Incredibly old.
They have grown very small over the millenia due to weathering effects.
The mountains in Munster are much older. The Andes are between 30 and 60 million years old. Mountains in Munster are between 250 and 270 million years old.
The range of fold mountains in Munster is called the Munster Chain or the Munster Hills. These mountains are part of the larger Munster Plateau region in Ireland.
Young Munster was created in 1895.
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.
The mountains of Munster were once higher due to geological processes such as tectonic plate movements and erosion. Over time, these processes have worn down the mountains, reducing their height.
Time and erosion turn young tall mountains into old, worn-down ones.
The Fold Mountains of Munster include the Commeraghs, the Knockmealdowns, the Galtees, the Caha mountains and the Macgillycuddy's Reeks.
The sedimentary rock found in the mountains of Munster is likely to be sandstone. Sandstone is typically composed of quartz grains that give it a red or brown color. It forms from the cementation of sand grains over time and is a common rock type in mountainous regions.
Can you answer it. NO!
young fold mountains are like Himalayas, the Alps and man other.
The main fold mountains in Munster, Ireland are the MacGillycuddy's Reeks and the Dingle Peninsula. MacGillycuddy's Reeks is home to Carrauntoohil, the highest peak in Ireland. These mountains were formed through tectonic plate movements and subsequent folding of the Earth's crust.
In Ireland, in Munster, the south of the island.