likely, the whales came here because there was so much food available. But it's also possible that the wind drove the whales here. But likely, many ended up in the lagoons and got trapped among the roots of the mangrove trees. But many also died a natural death from old age or illness. When a whale dies, it sinks to the bottom of the sea where it rolls around completely, likely due to its very strong back muscles. Buiten Egypte is er nog één plaats waar deze voorheen vierpotige walvissen veranderd zijn in zeedieren dat is in Pakistan. But in Egypt, it's the only place where you can actually see this evolution. You can still see it well in the skeletons. 55 million years ago, there was a massive global warming, and animals were forced to move to other places for their food and water. So, many species started living at the water's edge. Over time, they adapted to the new conditions, and started eating fish and other food from the sea. But here, petrified mangrove roots have also been found. That means that this part of the sea was an offshore area. To make it easier for them and so that they could move more effectively in the water, both on the surface and underwater, changes to the skeleton occurred. This is clearly visible in fossils, especially of Basilosaurus-Isis. He was busy with this development. He was the first whale with fully developed fins. But the memory of his former country life was still clearly visible. The toes, ankles, kneecaps, bones and lower bones were still clearly visible. In a skeleton of an 18 meter long whale, the legs were less than a meter long, which is far too short to carry the animal that weighed tons, let alone walk. The skulls of the Basiliosauris skeletons also clearly showed that they were completely ready for life under water. Skeletons of Basilosauris, Basilosauris-Isis, Durodon, and Protectus have been found here in the Wadi el Hitan.
The Wadi El-Rayan Valley is an area of 1759 km2 of which 113 km2 is the dominant water body of the Wadi El Rayan Lakes. It is located approximately 65 km southwest of Fayum City and 80 km west of the Nile River. The Wadi has been used for artificial lakes from agricultural waste, which has created a reserve of the two separate Wadi El Rayan lakes. The reserve consists of a 50.90 km2 upper lake and a 62.00 km2 lower lake, with waterfalls between the two. Among the springs are three sulfur springs on the south side of the lower lake, with extensive sand dunes. The Wadi El Rayan waterfalls are considered the largest waterfalls in Egypt. In the south and southeast of the springs is Gabal Manqueer Al Rayan, where marine fossils and archaeological remains can be found. Gabal Madwera, near the lower lake, is known for its extensive dune formations. The vegetation consists of 13 species of perennial plants and a few specimens of Calligonum comosum and Zygophyllum album. Wadi El Rayan is home to one of the world's few remaining populations of the endangered slender-horned gazelle The Dorcas gazelle is still found in small numbers in the area, while both the fennec fox and Rüppell's fox are scarce. There are 11 species of reptiles, 9 species of mammals, 13 species of native birds, and 26 species of migratory and wandering birds. The entire excursion day will be accompanied by employees of Egypte4allreizen (Dutch, Italian, or English-speaking guides).
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Min - Max (Persons) | Adult Price | Children Price |
---|---|---|
1 - 1 | €530.00 | €265.00 |
2 - 2 | €430.00 | €215.00 |
3 - 8 | €360.00 | €180.00 |
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