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This is a fantastic Impactite Fallback Breccia from Germany weighing 33.3 grams and measuring 65x49x8mm. 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 great 22 gram Impact Melt Breccia from the Gardnos Crater in Norway.  It is amazingly light considering its mass of 56x28x9mm. 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.

This impactite was formed between 385 and 900 million years ago in Precambrian time when a meteorite crashed into the earth making a ~5 kilometers wide crater locally known as the Hallingdal Impact Crater. 

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

This amazing specimen of Vesuvianite was collected in the now closed Jeffery Mine in Asbestos, Québec, Canada. The specimen is made up of a combination of green and mauve vesuvianite crystals also named violet manganoan vesuvianite. It is a large specimen in good condition. A great addition to any collection!

Vesuvianite was first discovered on Mount Vesuvius in Italy in the 18th century, hence its name. It typically occurs as a green, brown, yellow, or blue-green crystal, and is often found in metamorphic and igneous rocks. The alternate name, Idocrase, is from the Greek eidos “form”, and krasis “mixture”, because Vesuvianite often appears to combine the crystal forms of other minerals. It is used as a gemstone.

Name: Vesuvianite Crystal 
Specimen Size:  Miniature-Sized
Dimensions: 34x20x13 mm / 1.3x0.8x0.5 inches 
Weight: 10.74 grams / 0.4 ounces 
Origin: Mined in Jeffery Mine,  Asbestos, Québec, Canada

This is a must have 20.3 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 59x34x8mm.  Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

This is a rare and fantastic 8.5 gram Libyan Desert Glass from Kuffra, Libya, with dimensions of 32x18x17 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.  Characterized by its yellow to greenish-yellow color, it lacks the aerodynamic shapes of tektites and often appears as irregularly shaped pieces. It is almost pure silica (around 98%) with very few impurities. Throughout history, it has been regarded as a mystical and powerful material, sometimes used in talismans and amulets.

This piece displays extremely well and is a quality translucent specimen. It has an aesthetic shape with a beautiful wind eroded body from the years spent in the Desert. Would be a beautiful addition to any new or existing collection. Comes with a Canagem Collection specimen card.

Vanadinite crystals are small, hexagonal prismatic crystals that are typically red to brownish-red in color. They have a bright luster and a transparent to translucent appearance. The crystals often form in aggregates, creating intricate and interesting formations.  Vanadinite would hardly be as famous if not for the outstanding locality of Mibladen, Morocco. This locality has by far produced the most outstanding crystals of beautiful color and form. 

Vanadinite is believed to enhance vitality, motivation, and manifestation, while also promoting clarity, focus, and protection from negativity.

Product Type: Vanadinite Crystal On Barite 
Specimen Size:  Miniature-Sized
Dimensions: 45x34x23 mm / 1.8x1.3x.09 inches
Weight: 29.56 grams / 1.0 ounces
Origin: Mibladen, Morocco

While it's commonly colorless or white, Calcite can also appear in various hues, including shades of green, blue, yellow, orange, red, brown, and even black.  This sphere is a beautiful example of yellow calcite.  The coloration is often due to impurities or exposure to different minerals during formation.  Calcite is typically transparent to translucent, allowing light to pass through and sometimes exhibit a phenomenon called double refraction.  is found throughout the world in sedimentary, metamorphic, and igneous rocks.

Calcite is associated with clarity, amplification of energy, and cleansing.  It is believed it can help with emotional healing, motivation, and creativity.

This is a nice looking individual fragment of a Sahara Desert NWA unclassified meteorite. It weighs 81.1 grams and measures 51x37x25 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 lovely pink Stilbite specimen from Parsboro, Cape d'Or, Nova Scotia, Canada. It was collected in 2002 and is a miniature size group of well terminated crystals with nice sharp edges. 

Stilbite is a zeolite mineral appreciated for its delicate crystal formations and pastel hues, ranging from colorless to white, yellow, pink, and peach.  It forms distinctive tabular crystals with a bowtie or butterfly shape and exhibits a vitreous to pearly luster. Commonly found in cavities in volcanic rocks, stilbite is often associated with other zeolite minerals. 

Stilbite is believed to have soothing and spiritually uplifting qualities, often associated with promoting emotional healing, inner peace, and mental clarity. Many consider it helpful for enhancing spiritual connection, deepening meditation, and supporting dream recall or lucid dreaming. Often linked to the heart chakra, it is thought to encourage love, compassion, and the release of emotional wounds. Stilbite may assist in navigating transitions, amplifying the energy of other crystals, and fostering a calming environment by shifting negative energy into positive vibrations.

Name: Stilbite Crystals
Specimen Size:  Miniature-Sized
Dimensions:  47x36x19 mm / 1.8x1.4x0.7 inches
Weight:  21.5 gr / 0.7 oz
Details: Mined in Cape D'Or, Nova Scotia, Canada

Peruvian pyrite is famous worldwide for its well-formed, highly lustrous crystals. The country is one of the top sources for high-quality pyrite specimens, particularly from the Huanzala Mine in the Áncash Region and the Quiruvilca Mine in La Libertad. These locations produce stunning pyritohedral crystals, often found in association with quartz, sphalerite, and galena.

The term “pyritohedral” refers to a specific crystal habit that pyrite (and occasionally other minerals) can form. In this structure, the crystal takes on a polyhedral shape with 12 faces. However, unlike a perfectly symmetrical shape with identical pentagonal faces, natural pyritohedral crystals often exhibit slight irregularities or distortions in their faces.

Pyrite is known as a stone of protection, abundance, and confidence.  It is believed to shield against negative energy and promote mental clarity and willpower. 

This top Peruvian specimen is in very good condition.  Would be a beautiful addition to any new or existing collection.

Name: Pyrite Cluster 
Specimen Size:  Cabinet-Sized
Dimensions: 66x47x34 mm / 2.6x1.8x1.3 inches 
Weight: 194 Grams / 6.8 oz
Origin: Mined in Quiruvilca Mine, Quiruvilca District, Santiago de Chuco Province, La Libertad, Peru

This specimen shows a group of well-shaped emerald-green dioptase crystals on pearly white calcite crystals . Dioptase is an uncommon copper mineral prized for its intense green colour. It is found in only a few copper mines world-wide, but the best examples come from Tsumeb, Namibia.

The Tsumeb Mine, one of the most famous mineral localities globally, produced dioptase with deep green hues, high clarity, and sharp crystal formations. Unlike dioptase from other locations, Tsumeb specimens often occur on a contrasting white calcite matrix, enhancing their visual appeal.

The Tsumeb Mine in Namibia is no longer actively producing dioptase. The mine, which was one of the world’s most famous mineral localities, ceased large-scale operations in the 1990s. While some minerals can still be found from old stockpiles, no new dioptase specimens are being extracted from the mine today.  This makes Tsumeb dioptase highly collectible, as no fresh supply is entering the market. Existing specimens, especially those with deep color, good transparency, and well-formed crystals on matrix, are increasingly rare and valuable among collectors

Dioptase is often associated with emotional healing, forgiveness, and heart chakra energy. Some believe it encourages letting go of past wounds and embracing compassion. It is also thought to promote inner clarity and transformation, making it popular for personal growth and emotional balance.

Name: Dioptase on Calcite Crystal
Specimen Size:  Cabinet-Sized
Dimensions:  65x50x38 mm / 2.6x2.0x1.5 inches
Weight: 116.72 Grams / 4.1 oz
Origin: Tsumeb Mine, Otavi, Namibia

This is a fantastic Impactite Fallback Breccia from Germany weighing 66 grams and measuring 74x53x9mm. 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.