Flood traces. Iran
Flood traces. Iran

Video: Flood traces. Iran

Video: Flood traces. Iran
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Anonim

The scientific world constantly says about earthly landscapes that they have been created by nature over millions of years by the forces of erosion. Basically - wind. In the north - a glacier. Almost none of them take into account the factor of global water erosion during the flood.

For them, the flood is the invention of dreamers, inaccurate references from the Bible, legends of semi-wild tribes, etc. And their eyes, too, do not see anything, from the word at all. I'm not even talking about ancient quarries, the rocks of which the forces of nature could not grind like that. They do not see the consequences of the catastrophic forces that have transformed many places on the planet in a short time.

gorynych1 pointed to one interesting place in Iran:

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Clear traces of water flows are visible.

into place. Footprints on an area of 85x120km

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When approaching, it is clearly visible. There are many photographs from this place in the Google Earth program. We look …

It is not entirely clear how this remnant could resist the elements?

Residual rock chains run along the direction of water flow

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Smooth vertical surfaces of the remains of the ancient surface.

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A little to the north of this place is a section of the ancient surface, which the water could not wash off, grind, as it happened in the rest of the territory.

View of the plateau from above

At the edge of this plateau

A view of its surface. The darker breed was still partially washed away.

At the edge of the plateau

View from the edge of the plateau to the area washed by the water stream

Further north there are canyons

The conclusion is unambiguous - in such a directional wind erosion could not make outliers oriented in the direction from the ancient surface. In addition, the products of wind erosion should have remained here in their greater mass. And only a stream of water could grind and transfer these volumes of rock somewhere further and deposited in the form of sands.

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