Outstanding impact craters around the world
Below are listed some of the most amazing and visually most interesting impact craters known on Earth, arranged by the part of the world and in an alphabetic order:
- Amguid crater – Algeria, Tamanghasset. Well preserved impact crater, less than 100,000 years old. Diameter – 500 – 530 m, 65 m deep.
- Aorounga crater – Chad, Borkou. Remnant of eroded impact crater with a diameter 12.6 km. Formed 345 million years ago or more recently. Looks impressive on satellite images.
- Aouelloul crater – Mauritania, Adrar. Well preserved impact crater. Formed approximately 3.1 million years ago (Pliocene). Diameter 390 m.
- BP Crater – Libya, Kufra. Old, eroded, but nevertheless visible impact crater. Diameter – 2 km, less than 120 million years old.
- Dar al Gani meteorite field – Libya, Jufra. A desert plateau – a famous site where more than 1200 meteorites have been found with total mass over 690 kg. Meteorites here have accrued over an extended time period.
- Hoba meteorite – Namibia, Otjozondjupa. The largest known single-piece meteorite and the largest known natural piece of iron on Earth. The stone fell some 80,000 years ago, it weighs more than 60 tons, 2.7 by 2.7 m long.
- Lake Bosumtwi – Ghana, Ashanti. The most recent medium sized impact crater, 10.5 km across, formed 1.07 million years ago. Filled with 8 km wide lake – the largest natural lake in Ghana. Surrounded by a dense rainforest.
- Kalkkop crater – South Africa, East Cape. Some 250,000 years old impact crater. Diameter – 640 metres. Crater now is filled with light limestone deposits and is visible as a white circle.
- Kamil crater – Egypt, New Valley Governorate. Well preserved, less than 5,000 years old impact crater. Width is 44.8 m, depth – 15.8 m. Around the crater still visible the rayed structure created by the blast.
- Roter Kamm crater – Namibia, Karas. Approximately 4 – 5 million years old impact crater. Diameter of the crater is 2.5 km, depth – 130 m. It was deeper earlier – the bottom is covered with 100 m thick layer of sand.
- Tenoumer crater – Mauritania, Tiris Zemmour. Well visible, interesting impact crater. Diameter – 1.9 km, depth 110 m, age – approximately 21,400 years.
- Tswaing crater – South Africa, Gauteng. Approximately 220,000 years old impact crater, 1.13 km in diameter, up to 119 m deep. At the bottom of the crater is hypersaline lake. People have visited this crater over the last 100,000 years.
- Vredefort crater – South Africa, Free State Province. The largest verified impact crater on Earth. This 160 m wide impact crater was created 2 billion years ago by a bolide 5 – 10 km in diameter.
- Elgygytgyn Lake – Russia, Chukotka Autonomous Okrug. Impact crater, filled with a lake. The lake is approximately 15 km in diameter, with a maximum depth of 175 m. Diameter of the crater is 18 km. Formed in Pliocene, 3.6 million years ago. The lake has never been covered with glaciers.
- Lonar crater – India, Maharashtra. A meteorite crater filled with saltwater lake. The bolide hit the basaltic rock approximately 570,000 years ago. The diameter of the crater is 1.8 km, with 1.2 km wide lake in it, depth of crater – around 150 m.
- Popigai crater – Russia, Krasnoyarsk Krai. Giant impact crater with a diameter of 100 km. Created approximately 35.7 million years ago (Eocene) by a 5 – 8 km large bolide. Here are found up to 1 cm large diamonds created by the impact.
- Sikhote-Alin meteorite strewn field – Russia, Primorsky Krai. A 1.3 km² large area, where in 1947 fell a meteorite shower with joint mass of 70 tons. The largest crater was 26 m across and 5 m deep.
- Tunguska event epicentre – Russia, Krasnoyarsk Krai. The site where an enormous explosion took place in June 30 1908. It is considered that this blast was caused by large meteoroid and is the largest impact in land in the newest history of Earth. Similar event in metropolitan area would lead to death of millions of people.
- Wabar craters (al-Hadida meteors) – Saudi Arabia, Eastern Province. Unusual impact craters in the desert of Arabia. Legendary site, where iron meteorites of large size have been found. Well preserved craters show that the impact was very recent, most likely – the early 18th century.
Australia and Oceania
- Boxhole crater – Australia, Northern Territory. Well visible impact crater, with a diameter of 170 m. Formed some 5,400 m years ago.
- Henbury meteorite craters – Australia, Northern Territory. A group of 13 – 14 meteorite craters with a diameter from 7 to 180 m, up to 15 m deep. Here have been found several tonnes of meteorites. Formed some 4,200 years ago.
- Mahuika Crater – New Zealand, near Snares Islands. Potential impact crater on the bottom of sea, 20 km wide and more than 153 m deep. It is possible, that the meteorite fell sometimes around 1443 AD, creating incredible tsunami waves up to 220 m high.
- Veevers crater – Australia, Western Australia. One of the best preserved small impact craters, formed some 4000 years ago. Diameter – 75 m, depth – 7 m.
- Wolfe Creek Crater – Australia, Western Australia. Very well preserved impact crater, one of most impressive ones. Formed some 300,000 years ago, diameter – 875 m, depth – up to 60 m.
- Kaali crater – Estonia, Saaremaa. Fairly recent (7 600 – 4 000 years old), well preserved meteorite craters. The largest crater has a diameter of 110 m and 22 m depth. It has a lake at its bottom and exposed limestone along its rim. The fall of meteorite created legends.
- Nördlinger Ries – Germany, Bavaria. Enormous impact crater – a large circular depression with a diameter of 24 km. Formed 14.3 – 14.5 million years ago (Miocene). Currently the crater is 100 – 150 m deep, at some places there are exposed the rims.
- Meteor crater (Barringer crater) – United States, Arizona. Visually the most impressive meteorite impact crater on Earth. The diameter of the crater is about 1,180 m, depth – 170 m. The outer side of the rim rises 45 m high above the surrounding plains. The bottom is covered with 210 – 240 m thick layer of rubble. Impact took place some 49,000 years ago.
- Clearwater Lakes – Canada, Quebec. A pair of large meteorite craters – two connected lakes. The diameter of lakes – 26 and 36 km, both created in Permian (290 million years ago). The larger lake has a ring-shaped circle of islands in the center.
- Chicxulub crater – Mexico, Yucatán. Ancient impact crater, with a diameter more than 180 km. One of the largest impact craters on Earth. It was shaped 65 million years ago and it is considered that this fall of bolide led to the great extinction of dinosaurs and many other animals and plants.
- Haughton impact crater – Canada, Nunavut. This impact crater is located in a very remote area on Devon Island. Diameter – 23 km, formed some 39 million years ago (Eocene). Permafrost has helped to preserve this impact crater very well and the site is considered to have a very similar environment to Mars.
- Manicouagan Reservoir – Canada, Quebec. Enormous, ring-shaped reservoir, formed in the impact crater. The impact took place 214 million years ago, shaping approximately 100 km wide crater. The central part of the lake is taken by the enormous René-Levasseur Island, with 2,020 km² area.
- Pingualuit crater (Chubb Crater) – Canada, Quebec. Well pronounced and well-preserved impact crater, 3.44 km in diameter. Formed some 1.4 million years ago, in Pleistocene. Rims of the crater rise 160 m above the tundra. Depth of crater is 400 m, it is partly filled with 267 m deep Pingualuit lake. Lake water is one of the purest in the world.
- Upheaval Dome – United States, Utah. Deeply eroded but nevertheless well visible impact crater. Diameter – 5 km, age – less than 170 million years (Jurassic). Now here are well seen the eroded central dome of the structure.
- Carancas impact site – Peru, Puno. Site, where in September 2007 fell a meteorite. It created 4.5 m deep and 13.5 m wide crater. Some local people later became ill, the nature of this illness is not explained.
- Campo del Cielo – Argentina, Chaco and Santiago del Estero. A strewn field of iron meteorites, which fell some 4 – 5 thousand years ago. The largest meteorite fragment weighs 37 tonnes and is the second heaviest after Hoba meteorite, total weight of meteorites – more than 60 tonnes. 26 impact craters, the largest is 115 by 91 m large.
- Monturaqui Crater – Chile, Antofagasta. Well pronounced meteorite crater, 350 – 370 m in diameter and less than 1 million years old.
- Vargeão Dome – Brazil, Santa Catarina. Less than 70 million years old impact crater – a circular depression with steep walls. Diameter – 12 km, up to 225 m deep.
Described impact craters
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Category includes outstanding impact craters – detectable scars on the surface of Earth left by a body coming from outer space. Category includes also meteorites – natural objects from the outer space.
Bombardment from the space
There are many pieces of solid matter flying around in the space. And VERY frequently they fall on the surface of Earth. There are estimates that every year on Earth fall 18,000 – 84,000 meteorites larger than 10 grams: e.g. one meteorite every 6 – 30 minutes. Every 500 years meteorites form a crater with a diameter of 100 m. It is rather unusual that no giant meteorite has devastated Earth over the last two million years – but it is also calculated that just a few percent or all small craters is found thus far.
The speed of meteorites is dizzying: up to 15 – 20 kilometres per second! Theoretically they might be even 70 km/s fast (252 000 km/h…). Now try to imagine what happens if meteorite has a diameter of one kilometre and hits the surface of Earth 300 times faster than jet aircraft! It burns a profound hole in atmosphere and kicks the crust of Earth with a terrible force.
Earth has experienced such terrible bombardment. It has been calculated that meteorites with a diameter of 1 km hit Earth every 500,000 years and sometimes there come true behemoths, with a diameter more than 10 km. They leave scars in the surface of Earth and traces in the history of climate and life.
The scars – impact craters
As the meteorite hits the ground, it is suddenly stopped by the solid mass of Earth’s crust. Energy can not disappear without a trace – and the immense kinetic energy of the meteorite is transformed into thermal energy: an incredible explosion takes place in the impact site. If the meteorite is smaller, it may explode before hitting the Earth surface, but if it is large – it penetrates the ground and explodes under it, creating a circular crater.
The size of such craters on Earth might be amazing. Vredefort Crater in contemporary South Africa was created by 5 – 10 km large asteroid some 2 billion years ago and has a diameter of 160 km. It seems that this blow triggered the creation of new volcanoes around the impact crater. Nowadays it would erase most life forms on Earth.
The giant impact craters have left much more profound changes and can be detected even billions of years later. Such catastrophic events happen very rarely – once in ten or a hundred million years. As a result these craters still exist but have lost their "visual appeal" – they are just circular structures in the Earth’s crust, very often covered with later sediments.
Smaller impact craters disappear much sooner (if a few million years go together with a term "sooner") but they are more frequent. If they are recent, they still look like true craters and have a visual appeal.
How many impact craters are on Earth?
The existence of impact craters on Earth has been proved recently – in the 1920s. Since then there have been found some 190 impact craters around the world. They are diverse. Some are small, distinctive and fairly new craters. Some are very old, large and eroded. And – some are covered with sediments and invisible.
Theoretically the density of impact craters on Earth should be uniform – there is no reason to believe that some parts of Earth are hit more often than others. The density of known craters though isn’t uniform. There are known more craters in:
- Places where the geological exploration has been more intense – United States, Europe, South Africa etc.;
- places, where are exposed old rocks – Canada, Scandinavia, Sahara, Australia.
Very few impact craters are known in oceans – the ocean floor is constantly renewed by geological processes and can not preserve impact craters which are hundreds of millions of years old.
It is expected that many more impact craters will be discovered in the future, but most of them will not be visually impressive structures – they are buried under thick layers of sediments. But there still are discovered visually very interesting impact craters as well – such as the Kamil Crater (Egypt), which was discovered through Google Earth application in 2008.
And, don’t forget, new craters will be formed as well. Every minute there can fall a large meteorite which can cause a devastating explosion and leave a fresh crater.
Craters have been found on planets and moons throughout the solar system, caused when asteroids or meteors have collided with them. Our Earth has not escaped these impacts, and nearly 200 craters are known on Earth today. Some are easily visited, others are in locations few would ever want to get near. This book details all the known terrestrial impact craters, telling their age, size, and other details, as well as highlighting those easily visited.
The best-preserved impact sites are often difficult to access – buried under ice, obscured by foliage, or baking in desert climes. These desolate landscapes are connected to another place outside of our world, and for photographer Stan Gaz they are sites of pilgrimage – steps in a journey begun as a curious young boy accompanying his father on geological expeditions, and culminating in a six-year journey traveling the globe in search of these sites, much of that time spent leaning his medium format camera out of an open-sided helicopter.