New Arrivals

Product Type: Rutilated Quartz  
Approx Weight (per piece): 12.8ct  
Size: 16mm  
Shape:  Round Cut  
Color: Clear White with Golden Needles  
Clarity: Transparent  
Origin: Brazil  

Rutilated Quartz is a beautiful variety of Quartz that contains needle-like inclusions of the mineral Rutile. These golden, coppery, or silver-colored needle inclusions create unique patterns within the Quartz.

Rutilated Quartz is thought to amplify energy, enhance clarity and intuition, facilitate spiritual connection, provide protection, and promote healing and manifestation.

Product Type: Smoky Quartz
Approx Weight (per piece):  6.9ct 
Size: 16x10mm
Shape: Barrel Cut 
Color: Dark Smoky 
Clarity:  Clean to the eye
Origin:  Brazil

Product Type: Tourmalinated Quartz  
Approx Weight (per piece):  13.3ct  
Size: 17x13mm  
Shape:  Octagon Cut  
Color:  Colorless  
Clarity:  Tourmalinated Clear  
Origin:  Brazil  
Treatment:  Natural - No known treatment  

The appearance of Tourmalinated Quartz is characterized by clear or milky quartz with dark, thread-like, or needle-shaped inclusions of black tourmaline running through the stone. These inclusions can vary in density, giving each piece a distinct and unique appearance.

Tourmalinated Quartz is a crystal that combines the properties of Clear Quartz and Black Tourmaline. It is believed to offer strong protection by shielding against negative energies and enhancing the grounding and balancing effects of Black Tourmaline. The crystal is thought to amplify intentions and promote emotional healing. It may also support spiritual connection, chakra alignment, and provide emotional support during challenging times.

This is a natural cluster formation of large calcite crystals with hematite inclusions. This piece has some white color to translucent crystals with areas of orange/red coloring from hematite inclusions, with sharp tabular crystal formations. There are some nicks and imperfections on a few crystals but would still shine in the proper setup.  They don't take away from how interesting this piece is.  Would be a nice addition to any new or existing collection.

Name: Calcite with Hematite Crystal Cluster
Specimen Size:  Cabinet-Sized
Dimensions: 75x54x55 mm / 2.8x2.1x2.2 inches 
Weight:  160.5 Grams / 5.7 oz 
Origin: Mined in Lane Quarry, Westfield, Hampden Co., Massachusetts, USA

Product Type: Ruby
Approx Weight (per piece): .54ct 
Size: 4mm 
Shape: Square Cut
Color: Pigeon Blood Red 
Clarity: Transparent
Origin: Madagascar

This is a must have 16.8 gram Impactite, monomict impact breccia from the Agoudal, Imilchil impact structure, Morocco.  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. According to the state of conservation of the meteorite into the sedimentary layers "Soltanian" and the dating of ancient lake sediments of the Isli lake, we can estimate their age limit to 40,000 years. 

More than 183 structures of meteoritical impacts are highlighted on the Earth, including only three reported dual impact craters. The impact craters of Isli and Tislit are respectively located at 10 km and 4 km from the Imilchil village on the Central High Atlas in Morocco at respective altitudes of 2272 and 2266 meters. They are spaced apart from each other by 9.4 km. The origin and the date of formation of these two lakes are still unknown today. Surveys undertaken near them and in the surrounding areas leads to believe that they correspond to a dual meteoritical impact crater.

Polymict and monomict breccias were observed at the edges of these craters but they don’t form big masses because of erosion. They consist of irregular fragments with millimeter and centimeter sizes, in a carbonate matrix. In the breccias collected on the southern edges of the Isli crater, we noted the presence of several shocked quartz grains in planar structures associated with rolling extinction, indicators of shock metamorphism. 

This gorgeous specimen displays very well with a mass of 35x35x25 mm. Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

This is a fantastic Impactite Fallback Breccia from Germany weighing 32.9 grams and measuring 70x48x7mm. 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.

Pseudomorphs are mineral specimens that have the external shape of one mineral but are composed of another.  The pseudomorph goethite after marcasite forms when marcasite is exposed to oxidizing conditions and starts to oxidize and break down. As the marcasite breaks down, goethite replaces it in the crystal structure, preserving the shape of the original marcasite crystal. The resulting specimen appears as a marcasite crystal, but is actually composed of goethite.

The Farafra Oasis, in the White Desert, has been known for a number of years to deliver incredible pseudomorph specimens. The pseudomorphs occur within the Cretaceous Khoman Chalk, from which the White Desert derives its name.

This specimen is remarkable for its relatively sharp marcasite crystal form.  It is in excellent condition.  

Name: Goethite After Marcasite Pseudomorph
Specimen Size:  Miniature-Sized Specimen
Dimensions:  27x24x21 mm / 1.1x0.9x0.8 inches
Weight: 20.8 grams / 0.7 ounces
Origin: White Desert, Farafra Oasis, Egypt

This is a must have 27.4 gram Impact Melt Rock from the Stac Fada Member Impact Structure, NW Scotland. It measures 67x37x5 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 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 beautiful Impact melt rock comes from the Stac Fada impact structure in Scotland. The structure has an estimated age of about 1.2Ga (1,200 Ma). The Stac Fada Member of the Precambrian Stoer Group in Scotland has previously been described as volcanic in origin. However, shocked quartz and biotite provide evidence for high-pressure shock metamorphism, while chromium isotope values and elevated abundances of platinum group metals and siderophile elements indicate addition of meteoritic material. Thus, the unit is reinterpreted as having an impact origin.

This gorgeous slice displays very well.  Would be a beautiful addition to any new or existing collection. Comes with two a Canagem Collection specimen card.

This is a superb looking slice of a Sahara Desert NWA unclassified meteorite weighing 7.47 grams. Its dimensions are 26x20x6 mm.  This never classified North West Africa stone was found in the Sahara desert in 2004.

It's a very good quality cut NWA meteorite specimens showing excellent internal structure (L5?) and are very attractive with light grey mottled interior with chondrules and metallic flakes. Low weathering grade. Display nicely.

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

This is a fantastic Impactite Fallback Breccia from Germany weighing 52 grams and measuring 69x51x10mm. 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 must have 4.71 gram impactite from the Boltysh Crater in Ukraine.  Its dimensions are 28x27x4mm.  Although not a meteorite, impactites are directly linked to them and their impacts and are probably going to be one of the rarest collection pieces you'll ever own. The Boltysh impactites are important geological specimens that are recognized by the scientific community as evidence of asteroid or comet impacts on Earth.

The Boltysh crater is a well-preserved impact crater located in central Ukraine. It was formed approximately 65 million years ago during the Late Cretaceous period, around the same time as the Chicxulub impact that is thought to have caused the mass extinction of the dinosaurs. The crater is estimated to be around 24 kilometers in diameter and is one of the best-preserved impact structures in the world.

The Boltysh crater has been extensively studied by scientists because of its importance in understanding the effects of large-scale impacts on the Earth's surface and the resulting environmental changes that occur. Studies of the rocks and sediments from the crater have provided valuable insights into the processes of impact cratering, such as the formation of impact melt rocks and the creation of shock metamorphic features.

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

This is a must have 16.88-gram Impactite slice from the Terny Astrobleme (Ukrainian Shield) in Cherkasy Region of Ukraine. Its dimensions are 53x32x8mm.  Although not a meteorite, impactites are directly linked to them and their impacts and are probably going to be one of the rarest collection pieces you'll ever own. The Terny impactites are important geological specimens that are recognized by the scientific community as evidence of asteroid or comet impacts on Earth.

The Terny astrobleme is a geological formation located in the Cherkasy region of Ukraine. It is believed to be the result of a meteorite impact that occurred approximately 65 million years ago during the Late Cretaceous period. The impact formed a crater that is estimated to be around 6 kilometers in diameter, although it is largely eroded and filled in with sediment.

It is an important geological site for studying the effects of meteorite impacts on the Earth's surface and the resulting geological processes that occur. It has been the subject of numerous scientific studies, and specimens of the impactite rocks found at the site have been collected and analyzed for their mineralogical and chemical properties.

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

Product Type: Olive Quartz
Approx Weight (per piece): 1.08ct 
Size: 8x6mm 
Shape: Oval Cut
Color:  Golden 
Clarity:   Clean
Origin:   Africa

Pseudomorphs are mineral specimens that have the external shape of one mineral but are composed of another.  The pseudomorph goethite after marcasite forms when marcasite is exposed to oxidizing conditions and starts to oxidize and break down. As the marcasite breaks down, goethite replaces it in the crystal structure, preserving the shape of the original marcasite crystal. The resulting specimen appears as a marcasite crystal, but is actually composed of goethite.

The Farafra Oasis, in the White Desert, has been known for a number of years to deliver incredible pseudomorph specimens. The pseudomorphs occur within the Cretaceous Khoman Chalk, from which the White Desert derives its name.

This specimen is remarkable for its relatively sharp marcasite crystal form.  It is in excellent condition.  

Name: Goethite After Marcasite Pseudomorph
Specimen Size:  Miniature-Sized Specimen
Dimensions:  40x34x35  mm / 1.6x1.3x1.4 inches
Weight: 44.4 grams / 1.6 ounces
Origin: White Desert, Farafra Oasis, Egypt

Wavellite typically forms as radiating, spherical clusters or botryoidal (grape-like) aggregates, often appearing as green, yellow, brown, or even blue clusters on a host rock. The mineral typically forms in low-grade metamorphic rocks and phosphate-rich environments, often associated with minerals like quartz, variscite, and limonite.

Wavellite is found in several locations worldwide, with Arkansas, USA being one of the most famous sources, producing well-formed green botryoidal specimens. Other notable locations include England, Bolivia, Brazil, Germany, and Australia.

It is believed wavellite is linked to clarity, insight, and emotional balance, helping to provide a broader perspective on situations. It is sometimes associated with the heart chakra, thought to encourage compassion and emotional healing. 

Name: Wavellite on Matrix  
Specimen Size:  Miniature-Sized
Dimensions: 59x45x31 mm / 2.3x1.8x1.2 inches 
Weight: 71 grams / 2.5 oz
Origin: Mauldin Mountain, Mt. Ida, Arkansas, USA