Up to $50

This is a fine part slice specimen of the Northwest Africa (NWA) 2859 meteorite found in the Sahara Desert in 2004. This nice collectible H4 chondrite consista of a brecciated matrix with light and dark clasts and is characterized by abundant chondrules and metal flakes.  The total Mass is registered at 920 grams from a single stone.  The Shock stage is recorded at 2 and the Weathering grade is also a 2.  This is a nice piece weighing 10.4 grams with dimensions of 41x18x6 mm.

This piece displays very well and would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

This is a superb looking full slice of NWA 926 classified meteorite weighing 1.70 grams. Its dimensions are 15x12x5 mm. This H4 classified meteorite was found in 2001 with the total weight of the pieces recovered recorded as a low 201 grams.  This meteorite has a shock stage of 3 and weathering grade of 2.

This professionally prepared piece displays extremely well in its protective case. Would be a beautiful addition to any new or existing collection. Comes with a Canagem and a Pierre-Marie Pelé Collection specimen card.

This is a superb slice of the rare Northwest Africa 3134 meteorite, weighing 0.328 grams and measuring 11x10x1 mm.  This is 1 of 136 approved meteorites classified as EL-6.

This 328mg part slice of NWA 3134 is a Rare EL6, W0/1 Enstatite Chondrite found in 2004 in the Sahara Desert. Enstatites are very rare, accounting for less than 2% of the chondrites. The interior of this meteorite is extremely fresh rating a W0 (no weathering). The W1 was added because of an exterior weathering rind, which hid the beauty of this specimen until it was cut. A total known weight of 970 grams is recorded for this find.  Dual type specimens were submitted to two different institutions because rare minerals were found in an excellent state of preservation.

This hard to acquire piece displays very well with its diamond lap finish, it is a high quality specimen that would make an amazing addition to any new or existing collection. Comes  in a membrane box with a Canagem and a Hupé specimen card.

This is a superb Nantan meteorite individual specimen, directly from Guangxi, China. Its dimensions are 32x22x11 mm and it weighs 17 grams.

The Nantan meteorites are a must for all collectors, more so that it is now very difficult to find worthy specimen. They are a very interesting IAB-MG iron discovered in 1958 and there is an estimated 9.5 T of this material. This is 1 of 88 approved meteorites classified as Iron, IAB-MG.

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

This is a nice looking individual fragment of a Sahara Desert NWA unclassified meteorite. It weighs 32.3 grams and measures 53x30x16 mm. This never classified Northwest Africa stone was found in the Sahara desert around 2000.

It's a good quality NWA meteorite individual fragment. 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 superb Nantan meteorite individual specimen directly from Guangxi, China. Its dimensions are 38x22x11 mm and it weighs 16.3 grams.

The Nantan meteorites are a must for all collectors, more so that it is now very difficult to find worthy specimen. They are a very interesting IAB-MG iron discovered in 1958 and there is an estimated 9.5 T of this material. This is 1 of 88 approved meteorites classified as Iron, IAB-MG.

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

This is a nice etched 2.97 gram Seymchan Iron meteorite end cut measuring 21x13x13 mm. The meteorite was found in 1967 in a brook-bed flowing into the river of Hekandue, a left tributary of the river of Jasachnaja of the Magadan district, USSR. It is classified as an Iron Pallasite main group and is 1 of only 48 approved meteorites classified as such, with a recovered weight of about 323 Kg.

This piece was nicely prepared and it is very stable and rust free and will remain like this for years to come with minimal care. This piece displays extremely well and is a desirable size showing great features. Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

Indochinite is a variety of the mineral tektite, which is a natural glass formed by the intense heat and pressure of a meteorite impact.  These tektites are usually found as small, aerodynamically shaped objects, often teardrop or irregular in shape, resulting from the molten material solidifying as it cooled rapidly after being ejected from the impact site.

Indochinites are believed to have formed around 780,000 to 800,000 years ago, following a significant meteorite impact event that likely created the Southeast Asian tektite strewn field.  The strewn field is quite large, and the tektites can be found scattered over a vast area which includes Vietnam, Laos, and Thailand.   

This piece displays very well, showing multiple characteristics of its origin.  The specimen has a weigh of 27.8 grams and dimensions of 33x32x21.  Comes with a Canagem Collection specimen card.

This is a fabulous 11.4 gram Sericho Pallasite Main Group meteorite, it measures 28x18x17 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.

This is a fantastic shatter cone from France weighing 17.4 grams and measuring 38x26x16  mm. Although not a meteorite, impactites and shatter cones are directly linked to them and their impacts.   Shatter cones are evidence that the rock has been subjected to an extreme shock with very brief high pressures.

Shatter cones are rare geological features that are only known to form in the bedrock beneath large meteorite impact craters. They have a distinctively conical shape with thin grooves (striae) that radiate from the top (apex) of the cone. Shatter cones can range in length from 1 centimeter to several meters. The azimuths of the cones's axes typically radiate outwards from the point of impact, with the cones pointing towards the center of the impact crater.

This impactite was formed 186 million years ago.  This piece displays very well and is a very nice size showing multiple characteristics of its origin. Would make a beautiful addition to any collection. Comes with a Canagem Collection specimen card.

This is a fantastic Impactite Fallback Breccia from Germany weighing 67.3 grams and measuring 75x59x10mm. Although not a meteorite, impactites and shatter cones are directly linked to them and their impacts. The Steinheim Basin today exhibits a distinct morphological depression that is ∼110 m deep and ∼3.5 km in diameter; the height of the central uplift totals to more than 140 m. The original size of the pristine crater is estimated to be ∼3.8 km with an original depth of ∼205 m.

As this drainless morphological depression was filled by lake sediments shortly after the impact, the primary crater morphology is widely preserved. The crater rim is formed by steeply inclined and intensely brecciated Upper Jurassic limestone blocks that also contain numerous shattered chert nodules, as well as some loose blocks of the host limestone. An impact breccia, referred to as the so-called ”Primäre Beckenbrekzie” (“primary basin breccia”) and interpreted as a “fallback breccia”, is known from many drillings in the Steinheim Basin.

Mainly composed of Middle to Upper Jurassic limestones, marls, mudstones, and sandstones, the impact breccia inside the morphological depression of the Steinheim Basin is overlain by lake sediments and is obviously preserved in its original thickness and position.   This piece displays very well and is a very nice size showing multiple characteristics of its origin. Would make a beautiful addition to any collection.