What country is Mary from?
Turkmenistan
Mary, Turkmenistan
| Mary Merv medieval times-1937 Alexandria Margiana antiquity | |
|---|---|
| Coordinates: 37°36′N 61°50′ECoordinates: 37°36′N 61°50′E | |
| Country | Turkmenistan |
| Region | Mary |
| Government |
In which country is Ashgabat situated?
Ashgabat, formerly Ashkhabad, Ashkabad, Askhabad, or (1919–27) Poltoratsk, city and capital of Turkmenistan. It lies in an oasis at the northern foot of the Kopet-Dag (Turkmen: Köpetdag) Range and on the edge of the Karakum (Turkmen: Garagum) Desert, about 19 miles (30 km) from the Iranian frontier.
Who was William the Thirds wife?
Mary II, (born April 30, 1662, London, England—died December 28, 1694, London), queen of England, Scotland, and Ireland (1689–94) and wife of King William III.
Who killed Marys second husband?
Mary soon became pregnant. Mary’s private secretary, David Rizzio, was stabbed 56 times on 9 March 1566 by Darnley and his confederates, Protestant Scottish nobles, in the presence of the queen, who was six months pregnant.
Is Turkmenistan all desert?
Terrain of Turkmenistan consists of a flat-to-rolling sandy desert, the Karakum, with its dunes slowly rising to the south; by the time they reach the border with Iran, they become the low mountains known as the Kopet Dag. The Caspian Sea washes the western shores of this mostly arid country.
Where is the Karakum Desert in Central Asia?
Karakum Desert, also spelled Kara-Kum, Turkmen Garagum or Gara Gum (“Black Sand”), Russian Karakumy, great sandy region in Central Asia. It occupies about 70 percent of the area of Turkmenistan.
Is there a natural gas crater in the Karakum Desert?
The Darvaza gas crater, also called the “Door to Hell” or the “Gates of Hell” by locals, a crater of natural gas that has been burning since 1971, is located in the Karakum Desert. The crater is a major tourist attraction, with hundreds of visitors arriving each year.
How tall is the sand in the Karakum Desert?
The plain of the Central Karakum runs from the Amu Darya to the Caspian Sea along the same incline as the river. The height of wind-accumulated, half-overgrown sand ridges ranges from 250 to 300 feet (75 to 90 metres), depending on age and wind velocity.
How did the Karakum Desert become a saline area?
Saline areas called solonchaks are also formed by the evaporation of subsoil water. Some 30 million years ago the entire Karakum region was covered by the sea. Orogenic (mountain-building) processes in the southern part of the Turan Plain resulted in a gradual diminishing of the sea and, ultimately, in its disappearance.