New Arrivals

This is a superb individual Tsarev meteorite weighing 56.2 grams. Its dimensions are 53x38x18 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.

This is a 620 gram impact melt rock from the Gallejaur Crater, northern Sweden.  Although not a meteorite, impactites are directly linked to them and their impacts and are probably going to be one of the rarest collection items you'll ever own. Impactite is a slag-like glassy object found on the surface of the earth, formed from rock melted by the impact of a meteorite.

The term impactite encompasses shock-metamorphosed target rocks, melts or suevites and mixtures of the two, as well as sedimentary rocks with significant impact-derived components and shocked mineral grains, tektites, anomalous geochemical signatures, etc.

Rocks, interpreted as impact generated lithologies, occur in a large area surrounding the Gallejaur magnetic structure at latitude 65°10/longitude 19°30 in northernmost Västerbotten County in northern Sweden. These rocks comprise a variety of different types of breccias: authigenic The Gallejaur structure is located in the central part of the Skellefte mining district in the Precambrian Baltic Shield. The ca. 1.9 Ga old Skellefte district is an extensively mineralized, mainly felsic, submarine volcanic belt.  The rocks are described as impact-generated, have been called the Vargfors Group and overlie the Skellefte volcanics and sediments with an angular unconformity.  The youngest rocks in the area, intruding the Skellefte district supracrustals and probably the impact-generated rock, are A/I-type granitoids belonging to the Revsund-Adak granite suite, which have been dated at ca. 1.80 to 1.78 Ga.

This great bookend slab displays very well.  It has a mass of 190x97x39 mm.  Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

This is natural rough tourmaline from Mount Mica Quarry, Paris, Oxford County, Maine, USA.  Mount Mica is one of the most well-known sources of high-quality tourmaline in the world, and it has been a significant site for gem mining since the 1800s. This tourmaline crystal cluster will come protected in a Perky Box.

It is believed that Tourmaline can be used to repel negativity.  It is said to enhance one's physical wellbeing by providing an increase in physical vitality, emotional stability, and intellectual acuity. 

Name:  Tourmaline Cluster
Specimen Size:  Thumbnail-Sized  
Dimensions:   Specimen 25x17 mm / 1.0x0.7 inches
                        Specimen Box 33x33 mm / 1.3x1.3 inches  
Weight:  11.8 Grams / 0.4 Ounces (including box)  
Origin: Mined in Mount Mica Quarry, Paris, Oxford County, Maine, USA

Fulgurite, also known as “fossilized lightning”, are natural glass tubes or formations that are created by the heat of lightning strikes.  When a lightning bolt hits the ground it generates temperatures of up to 30,000 Kelvin (over 53,000°F), hotter than the surface of the sun. This intense heat melts the silica rich sand and fuses it almost instantly, forming hollow branching structures that solidify as they cool.  In the Sahara Desert where thunderstorms occasionally roll in across the desert, these cooled formations can be found beneath the sand. 

The fulgurites from the Sahara Desert are special because of their environment. The desert’s quartz rich sand is the perfect material for these glassy formations. Over time the wind blown sand often buries and preserves these delicate formations protecting them from erosion. Fulgurites are scientifically important because they trap the energy of the lightning and often preserve the composition of the atmosphere at the time of their creation. They are valuable to researchers studying geophysical processes and past climate conditions. And with their irregular shapes and glassy texture they are a sought after collectible for mineral enthusiasts and natural history museums.

Of note, since Fulgurite is created by an impact of lightning hitting the ground, it cannot be called impactite as it is not created by a meteoritic event. 

An olivine volcanic bomb is a type of volcanic rock that contains olivine crystals and has been ejected during a volcanic eruption. Olivine is a mineral that is commonly found in the Earth's mantle and is one of the first minerals to crystallize as magma cools.

Volcanic bombs are large clots of lava that are ejected from a volcano during an explosive eruption. They can vary in size, and their shapes are often streamlined due to their molten nature as they are thrown through the air. When these volcanic bombs contain olivine crystals, they are referred to as olivine volcanic bombs.

This piece has been cut to showcase the beautiful green olivine crystals.  It would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card and a stand will also be included.

Name: Olivine Volcanic Bomb  
Specimen Size:  Miniature-Sized  
Dimensions: 55x26x21 mm / 2.2x1.0x0.8 Inches  
Weight:  34.3 Grams / 1.2 Ounce  
Details: Volcanic activity Mortlake, Victoria, Australia  

This is a superb looking Stony-iron or Mesosiderite Vaca Muerta (Dead Cow) classified meteorite weighing 2.73 grams. Its dimensions are 12x11x8 mm.

This classified meteorite was found in 1861 in the driest desert of the world called the Atacama, in Chile. Mesosiderites are formed on the surface of a parent body as a result of impacts with another body. The impact mixed broken fragments of surface eucrites with iron and olivine from deep within the body. Eucrites are believed to have come from the asteroid Vesta. Analysis has shown, however, that the Vaca Muerta eucrite inclusions are not consistent with other eucrites and possibly originated on a different parent body. Although most have a weathered exterior, they also have lots of metal inside and can be prepared and cut to show this.

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

This is an individual Northwest Africa or NWA 4293 formerly known as NQ10, an H6 chondrite found in the Sahara desert in 2005.  It is one of 5854 approved meteorites classified as such. The meteorite weighs 7.0 grams with dimensions of 20x19x15 mm.  

This fascinating meteorite was mainly found as small individuals and the total weight of the 100's of pieces recovered is recorded as a low 25 kg. The meteorite has a shock stage of 4 and weathering grade of 2.  NWA 4293 is interesting in the way it looks as can be seen in the images.  Most pieces are free of caliche, have a smooth gray surface and are small complete individuals.  The unusual appearance is due to shock hardening and being sandblasted in the desert.

This specimen comes with a Canagem specimen card.  Would make a beautiful addition to any new or existing collection.

This is a superb Nantan meteorite individual specimen, directly from Guangxi, China. Its dimensions are 35x23x16 mm and it weighs 20.9 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 great 145.8 gram Red Suevite Fallback Breccia from the Sääksjärvi crater in Finland. It has dimensions of 79x38x45 mm.  Although not a meteorite, impactites are directly linked to them and their impacts and are probably going to be one of the rarest collection item you'll ever own. Impactite is a slag-like glassy object found on the surface of the earth, formed from rock melted by the impact of a meteorite.

The term impactite encompasses shock-metamorphosed target rocks, melts or suevites and mixtures of the two, as well as sedimentary rocks with significant impact-derived components and shocked mineral grains, tektites, anomalous geochemical signatures, etc.

Sääksjärvi is a lake in Kokemäki, Satakunta, western Finland, east of the town of Pori. The lake is notable because it overlies an impact crater.  The crater is 5 kilometres (3 mi) in diameter and is completely buried under the lake and is not visible at the surface. The age of the impact structure is estimated to be about 543 ± 12 Ma (million years ago), at the boundary between the Ediacaran and Cambrian periods. The enormous heat and pressure at the impact explosion created an interesting melt, a Suevite, and shattered rocks and dust which fell back into the crater area becoming cemented together over the centuries.  These rock formation is known as Fallback Breccia.

These are some of the best looking breccias we've found. Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

This is a rare and fantastic 26.8 gram Libyan Desert Glass from Kuffra, Libya, with dimensions of 51x40x25 mm.

Although its exact origin is still debated, the leading theory suggests it was formed by a high-energy event, such as a meteoric impact or airburst, that melted the desert sand directly where it lay, without being ejected into the atmosphere and re-entering. This results in different physical characteristics compared to tektites​. Libyan Desert Glass is found specifically in the Great Sand Sea of the Eastern Sahara, within a more localized area spanning parts of western Egypt and eastern Libya.

This is a must have 17.8 gram Impactite from Norrbo, Sweden.  Although not a meteorite, impactites are directly linked to them and their impacts and are probably going to be one of the rarest collection items you'll ever own. Impactite is a slag-like glassy object found on the surface of the earth, formed from rock melted by the impact of a meteorite.

The term impactite encompasses shock-metamorphosed target rocks, melts or suevites and mixtures of the two, as well as sedimentary rocks with significant impact-derived components and shocked mineral grains, tektites, anomalous geochemical signatures, etc.  This impactite was formed approx. 89 million years ago when a meteorite crashed into the earth.

This gorgeous slice displays very well.  It is amazingly light considering its mass of 42x38x9mm.  Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

Here we have for you an amazing 1.2 grams premium shaped Irghizite Tektite from the Zhamanshi Crater in Kazakhstan. Its Dimensions are 28x8x5 mm.  These specimen were first found in 2003 and date back 900,000 ± 100,000 years.

This stretched and twisted Irghizite is typical of this material. Unlike other Tektites which can be found hundreds of miles from their point of origin, this is found in and around the crater formed by the impacting body.  In this case it is speculated to be of cometary origin due to analysis of the elements contained within the Irghizites and other impactite found in the crater which are called Zhamanshinite.

This piece displays very well and is a very nice size showing multiple characteristics of its origin.  Would be a beautiful addition to any new or existing collection. Comes in a small specimen box and with a Canagem Collection specimen card.