Meteorites

This is a superb whole specimen of the famous Northwest Africa 2965 meteorite weighing 20.6 grams. This is a beautiful specimen from the Thomas Phillips Meteorite Collection.

Its dimensions are 34x20x20 mm. This North West Africa was classified originally as an Enstatite EL6/7, then later as an EL3 and finally an EL-Melt Rock meteorite which was found along with the rest of the total mass of more than 100 Kilograms in the Algerian Desert in August 2005.  This is one of the oldest meteorites on our planet in terms of terrestrial age and has been referred to as a fossil meteorite. 

This Enstatite chondrite shock Level is minimal and weathering varies from 2 to 5. This piece displays extremely well and if cut would show a completely recrystallized enstatite chondrite with polygonal to irregular grain outlines. The grain size varies from 0.02 to 0.7 mm. Round, curved, blocky objects contain coarser-grained orthopyroxene than in the matrix. No relict chondrules were observed.

This hard to acquire piece displays very well with its prehistoric look.  This rare and quality specimen would make an amazing addition to any new or existing collection. Comes with specimen card.

Here we have for you a superb looking Dhofar 020 classified meteorite weighing 17.15 grams. Its dimensions are 31x19x20 mm.  Found 10 March 2000 in Dhofar, Oman, in the Arabian Peninsula this H4/5 classified chondrite has a TKW of 256 Kg with a shock stage of S4 and weathering grade of W3 by the Russian Academy of Sciences, USSR.

Dhofar 020 is an ordinary stone chondrite meteorite. The meteorite is high in free metal and therefore falls in the H class. S4 tells it is highly shocked. Slices of the meteorite, show veins of the cosmic impact created mineral Ringwoodite, although fractures in the stone tend to hide this some. It almost appears to me to have splinted upon impact. The meteorite falls in 4-5 petrology class, a reference to how metamorphed the meteorite is from its original state. This is judged by studying a thin section of the meteorite, most visually at the chondrules, a feature unique to stone meteorite. In a thin section under polarized light, pyroxene chondrules seem more common then their olivine pair. Still some regions in the meteorite show scattered patches of bright olivine inclusions. These are fairly rare, at least on my thin section, and most of the meteorite's olivine and pyroxene, some of the easier things to see in a thin section, appear to have went through a metamorphism, and have "melted" into the matrix and are at times undistinguishable.

This piece displays extremely well, it has a beautiful crust and is a good size. Would be a beautiful addition to any new or existing collection. Comes with a Michael Farmer Meteorites and a Canagem Collection specimen card.

This is a superb looking fragment of the Columbus classified meteorite weighing 3.83 grams. Its dimensions are 16x13x12 mm. This rare H5 classified meteorite was found in Luna County, New Mexico USA in 1997. The total weight of the stones recovered is recorded as a minuscule 165 grams. 

Here's what the finder, Michael Cottingham told us: "This is the Meteorite that started it all for me! My wife and I were out looking for meteorites on a dry lake bed in Southern New Mexico and I found one! This was a new meteorite discovery and it only took me 300 hours of searching to find my First One!  The COLUMBUS Meteorite was found by me in January of 1997. It was Classified by A. Rubin at UCLA as a H5 Chondrite. It was found near Columbus, Luna County, New Mexico and the Total Known Weight is ONLY 184 grams. Very Rare indeed."

This piece is part of America's history and is 1 of 228 approved meteorites from that location. Would be a beautiful addition to any new or existing collection. Comes with a Michael Cottingham Meteorites and a Canagem Collection specimen card.

This is a stunning fragment of the very rare Veevers classified meteorite weighing 1.74 grams. This meteorite is one of only 15 associated with a crater larger than 10 meters across. The crater is about 1 million years old and is one of only 2 craters older than 50,000 years that have meteorites associated with them. This amazingly well preserved specimen measures 13x8x4 mm.

The Veevers crater is located in the Gibson Desert of Western Australia. It has a diameter of 60-80 meters across and a depth of about 6-7 meters. The crater's rim is raised 1.5m above the surrounding plain, and contains exposed rocks thrown from the center of the crater. The sides are gravelly rock with a few larger rocks mixed within. The bottom of the crater is covered with sand.  Veevers is isolated in a vast, flat landscape with no other features in sight. Discovered in the mid-1970's and named by Yeates, A.N., Crowe, R.W.A. & Towner, R.R., in 1976, as The Veevers Crater in honor of Australian geologist Prof. John Veevers, for his work at mapping Western Australia.

In 1984, Dr. Carolyn and Eugene Shoemaker investigated meteorite craters and ancient impact structures throughout Australia. Their search recovered thirty-six small meteoritic fragments from the Veevers crater. Their finds totaled 298.1 grams, and included the largest found to date, 36.3g., now cleaned and coated it weighs 37.0 grams. The Veevers fragments have been described as single crystals of kamacite. Kamacite is a metallic iron with up to 7.5% nickel. Since the Shoemaker trip, more meteorite fragments have been found, bringing the total known weight to around 1 kg. The Veevers crater is naturally rich in iron-rich laterite, which makes recovery of small meteorite fragments hard. It is one of only two impact craters where group IIAB meteorites have been discovered. The other being the Sikhote-Alin craters in Eastern Siberia, Russia.

Would be an exceptional and rare addition to any new or existing collection.  This historically important specimen will come with a ELKK Meteorite Collection and Canagem Collection specimen cards.

Here we have for you a nice looking individual fragment of a Sahara Desert NWA unclassified meteorite weighing 86.5 grams. Its dimensions are 73x43x34 mm. This never classified North West Africa stone was found in the Sahara desert around 2000.

It's a good quality individual fragment NWA meteorite specimen. Some weathering shows the meteorite's time spent aging in the desert. Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

This is a fabulous 16.4 gram Sericho Pallasite Main Group meteorite, it measures 31x21x19 mm.  In 2016, two brothers were searching for their camels and came across several large, dense stones west of the village of Habaswein and south of Sericho, Kenya.  Though recognized as meteorites in 2016, the masses had been known to camel-herders for decades. One village elder said that as a child, he and his brothers would play on top of the stones.  It is classified as an Iron Pallasite main group with low weathering and is 1 of only 68 approved meteorites classified as such, with a recovered weight of about 2.8 T.

This piece displays extremely well and is a nice size showing great features. Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

Here we have for you a nice looking end cut of a Sahara Desert NWA unclassified meteorite weighing 82 grams. Its dimensions are 54x47x20mm. This never classified Northwest Africa stone was found in the Sahara Desert around 2000.

It's a good quality cut NWA meteorite specimen showing interesting internal structure (L5?) and attractive mottled interior with chondrules and metallic flakes. Some weathering shows the meteorite's time spent aging in the desert. 

Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

Here we have for you a nice looking individual fragment of a Sahara Desert NWA unclassified meteorite weighing 87 grams. Its dimensions are 47x45x28 mm. This never classified North West Africa stone was found in the Sahara desert around 2000.

It's a good quality individual fragment NWA meteorite specimen. Some weathering shows the meteorite's time spent aging in the desert. Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

These are fragments of the Abee meteorite (MB 8) that fell in Alberta, Canada at 11:05 p.m. on June 9th 1952.  It took five days to find it in a wheat field belonging to Mr Harry Buryn.  It is located in the community of Abee, Alberta, Canada in Thorhild County, along the Canadian National Railway and Highway 63, 16 km north of Thorhild and 49 km from Boyle.

This rare and highly collectable EH4 Enstatite chondrite is 1 of only 21 approved meteorites classified as such, 1 of 3 being an observed fall and only 1 of 5 not found in Antarctica. The total Mass is registered at 107 Kilograms in one stone recovered from a 6 ft (1.8 m) deep crater.  This is a great opportunity to acquire fragments that were used for testing in laboratory weighing 508 milligrams.

This hard to acquire rare specimen would make an amazing addition to any new or existing collection. Comes with a Dr. Martin Horejsi Collection of Meteorites and a Canagem Collection specimen card and is displayed and protected in a pill case.

This is a superb tumbled individual Tsarev meteorite weighing 38.5 grams. Its dimensions are 45x27x25 mm. Twenty-eight specimens of this L5 classified meteorite were found in fields.  The largest mass weighs 284 kg, the smallest 761 gr with a total weight of 1.23 Tons. The greatest distance between the find sites was 6.0 km.

In 1968, amidst a global surge in conflicts, a remarkable discovery was made in a small village in Volgograd Oblast. This region, known as the primary site of the Battle of Stalingrad—one of the largest and bloodiest battles in history—yielded an extraordinary find in the quiet fields near the rural village of Tsarev.

The Tsarev meteorite, named after the Russian word for czar, is a stone meteorite responsible for one of the largest meteorite showers in Russian history. This meteorite shower occurred on December 6, 1922, but the stones were not discovered until 1968 and only recognized in 1979. The Tsarev meteorite's mineral composition matches that of ordinary chondrites, including olivine, orthopyroxene, clinopyroxene, maskelynite, calcium phosphates, nickel-iron, troilite, chromite, ilmenite, and rutile.

Academic analysis of the Tsarev meteorite reveals significant features: large grains of nickel-iron, light grey areas with well-preserved chondritic texture, and dark areas containing a matrix with olivine grains and remnants of chondrules. 

This specimen would be a beautiful addition to any new or existing collection.  Will come with a Canagem specimen card.