China's Rainbow Mountains were born around the same time as the Himalayas.

The colorful swirls and stripes that characterize China's Rainbow Mountains would have remained hidden without the epic tectonic collision that created the Himalayas.

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Name: Rainbow mountains

Location: Zhangye Danxia National Geopark, Gansu, China

Coordinates: 38.96080921027964, 100.07034421783024

Why it's incredible: The mountains' folded rocks form stunning rainbow patterns.

As the name suggests, China's Rainbow Mountains are multicolored formations in the northwest of the country. The landscape in this region is otherworldly, with vibrant bands that look like they were spray-painted onto the rocks.

The Rainbow Mountains are located in the foothills of the rugged Qilian mountains and likely formed around the same time as the Himalayas, approximately 50 million years ago, according to NASA's Earth Observatory. Land that was once relatively flat was scrunched up and folded into jagged terrain when the Indian tectonic plate collided with the Eurasian plate. This was because these plates have a similar rock density, so neither could slip beneath the other to form a subduction zone, according to the U.S. Geological Survey (USGS).

But the basis for the mountains' rainbow pattern was laid long before the epic collision.

The Rainbow Mountains are made of sandstone and siltstone — sedimentary rocks that form when sand and silt, respectively, are compacted and cemented together over long periods of time. These rocks — with their bands of different colors — were deposited before the Himalayas formed.

The colorful bands are the result of iron and other trace minerals in the stone. Each band has a different composition that determines its pigment. For example, the deep red stripes are rich in iron oxides, the yellow layers contain abundant iron sulfide and the green bands hold more chlorite and iron silicates, according to a 2016 article in Forbes.

The mountains are made of mineral-rich sandstone and siltstone.

Iron and other minerals accumulated in the rock while the sand and silt grains were still cementing together. Groundwater circulating in the pore space between the grains deposited the minerals, coating each grain and further gluing the rocks together.

The slanted bands we see on the flanks of the Rainbow Mountains today are upturned layers that would have remained buried and horizontal had the Indian and Eurasian plates not smashed into each other. The bunching of the land by plate tectonics was followed by intense erosion, which wiped away any sediment covering the colorful layers. Luckily for modern visitors, there is no vegetation to obscure the striking rainbow pattern.

The Rainbow Mountains are a popular tourist attraction. They are protected as part of the Zhangye Danxia National Geopark, but visitors can climb to the top of the hills and admire the view using wooden stairs and platforms.