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Q: Why Iran has fold mountains but no volcanoes?
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Related questions

What is the location of the fold mountains of the world?

The Jura mountains in France, and the Zagros mountains in Iran & Iraq are both examples of fold mountains.


What type of mountains are produced by ocean ocean convergence?

Mountains like the Andes, fold mountains with Volcanoes,.


What type of mountains are produced by ocean continetial convergence?

When an oceanic plate collides with a continental plate, it results in the formation of coastal mountain ranges, such as the Andes in South America and the Cascades in North America. This collision causes the oceanic plate to subduct beneath the continental plate, leading to the uplift and deformation of the continental crust, forming high mountain ranges.


What are the 5 types of mountains?

There are actually 4 types of mountains.They are Fold Mountains,Block Mountains, Dome Mountains and Volcanoes.


What are three landforms produced by compression. in the crust?

Volcanoes, fold mountains, plateaus.


How and why are volcanoes and fold mountains formed in the same area on the earth's surface?

The plates dont move.


Which two types of plate boundary forms volcanoes?

Fault Block mountains such as the Sierra Nevada Mountains, and Fold & Thrust Mountains such as the Himalayans.


What two different types of convergent boundaries occur?

Type - SubductionFeature - Trenches or Volcanic mountainsType - CollisionFeature - Folded mountains


What are four things that can happen at plate boundaries?

volcanoes,mid ocean ridges,fold mountains and hot spots


What type of mountains is the Appalachians?

The appalachain mountains are fold mountains


Are the mountains in northern Ethiopia's fold mountains?

the mountains in northern Ethiopia's fold mountains


A range of fold mountains in munster?

The MacGillycuddy's Reeks in County Kerry are a prominent range of fold mountains in Munster. These mountains include Ireland's highest peak, Carrauntoohil. The mountains were formed by the collision of tectonic plates, leading to the folding and uplifting of rock layers.