Crater, impact crater

Crater

A crater on Mars.

The lunar crater Sulpicius Gallus is named after him.

This crater is potentially valuable for astronomical observation.

The largest crater in Planum Australe is McMurdo Crater.

The town was established in 1876 on a farm called Visgat, on the Vredefort crater, the largest and oldest visible bolide impact crater in the world (with a diameter of ).

This is European space agency Mars Express, image of a crater on Mars and in the middle of the crater we have liquid water, we have ice.

It has volcanoes on it. And that's Mount Olympus on Mars, which is a kind of huge volcanic shield on that planet.

The crater Wrottesley on the Moon is named in honour of John Wrottesley.

So, specifically what we are doing now is that Rover is going down in that crater.

Kärdla is a meteorite crater near the town of Kärdla in Estonia.

Mars has the largest impact crater in the solar system, Hellas Basin.

So, this is called Victoria Crater, which is about a few football fields in size.

At the north pole, the rim of Peary Crater has been proposed as a favorable location for a base.

Some 400 porters carry sulphur baskets on their shoulders from the crater.

The rim of Shackleton Crater, towards the Lunar south pole, also has a near constant solar illumination.

The site is now occupied by the hamburgmuseumThe crater Repsold on the Moon is named after him, as is the asteroid 906 Repsolda.

On the left you can see a lava tube forming at a recent eruption Mount Etna in Sicily and this is the way these tubes form.

The Nazca pampas are made of a very fine layer of reddish alluvial material of granitic volcanic origin (from Batolito de la Costa).

Argyre Planitia is a plain located within the impact basin Argyre in the southern highlands of Mars.

It was named in honor of Merton Davies (1917 2001), a pioneer in the cartography of planetary bodies.

Zeeman is a lunar impact crater located on the far side of the Moon near its south pole.

Numerov is a lunar impact crater that is located on the Moon's far side, deep in the southern hemisphere.

Hellas Planitia is a plain located within the huge, roughly circular impact basin Hellas located in the southern hemisphere of the planet Mars.

The region includes the volcanoes (from north to south) Hecates Tholus, Elysium Mons and Albor Tholus.

And what you're seeing here is a cloud of densely packed, hydrogen sulfide rich water coming out of a volcanic axis on the sea floor.

Airy 0 is a crater on Mars whose location defines the position of the prime meridian of that planet.

Davies is a crater on Mars located at 46 N 0 E on the fringe of Acidalia Planitia near Arabia Terra.

Defying the shadows, Anto descends the crater and lights the path with a small torch attached to the helmet he bought with his money.

The crater D'Arrest on the Moon is named after him, as well as a crater on the Martian satellite Phobos and the asteroid 9133 d'Arrest.

There are many areas and features that could be subject to long term study, such as the Reiner Gamma anomaly and the dark floored Grimaldi crater.

The crater has a diameter of 6.1 kilometers and is located at 14.5 deg south and 174.7 deg east, within the larger crater Gusev.

And the most amazing thing that came out of that mission was a strong hydrogen signature at Shackleton crater on the south pole of the moon.

An equatorial belt was noted with a crater age distinctly younger than the northern part of the province and of Noachis Terra to the south.

Established in 1902, Crater Lake National Park is the fifth oldest national park in the United States and the only one in the state of Oregon.

This, we later found out, is, in fact, a crater, but there are very few craters on the surface of Titan, meaning it's a very young surface.

It was named in honor of the British Astronomer Royal Sir George Biddell Airy (1801 1892), who in 1850 built the transit circle telescope at Greenwich.

Geological history Taal Volcano is part of a chain of volcanoes along the western side of the edge of the island of Luzon, which were formed by the subduction of the Eurasian Plate underneath the Philippine Mobile Belt.

Geologists have noted the chemical and geological content of these three mountains to be much different than that of the Cascade Range, simply because they are not volcanic in origin, while the entire Cascade Range is postulated to have formed from volcanic action.

So what you are seeing here are the layers on the wall of that crater, and the Rover is going down now, measuring, you know, the properties and analyzing the rocks as it's going down, you know, that canyon.

Examination of images from the Clementine mission appear to show that parts of the crater rim are permanently illuminated by sunlight (except during Lunar eclipses).

To do so, he has to descend every day to the bottom of the crater, where the sulphurous gas emanating from the bowels of the earth solidifies on contact with air.

And the first paper is a standard scientific paper presenting evidence, Iridium Layer at the K T Boundary, Potassium Argon Dated Crater in Yucatan, Indicate That an Asteroid Killed the Dinosaurs.

This is one very large crater. Geologists love craters, because craters are like digging a big hole in the ground without really working at it, and you can see what's below the surface.