Introducing the above attractions, this article tries to attract the attention of responsible persons and researchers more towards the importance and role of geotourism in this area. Attractions like semi-active volcanoes of Taftan and Bazman, standing the bulk of Iran's mud volcanoes in this area with variant beautiful shapes, huge sand dunes of Loot desert, Chabahar Bay, Miniature Mountains, Ladiz cave, Khaje Mountain and tens of other natural landscapes convert this area to one of the most unique geotourism areas in the world. Including unique geological phenomenon, this area showed novel sights of geomorphologic attractions in an accessible range. Therefore, South East of Iran (Sistan and Baluchistan Province) is selected for study because of having valuable geological heritage and lack of necessary economic development. Geological attractions and sustainable economic development are some branches of geotourism. The property represents an exceptional example of ongoing geological processes.If an area has geological attractions and necessary infrastructures prepared for tourism, geotourism can have a direct effect on sustainable development, employment and improvement of the local economy situation. The range rises 1,818 meters (6,000 feet) above sea level and. widely referred to as Dasht-e Lut, is a large salt desert located in the provinces of. The hottest place on earth is Lut desert in Iran. The image takes advantage of the Sun’s low angle to reveal linear geological structures of the Iranian mountain range bordering the western edge of the basin known as Dasht-e-Lut. 56 1.2K views 1 year ago IRAN IN 4K : LUT.
It also contains extensive stony deserts and dune fields. An International Space Station crew member took this striking photograph one evening in late February. Consequently, the site presents some of the most spectacular examples of aeolian yardang landforms (massive corrugated ridges). Between June and October, this arid subtropical area is swept by strong winds, which transport sediment and cause aeolian erosion on a colossal scale. The Lut Desert, or Dasht-e-Lut, is located in the south-east of the country. According to a local legend, the name (in translation from Persian - “Toasted wheat”) originates from an accident where a load of wheat was left in the desert which was then scorched by the heat in a few days. The hottest part of Dasht-e Lut is Gandom Beryan, a large plateau covered in dark lava, approximately 480 square kilometers (190 sq mi) in area. Precision of measurements is 0.5 K to 1 K. Measurements of MODIS (Moderate-Resolution Imaging Spectroradiometer) installed on NASA’s Aqua satellite from 2003 to 2010 testify that the hottest land surface on Earth is located in Dasht-e Lut and land surface temperatures reach here 70.7 ☌ (159.3 ☏), though the air temperature is cooler. Yardangs in Lut Desert, Kerman Province, Iran.
The southeast is a vast expanse of sand, like a Saharan erg, with dunes 300 meters (980 ft) high, among the tallest in the world. This area is also riddled with ravines and sinkholes.
#Dasht e lut iran series#
In contrast, the center has been sculpted by the wind into a series of parallel ridges and furrows, extending over 150 km (93 mi) and reaching 75 meters (246 ft) in height. The eastern part of Dasht-e Lut is a low plateau covered with salt flats. During the spring wet season, water briefly flows down from the Kerman mountains, but it soon dries up, leaving behind only rocks, sand, and salt. The other large basin is the Dasht-e Kavir. Dasht-e Lut is one of the largest of these desert basins, 480 kilometers (300 mi) long and 320 kilometers (200 mi) wide, and is considered to be one of the driest places on Earth.Īrea of the desert is about 51,800 square kilometers (20,000 sq mi). The Dasht-e Lut has an area of about 20,000 square miles and is among the largest in the vicinity. Iran’s geography consists of a plateau surrounded by mountains and divided into drainage basins. The Lut Desert is part of the Dasht dry lake basins (that are now deserts) in Iran alongside the Dasht-e Loot, Dasht-e Kavir, and other smaller ones. As a result, the desert is largely an abiotic zone. In near-tropical deserts, elevated areas capture most precipitation. The patchy, elongated, light-colored feature in the foreground (parallel to the mountain range) is the northernmost of the Dasht dry lakes that stretch southward 300 kilometers (190 mi). These winds took 120 days long during the year called Sistan’s one- hundred-and-twenty-day winds, play a major role in creating morphological structures across the lut desert (Dasht-e Lut) ( Rahnama Rad and Saheb Zade 2010), 7. Iran is climatically part of the Afro-Asian belt of deserts, which stretches from the Cape Verde islands off West Africa all the way to Mongolia near Beijing, China. Dasht-e Lut’s (lut desert) location in Iran.
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