The Semien Mountains are the highest parts of the Ethiopian Plateau (more North Part Of Ethiopia than 2,000 meters; or 6,560 feet). They are surrounded by a steep, ragged escarpment (step), with dramatic vertical cliffs, pinnacles, and rock spires. Included in the range is the highest point in Ethiopia, Ras Dashen at 4,533 meters (14,926 feet).
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Lalibela Church Ethiopia https://www.facebook.com/ethiotravelandtours?__tn__=-]K*F The rock-hewn churches at Lalibela are made through a subtractive processes in which space is created by removing material. Out of the 11 churches, 4 are free-standing (monolithic) and 7 share a wall with the mountain out of which Lalibela Ethiopia they are carved. The churches are each unique, giving the site an architectural diversity that is evident by the human figures of bas-reliefs inside Bet Golgotha, and the colorful paintings of geometrical designs and biblical scenes in Bet Mariam.[3]
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Danakil Depression desert Ethiopia
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North East Part Of Ethiopia 🇪🇹 Danakil Depression
Embedded in the horn of Africa is a region called the Afar Triangle. It's kilometers from any settlements and seems to offer little in the way of hospitality. Geologically, however, it's a scientific treasure trove. This desolate, desert region is the home of the Danakil Depression, a place that seems more alien than Earth-like. It's the hottest place on Earth and during the summer months, temperatures can get up to a high of 55 degrees Celsius (131 degrees Fahrenheit) thanks to geothermal heat caused by volcanic activity.
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The bull jumping event involves running across the backs of seven to ten castrated bulls multiple times without falling. It is an important ritual for the Hamer tribe and essentially qualifies young men for marriage, raising children
The “Portuguese Bridge” bridge, was not as it’s name suggests built by the Portuguese but was in fact built in the 19th century by an Portugal , called Ras Dargein. It as built in the style of the 17th century bridges around the Nile. The view in this area is simply breathtaking, with a waterfall and a deep gorge leading down to the Jemma River valley. It is also a habitat of several rare birds (lammergeyer, Abyssinian ground hornbill, endemic banded barbet, Abyssinian woodpecker and much more) and endemic Gelada baboons.
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The Bale Mountains (also known as the Urgoma Mountains) are mountain ranges in the Oromia Region of southeast Ethiopia, south of the Awash River, part of the Ethiopian Highlands. They include Tullu Demtu, the second-highest mountain in Ethiopia (4377 meters), and Mount Batu (4307 meters). The Weyib River, a tributary of the Jubba River, rises in these mountains east of Goba. The Bale Mountains National Park covers 2,200 square kilometers of these mountains. The park's main attractions are the wild alpine scenery and the relative ease with which visitors can see unique birds and mammals.
The Simien Mountains National Park in Northern Ethiopia is an exotic setting with unique wildlife and breath-taking views on a landscape shaped by nature and traditional agriculture. The natural beauties of this region have always filled visitors from Ethiopia and abroad with awe. Gentle highland ridges at altitudes above 3600 meters above sea level (m asl), covered with grasses, isolated trees (Erica &bored) and the bizarre Giant Lobelia (Lobelia rhynchopetalum) are found on the high plateau that ends abruptly at 1000- to 2000-m deep escarpments.
The margins of this high plateau consist of precipitous cliffs and deep, canyon-style gorges. In some places, the escarpment forms small elevations that offer splendid natal lookout points. The spectacular views from the observation points at Gidir Got and lmet Gogo in the center of the Park offer unparalleled panoramas along the high plateau and down to the lowland areas. Given the right meteorological conditions, views reaching up to a hundred kilometers over the valleys and the terraces of the Tekeze lowland basin are no exception. Geologically speaking, the entire highlands of the Simien mountains consist of dark Trapp basalt and bright, soft turf. They alternate and constitute a massive complex that is more than 3000 m thick. This complex was formed by volcanic eruptions in the Tertiary Oligocene-Miocene Age some 20-30 million years ago; ever since, it has been going through processes of uplifting and erosion.
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