It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
Originally posted by Gazrok
If we're to accept the photo, most likely candidate would be an impact crater from a large meteor...would certainly account for the shape of it...
Originally posted by LucidDreamer85
Originally posted by Gazrok
If we're to accept the photo, most likely candidate would be an impact crater from a large meteor...would certainly account for the shape of it...
find us an impact crater that looks like us so we can compare as an example? Don't just make the statement, add some evidence . Not saying it isn't but you can't just say it is. The shape to me seems different from an impact crater as the IC are usually more indented into the ground, and this seems to be more of a hill shape.
Source (a lot of text but it seems relevant)
On Earth, a meteorite crater, also known as an impact crater, forms when a meteorite greater than 3 feet (0.9 meter) in diameter hits the surface. The size and depth of the crater depend upon the size and incoming speed of the meteorite. In general, a meteorite that hits Earth's surface creates a crater twelve to twenty times its size. When a meteorite slams into Earth, it forms one of two types of craters: simple or complex. A relatively small meteorite forms a simple impact crater. Measuring typically less than 3 miles (5 kilometers) in diameter, this type of impact crater is relatively smooth, bowl-shaped, and nearly circular.
The rim or upper edge of the crater is well-defined and raised above the surrounding landscape. The interior of the crater is steepest near the rim. The slope gradually decreases toward the center of the crater. Partially lining the interior of the crater is a layer of breccia (pronounced BREH-chee-ah; a coarse-grained rock composed of angular, broken rock fragments held together by a mineral cement).
The energy of the impact typically causes some rocks to melt. In simple craters, this impact melt is often found as small blobs of material within the breccia layer. Surrounding the rim of the crater is a circular layer of rock and dust thrown out of the crater during its formation. Known as an ejecta blanket, this layer is deepest close to the rim. It becomes increasingly shallow outward from the crater.
Famous Patom crater, discovered in 1951 by geologist Vladimir Kolpakov, is still one of the most mysterious objects in the natural world. First, it is unclear how he appeared on the surface of the earth, and secondly, why over fifty years, no one has studied it. Only in 1971 was made a few pictures from the helicopter. In size and appearance it is similar to a lunar crater. Height of about 40 meters, diameter of the ridge - 86 meters. Approximate weight of the Makhin of crushed limestone blocks - about a million tons. At the crater rising several 200-year-old larch. Irkutsk scientists brought from a summer expedition cut one of these trees. There are several dozen versions of the appearance of the crater. Two basic: its volcanic origin, but no signs of lava. The second version - that it should not drop to the ground a huge meteorite. It insists its discoverer crater Vladimir Kolpakov. - That is, initially all the same meteorite origins, but a specific meteorite. What no one has ever seen - the director of the astronomical observatory ISU Sergei Yazev. During the expedition Irkutsk scientists measured the size of the crater, took samples of soil. Now they are studying at the Irkutsk Institute of Geochemistry. A Research Center held a discussion meeting of the club. Showed video captured during the summer, and then everyone can make their case. There were, and sensational statements: for example, geologists have argued that only a few years ago just west of the crater Patom were found a few more similar sites. There is documentary evidence. And if one considers that roughly the same area in 2002 was recorded drop Vitim bolide, it may be assumed that Bodaybinsky area as a magnet attracts various phenomena of outer scale. - Either we have here the polar night long, all day. Either we have here is a zone, the bands, where the fall of space aliens, clots of energy, and the like, - said geologist Valery Andreyev.
Originally posted by andre18
WHy hasn't anyone mentioned a meteoroid as the probable cause???
The split in the sky grew larger, and the entire Northern side was covered with fire. At that moment I became so hot that I couldn't bear it, as if my shirt was on fire; from the northern side, where the fire was, came strong heat. I wanted to tear off my shirt and throw it down, but then the sky shut closed, and a strong thump sounded, and I was thrown a few yards. I lost my senses for a moment, but then my wife ran out and led me to the house. After that such noise came, as if rocks were falling or cannons were firing, the earth shook, and when I was on the ground, I pressed my head down, fearing rocks would smash it. When the sky opened up, hot wind raced between the houses, like from cannons, which left traces in the ground like pathways, and it damaged some crops. Later we saw that many windows were shattered, and in the barn a part of the iron lock snapped."
Source
The Patom crater, in contrast to similar forms of relief known to science, is strikingly peculiar because it looks very much like a volcano but contains no trace of erupted in-depth rock. It all consists of fragments and boulders (sometimes several meters thick) of local sedimentary rocks, i.e. Precambrian limestone. The entire mountain is composed of the same limestone, and both inside and outside the crater the limestone contains no trace of a change induced by hydrothermal or any other processes. Nor does the shape of that relief feature look like a classic blast-made meteorite crater. It does not resemble a crater from which the rock was ejected by force of explosion.
Source (as above)
...the celestial body in question was made the mounted boulders of solid methane rather than solid hard iron or olivinite and they scattered loose when it passed through the dense layers of the atmosphere flying 30 km high and some fragments dispensed as flying cassette elements fell out upon the ground within the “zone” extended in the northern direction. If a meteorite flying at a space velocity penetrates the earth, thus creating a rock grinding zone around itself (without a blast discharge) of about one million cubic meters, and if we apply the soil loosening factor for normal explosion processes (1, 2), an increase in the volume of rock mass will amount to 200,000 cubic meters. Calculations have indicated that the depth of such a zone should be over 200 m.
In the "nest of fire eagle" is a huge egg
Under Patom crater at a depth of 100 meters, scientists discovered a strange three-dimensional object.
Now I'm one hundred per cent I can say that under the crater, we have identified three-dimensional object that has increased electrical conductivity. Its shape resembles an ellipsoid or a cylinder, the tip of which is located at a depth of approximately 100 meters. Down it goes to 600 - 700 meters.
But, judging by the results, it is not made of iron, not from any other metal known to mankind. But the fact that there is something - a fact!
Originally posted by internos
If i'm not mistaken, that would be Patomsky crater (патомский кратер),
i remember to have seen a picture in which the central peak looked the same, but even the angulation of the photo was the same, maybe it was even the same photo: but i'm not sure, honestly.
Manicouagan Reservoir lies within the remnant of an ancient eroded impact crater (astrobleme). The crater was formed following the impact of a 5 kilometres (3 miles) diameter asteroid which excavated a crater originally about 100 km (62 mi) wide although erosion and deposition of sediments have since reduced the visible diameter to about 72 km (45 mi). It is the fifth largest confirmed impact crater known on earth[1]. Mount Babel is interpreted as the central peak of the crater, formed by post-impact uplift.