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The Köpet Dag, Kopet Dagh, or Koppeh Dagh, also known as the Turkmen-Khorasan Mountain Range, is a mountain range on the border between Turkmenistan and Iran that extends about 650 kilometres (400 mi) along the border southeast of the Caspian Sea, stretching northwest-southeast from near the Caspian Sea in the northwest to the Harirud River in the southeast. The highest peak of the range in Turkmenistan is the Mount Rizeh, located at the southwest of the capital Ashgabat and stands at 2,940 metres (9,646 ft). The highest Iranian summit is Mount Quchan with 3,191 metres (10,469 ft).
Mount Frissell, 2,454 feet (748 m), which straddles the border of southwest Massachusetts and northwest Connecticut, is a prominent peak of the Taconic Range.
The Karkas mountain chain is a mountain range which is located almost in central Iran. Having a northwest-southeast direction, it is stretched from Kashan to Ardestan for more than 100 kilometres. With an elevation of 3895 metres, the highest peak of the Karkas Mountains is Mount Karkas which is situated close to Natanz.
The Black Mountains of northwest Arizona are an extensive, mostly linear, north-south trending 75 miles (121 km) long mountain range. It forms the north-south border of southwest Mohave County as it borders the eastern shore of the south-flowing Colorado River from Hoover Dam.
The Alborz range, also spelled as Alburz, Elburz or Elborz, is a mountain range in northern Iran that stretches from the border of Azerbaijan along the western and entire southern coast of the Caspian Sea and finally runs northeast and merges into the Aladagh Mountains in the northern parts of Khorasan. This mountain range is divided into the Western, Central, and Eastern Alborz Mountains. The Western Alborz Range runs south-southeastward almost along the western coast of the Caspian Sea. The Central Alborz runs from west to east along the entire southern coast of the Caspian Sea, while the Eastern Alborz Range runs in a northeasterly direction, toward the northern parts of the Khorasan region, southeast of the Caspian Sea. Mount Damavand, the highest mountain in Iran measuring 5,610.0 m, is located in the Central Alborz Mountains.
The Moccasin Mountains is an 11-mile-long (18 km) mountain range located at the Arizona–Utah border in Mohave County, Arizona, and a small north section in Kane County, Utah.
The Aladagh Mountains or the Aladagh Range refers to a mountain range situated in the southeastern section of North Khorasan Province in the northeastern part of Iran southeast of the Caspian Sea. The range is located almost 25 kilometres south of Bojnurd, the capital city of North Khorasan. The Aladagh Mountains merge with the Elburz or Alborz Mountains in the west and then run southeastwards in a northwest-southeast direction. The highest peak of the range is Mount Shahjahan with an elevation of 3032 metres. This peak is located about 35 kilometres east of Esfarayen almost in southeastern part of North Khorasan Province.
The Binalud Mountains or the Binalud Range is a mountain range that runs in a northwest-southeast direction between the Nishapur and Mashhad regions in Razavi Khorasan Province in northeastern Iran, to the southeast of the Caspian Sea. Although far from the Aladagh Mountains, which lie to the northwest in the Province of North Khorasan, the Binalud Mountains are located in such a way that both the Aladagh Mountains and the Binalud Range lie approximately in the same arc, curving from the northwest to the southeast. The city of Mashhad or Meshed is located in the northeastern part of the Binalud Range, and the city of Nishapur or Neyshabur lies on the southwestern section of the range. Situated somewhat to the west of the Binalud Range proper, and with an elevation of 3211 metres, Mount Binalud is the highest point both of the Binalud Mountains and of Razavi Khorasan Province as a whole.
With an elevation of 3032 metres, Mount Shahjahan is the highest point in the Aladagh Mountains and North Khorasan Province in the northeastern part of Iran. This peak is located in the southeastern part of the Aladagh Range. The cities of Faruj and Shirvan are situated in the northeast and the north respectively, the city of Esfarayen lies in the west, and Bojnurd, the capital of North Khorasan, is in the northwest of Mount Shahjahan. Mainly formed in the Miocene and the Pliocene, Mount Shahjahan is made chiefly of Jurassic rocks.
The Bashagard Mountains or the Bashagerd Mountains is a mountain range that is located in southeast of Iran. The mountain range runs in an arc almost in a northwest-southeast direction from eastern parts of Hormozgan Province along the border with Kerman Province and stretching into southern part of Sistan and Baluchestan Province. With an elevation of 2185 metres, Mount Buniken is the highest point of the range located in the western section of the Bashagard Mountains, east of Sardasht in Bashagard County in Hormozgan Province, and in the vicinity of a place that marks the borders of Kerman, Hormozgan, and Sistan and Baluchestan provinces. Made of ophiolite, an assemblage of mafic igneous rocks representing remnants of former oceanic crust, the mountain range was formed finally in the Miocene and the Pliocene during the Alpine orogeny. The mountain range is located in a region with a hot semi-desert climate.
Kuhbonan Mountains or Kuhbonan Highlands,, are a group of mountains that are located in the northern part of Kerman Province in Iran. Stretching in a northwest-southeast direction, the mountain range is situated in northwestern, eastern, and southeastern part of the city of Kerman, northeast of the town of Zarand, and southwest of the town of Ravar. With an elevation of 4233 metres, the highest point of the range is Mount Pelvar or Mount Palvar that is located southeast of the city of Kerman and about 25 kilometres east of the town of Mahan.
The main points that are discussed in the geology of Iran include the study of the geological and structural units or zones; stratigraphy; magmatism and igneous rocks; ophiolite series and ultramafic rocks; and orogenic events in Iran.
Mount Donbeh or Kuh-e Donbeh is a mountain which is situated just southwest of the city of Isfahan in Isfahan Province in Iran. Stretching in a northwest-southeast direction, Mount Donbeh is located south of the Zayanderud River and northwest of Mount Soffeh in the Sanandaj-Sirjan geologic and structural zone of Iran. The mountain is mainly formed of Lower Cretaceous limestone. Only the southeastern part of the mountain is made of Jurassic shale.
Mount Kolah Qazi or Kuh-e Kolah Qazi is a mountain that is located about 30 kilometres southeast of the city of Isfahan in Isfahan Province in Iran. With an elevation of 2534 metres, the highest peak is in the north-central part of the mountain. Having a general northwest-southeast direction, this mountain is situated southeast of Mount Shah Kuh and west and almost parallel to Mount Qaruneh. With an average width of about 5 kilometres and a length of almost 20 kilometres, this mountain is a part of the Mount Kolah Qazi Protected Nature Reserve which covers an area of about 50,000 hectares of national park and 3,000 hectares of protected wildlife region.
Mount Qaruneh or Kuh-e Qaruneh is a mountain which is located about 30 kilometres southeast of the city of Isfahan in Isfahan Province in Iran. Situated southeast of Mount Shah Kuh and being almost parallel to Mount Kolah Qazi this mountain has an average width of about 2 kilometres and a length of around 25 kilometres. Mount Qaruneh has a general northwest southeast direction. With an elevation of 2030 metres, the highest peak is located in the southern section of the mountain. Mount Qaruneh is situated in the Sanandaj-Sirjan geologic and structural zone of Iran and is made mainly of Lower Cretaceous limestone.
Shah Kuh or Mount Shah Kuh is a mountain which is located about 15 kilometres south of the city of Isfahan in Isfahan Province in Iran. With an average width of about 3 kilometres and a length of almost 20 kilometres, this mountain has a general northwest-southeast direction and is situated almost northwest of Mount Kolah Qazi. The highest peak is located in the northern section of the mountain and has an elevation of 2418 metres. Mount Shah Kuh is situated in the Sanandaj-Sirjan geologic and structural zone of Iran, and except for a very small section of Jurassic rocks in its north-central part this mountain is mainly formed of Lower Cretaceous limestone.
Qaflankuh or Qaflankuh Mountain Range is a mountain range that is located about 20 kilometres north of the city of Zanjan in Zanjan Province, Iran. With an average width of almost 20 kilometres and a length of about 100 kilometres, this mountain range is stretched in a northwest-southeast direction, beginning from northwest of Zanjan, passing north of Zanjan and ending southeast of Zanjan. The Qezel Owzan River flows in a valley that separates Qaflankuh Mountains on the south from Talish Mountains on the north. With an elevation of 2971 metres, Mount Sendan Dagh is the highest mountain of the range which is located in the southeast section of this mountain range. There are some mineral hot springs containing sulphur in different parts of this range. Geologically, Qaflankuh Mountain Range was formed during the Tertiary volcanism and plutonism and is made mainly of the Eocene volcanic rocks with very small sections of intrusive rocks in the northern and southern parts of the range.
Hezar Masjed Mountains are a group of mountains that form the southeastern section of the Kopet-Dag Range. Located about 40 kilometres east of Quchan and 70 kilometres north of Mashhad in Razavi Khorasan Province in Iran and stretched in a northwest-southeast direction, the mountains are situated almost at the extreme northeastern part of Iran. With an elevation of 3040 metres, Mount Hezar Masjed is the highest peak of the group and is located almost in central section of the Hezar Masjed Mountains.
The Sahand-Bazman Volcanic and Plutonic Belt or the Sahand-Bazman Igneous Arc or the Central Iranian Range is a mountain range that is made by igneous and pyroclastic rocks. Located East and almost parallel to the Zagros Mountains, the Central Iranian Range is stretched in a north-west-southeast direction from Mount Sahand in Azerbaijan in the north-west to Mount Bazman in Baluchistan in the Southeastern part of Iran. This range was mainly formed during the Tertiary volcanic and orogenic phase and especially in the Eocene volcanism and plutonism. The Central Iranian Range or the Sahand-Bazman Volcanic Belt includes famous mountains such as the Sahand in East Azerbaijan Province, Mount Karkas in the Karkas Mountains and Mount Marshenan in Isfahan Province, the Jebal Barez, Mount Hezar and Mount Lalehzar in Kerman Province, and the Bazman in the Sistan va Baluchestan Province of Iran.
The Pennsylvania State Game Lands Number 166 are Pennsylvania State Game Lands in Blair and Huntingdon Counties in Pennsylvania in the United States providing hunting, trapping, bird watching, and other activities.
References
- ↑ Microsoft Encarta Interactive World Atlas, (2001), Microsoft Corporation
- ↑ Geological Map of Iran, National Geoscience Database of Iran, www.ngdir.ir