$ 15 & Under

This is a fantastic Impactite Fallback Breccia from Germany weighing 21.3 grams and measuring 60x41x6mm. 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.

This is a nice looking individual fragment of a Sahara Desert NWA unclassified meteorite. It weighs 11.8 grams and measures 25x27x14 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 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 4 grams with dimensions of 16x14x11 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.

Iceland Spar, also known as optical calcite, is a clear, transparent variety of calcite famous for its unique optical property called double refraction. When you place the crystal over text or an image, it appears doubled — a visual effect that occurs because light splits into two rays as it passes through the crystal. This fascinating trait made Iceland spar historically important in early optical instruments and scientific studies, including navigation and the development of polarizing microscopes.

It’s typically colorless or very lightly tinted and forms naturally in sharp, rhombohedral shapes. High-quality Iceland spar is most famously found in Iceland, though it also occurs in places like Mexico, the U.S., and China.

Iceland Spar (optical calcite) is often associated with clarity, insight, and truth. Because of its double refraction property, some see it as a symbol of seeing beyond surface appearances — helping to highlight different perspectives or reveal hidden aspects of a situation. It's thought to support clear thinking and honest communication, making it a favorite for meditation or decision-making spaces.

Name: Iceland Spar Optical Calcite
Specimen Size:  Miniature-Sized
Dimensions: 30x27x25 mm / 1.2x1.1x1.0 inches 
Weight: 44 Grams / 1.5 Ounces
Origin: Guangxi Province, China

This is an outstanding Impact Melt Glass specimen or bomb weighing 1.0 grams.  Its dimensions are 20x14x6 mm.  Although not a meteorite, impactites are directly linked to them and their impacts.

This Henbury glass, or more specifically vesicular impactite, was found in the Northern Territory of Australia. Thirteen craters were found 8 miles southwest of the town of Henbury, the largest of which was 720 x 360 feet.  Henbury impactite was formed by a meteorite impact that occurred around 4,700 years ago. The meteorite is believed to have exploded upon entering the Earth's atmosphere, creating multiple craters which produced the impact glass.

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 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 piece displays extremely well.  It is amazingly light considering its mass.  It has a unique hollow sound when you tap it.  This Australian find is very well shaped and preserved. These pieces are becoming more difficult to acquire so this is a good time to get a fine specimen.  Would be a beautiful addition to any new or existing collection.  Will come with a Canagem specimen card.

These are metallic-black, orthorhombic brookite crystals.  They are fine specimens from the famous mines at Magnet Cove, Arkansas. They are excellent, older material for the species and locality. The crystals come in a small glass vial.

Brookite is often associated with energy expansion, transformation, and heightened awareness. Some believe it helps with breaking through mental or spiritual barriers, making it a useful stone for those seeking personal growth or deeper understanding.

Name: Brookite var. Arkansite 
Specimen Size:  Thumbnail-Sized
Dimensions: 22x14 mm / 0.9x0.5 inches 
Weight: 4.6 Grams / .2 Ounces (incl glass vial)
Origin:  Fisher Mountain, near Mount Ida, Arkansas, USA

This is a sculpted plate of Limonite after Pyrite.  Limonite after pyrite is a type of pseudomorph, meaning limonite has replaced the original pyrite crystal structure while keeping its shape. This occurs when pyrite oxidizes over time, often in the presence of water and oxygen, transforming into limonite, a mixture of hydrated iron oxides. The result is a rusty brown to yellowish mineral that retains pyrite’s cubic or pyritohedral shape but with a softer, earthy texture.

It believed that limonite after pyrite combines pyrite’s energy of strength and manifestation with limonite’s grounding and protective qualities. It is sometimes associated with stability, resilience, and transformation, symbolizing the ability to adapt and grow through life’s changes.

This is a great thumbnail sized Limonite after Pyrite pseudomorph specimen from Spain.

Name: Limonite after Pyrite Cluster
Specimen Size:  Thumbnail-Sized
Dimensions: 25x15x7 mm / 1.0x0.6x0.3 inches
Weight: 3.09 Grams / 0.1 oz
Origin: Mined in Carratraca, Spain

This is a fantastic Impactite Fallback Breccia from Germany weighing 16 grams and measuring 48x37x7mm. 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.

This is a fantastic 3.87 gram part slice NWA (Northwest Africa) 869 L3-6 classified meteorite. The dimensions of the specimen are 15x9x9 mm.  This part slice displays a superb crust on one surface and and multiple cut faces that have been professionally prepared to show all the chondrules typical of the best 869s.  

Most NWA 869 samples are individual meteorites but some fragments (mostly >1 kg) also occur. In most cases the fusion crust has been polished or ablated by wind erosion. Many samples are more severely affected and show faces with deep wind erosion features. Fracture faces, formed by ground collision, show a typical gray-green color and sometimes visible brecciation (light and/or dark clasts). 

This premium quality specimen shows the best of 869 you can get today and would be a beautiful addition to any new or existing collection. Comes with a signed Mark Bostick Collection and a Canagem Collection specimen card.

This is a beautiful black Biotite crystal book from the Calcite Vein-Dikes of the Grenville Geological Province Ontario, Canada. This specimen is a great example of both the classic crystal shape and attractive dark coloration. 

Biotite is rarely considered a valuable mineral specimen, but it can accompany other minerals and compliment them. In Bancroft, Ontario, Biotite forms large crystals with green apatite and hornblende. Single large plates or "books" of biotite can grow to considerable size and can make impressive mineral specimens. 

Stand not included.

Name:  Biotite Mica  
Specimen Size:  Large Cabinet-Sized  
Dimensions:  125x71x3 mm / 4.9x2.8x0.1 inches  
Weight:  39 Grams / 1.4 Ounces  
Origin:  Ontario, Canada  

You will receive 1 Sikhote-Alin meteorite.  This size of Sikhote-Alin is great for jewelry making and a variety other small projects.

These are great looking Russian Sikhote-Alin classified meteorites weighing 0.2-0.49 grams.  This Iron (IIAB) Coarsest Octahedrite classified meteorite was recovered in Russia after the fall of February 12, 1947.  So far approximately 23 tons of this material have been recovered.  These specimens are known as shrapnel specimens, ripped and torn edges reminiscent of bomb shrapnel. They broke due to atmospheric pressure and/or mid-air collisions, and possibly explosive fragmentation upon impact. These pieces are a good example of the shrapnel type Sikhote-Alin.

Comes with a Canagem Collection specimen card.

This is a 22.3 gram Grey Melt Rock from the Köfels Structure, Austria. It measures 38x22x21 mm.  The specific origin of kofelsite rocks is uncertain & debated. The rocks are found in a landslide deposit in western Austria. Researchers have suggested that the landslide was impact-triggered. The kofelsite samples in the landslide deposit thus may be impactites (fused rocks from the heat of impact). Some workers have suggested that the rocks are frictionites (fused rocks from landslide heating).

The Köfels landslide was a huge mountain rockslide (a Sturzstrom) that occurred in the Austrian Alps about 9800 years ago near the present day village of Köfels. Some of its features mystified geologists for quite some time. One hypothesis was that it had been caused by an asteroid impact — a Köfels impact event — but more recent research has rejected the idea. This didn't stop a pair of British engineers from publishing a book that claims that a) it was an asteroid impact, b) it inspired a lot of myths, and c) it was recorded on an ancient Sumerian clay tablet.

The reason for the original impact hypothesis was the presence of fused rock. At the time, the only processes known to be able to do this were either volcanism or meteor impacts. Later research found that it can be also produced by friction and similar fused rock has been found in other large rockslides.

This specimen displays very well even if not proven to be meteorite impact related.  Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

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. 

Fulgurite is often considered a symbol of transformation, energy, and connection to the divine, primarily due to its association with lightning.  Some believe fulgurite carries the power of lightning itself—acting as a conduit between the physical and spiritual realms. It's said to help with spiritual awakening or to encourage personal growth by clearing blockages, especially when it comes to energy flow or communication with higher states of consciousness. Because of its fiery origins, it can be seen as a tool to help ignite creativity or insight, as lightning strikes are associated with sudden inspiration or illumination.

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 5.2 grams with dimensions of 25x16x10 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 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 5.5 grams with dimensions of 22x18x9 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 specimen of Star Mica or Muscovite cluster.  These clusters show crystals that grow in sheets or book formations.  It is silvery gold with good transparency when held up to the light.  The name Muscovite comes from the term Muscovy Glass which was a name for the thick sheets of Mica used as a substitute for glass Russia. The name Mica is derived from the Greek word that means to split.

On this nice specimen, the matrix faces are covered with beautiful golden yellow point stars of muscovite mica, a typical shape for this rare mica formation. The stars are the result of twinning; the points show a bit of wear but this does not detract from the beauty of such a piece.

Name: Star Mica - Muscovite
Specimen Size:  Miniature-Sized  
Dimensions:  53x40x24 mm / 2.1x1.6x0.9 inches  
Weight:  51.3 Grams / 1.8 ounces  
Origin: Mined in Minas Gerais, Brazil