Iran (Persian: ایران Irān [ʔiːˈɾɒːn] ( listen)), also known as Persia (/ˈpɜːrʒə/), officially the Islamic Republic of Iran (Persian: جمهوری اسلامی ایران Jomhuri-ye Eslāmi-ye Irān ( listen)), is a sovereign state in Western Asia. With over 81 million inhabitants, Iran is the world's 18th-most-populous country. Comprising a land area of 1,648,195 km (636,372 sq mi), it is the second-largest country in the Middle East and the 17th-largest in the world. Iran is bordered to the northwest by Armenia and the Republic of Azerbaijan, to the north by the Caspian Sea, to the northeast by Turkmenistan, to the east by Afghanistan and Pakistan, to the south by the Persian Gulf and the Gulf of Oman, and to the west by Turkey and Iraq. The country's central location in Eurasia and Western Asia, and its proximity to the Strait of Hormuz, give it geostrategic importance. Tehran is the country's capital and largest city, as well as its leading economic and cultural center.
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near Kazerun there are some bath relief and a nice temple and in the peak of the mountain a big sculpture. this city has many stories. near Kazerun also there are some nomads that you can experience their simple life for one night. if you like hiking mountain, historical and cultural place don't miss it. If you need more information you can text this number: +989355190268
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Kutalokhor Cave is a dry-water cave located in Zanjan province, Khodabandeh, 80 km south of Khedar and 173 km north of Hamadan, 410 km from Tehran and 5 km from Garmab small town. In some parts of western Iran, it is said to be low-lying mountains, and it is likely that the cave sign is due to the fact that the cave is located in one of these mountains and that the sun rises from behind and instead of the sun it is called " The Kataleh Khor Cave was discovered before the year 1300 and was registered in 1330 by a person named Jamali Zanjani. Around the year 1343, the climbers' sun was exposed due to the length of the entrance corridor and the shortage of its ceiling and the traffic problems and the lack of attractions. However, in 1365 a group of cabrioleists from Hamedan visited a large cave and managed to form the cave Related to the Jurassic era. (That is, more than 120 million years ago), the building is located below the Koht Chork and downstream of the crater of the Rudshur, which is located at the lower parts of the Gozlouzan. The cave is formed in a rectangular area of 1500 × 2000. In place, the mechanical weathering function and internal forces together have created a number of cracks or cross faults in the interior space of the space and, due to the provision of other conditions, the cave production process has begun. The cave consists of three floors, with its sub-tunnels, slouches and aclactamites, and many columns on the main passageways. The cone hinged from the ceilings has various colors due to impurities, and they The compounds do not have or do not come in the form of crystal clear glass. Kutal Khour Cave is a limestone cave that is visible in some places in clay and soils containing iron oxide. This cave is about the same age as Alisadr Cave in Hamadan. Of course, these two caves differ from two directions. One is that the cave of al-Assadr in Hamedan is completely cavernous, but the cave of Kotaleh Kord Zanjan is almost dry. Secondly, the cemetery lime is much purer than the lime of Alisadr Cave, which is a factor in the cave's beauty, because the pureness of the lime causes them to be transparent, and thus the light passes through the candles. The mouth of the cave is at an altitude of 1700 meters above sea level, and its height difference is 50 meters from the height of the eye that drains the freshwater from the cave and flows into the river. The entrance of the cave is a 4000-meter wide corridor with a short roof without a stone cave and a few atrioventricles, followed by an atrium of a 950 meter wide corridor with elevations of 2 meters in height and dry pits, which continues with a plunger of 50 meters, and after Crossing a hill to a large courtyard covered with abstracts and abbreviations and pillars. Inside the small crystalline hall, which encloses the columns of columns, a well is 8 meters deep, which is likely to be the outlet of the cavernous forgeries. At present, the cave is divided into three cultural, recreational and sports divisions. Its sports section is only used by cavers and climbers, it is about 4 km, though its end has not yet been discovered. The cave section, also used for general public use, is about 2 km straight, which is said to be just 1.3% of the entire cave. The cultural section of the cave is located in the southern part of the city. The main part is a natural passageway used to hold various ceremonies. Of course, these corridors have no way out and the way out is artificial, but the hall itself is completely natural.
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Area detail This cave located in 11 Km Northeast of Delijan and it’s in the way of Naragh one of city of Markazi Province and on the slop of Takht mountain with 1716 m hight, also this cave is near Kerugan, Veshtegan and Harazijan villages. Type of cave This cave is one of the Calcareous caves and has several floors and it consider a class caves. The unique features of this cave is livelihood of the cave which it can repair cracks automatically. 95% of cave’s wall covered by Calcareous deposits. Formation time According to some experts, this cave belongs to the third period is geology and antiquity of the cave is about 70 million years. Cause naming In the past this area used as a hunting ground, and hunters lead their hunt down to the area and then hunted them. Chal means down, Nakhjir means hunting ground = Chalnakhjir means below the hunting ground Crater details The height of the crater of cave is between 10 to 40 meters and has a cross section of 40 meters. This cave’s crater is higher than the wells of drinking water in Delijan city and didn’t have current area and it is because of Non-principled explosions. Time of discovery This cave was discovered in February of 1988 when digging a well for drinking water of Delijan city. The First caving in this cave At the first time Kamran Soleimani entered the cave for discovering and keep going to depth of 500 meters from the cave but he had to back because his marking rob was finished. The depth of the cave The depth of the cave is between 8 to 10 kilometers and as yet 4 kilometers discovered by local people and cavers. Also 1.2 kilometers of the cave has been improvement for public people. According to experts, there is a lake at the end of the cave that people can boating. In the preliminary depth of the cave can see crystal prisms and also crystalline sponges, charms and coral garden given a lot of beauty to this cave. Cave length The cave has 2 route that both of them are the same at first 600 meters of the route and after that divided two direction, one of them toward the Northeast and the other toward the Northwest. It should be note that the length of each of the routes is over 1300 meters. Geology The reason for the shape of the cave is the opposite fault of the karst region of warren. Most of the shapes in the cave are made of calcium carbonate, aragonite and gypsum. Seams and cracks in the rocks have been created due to the pressures on the rocks. In another step, atmospheric precipitation that have carbonic gas and acidic content has penetrated into fractures and imperfections, resulting in the dissolution of calcium carbonate. In the next step, the solution has cheerful and after millions of years the cave has been created. This cave is one of the upper ceiling and the height of the roof is an average of 8 meters. If we want to mention about other features of this cave, we can say that is considered as a wet and horizontal cave. Also, the permanent ventilation of the cave, which has never caused the lack of oxygen in the cave, is another unique feature. The temperature of the cave in different season is from 7 to 14 degrees, causing the cave has cool air in the summer and warm weather in the winter. The ChalNakhjir Cave was listed by the Cultural Heritage Organization of the Islamic Republic of Iran in 2006.
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