Let us look at some of mother nature’s most beautiful Minerals and Crystals.


Who is the most outstanding creator you have ever seen? At the moment, many names have to be popping up in your brain. But it’s not any of those personalities. It’s nature.

The landscapes, peaks, streams, rivers, and waterfalls are breathtaking. Although, because the smaller items are concealed underground and are not immediately visible, we tend to overlook them. So you may be thinking, what are the small things? It’s nothing but the Crystals and minerals with startling and distinctive beauty.

Do you realize the distinction between a crystal and a mineral, though? Maybe you may have been thinking there’s no difference at all.

Any solid with a well-organized structure is referred to as a crystal; This implies that the atoms are spaced at exact distances and angles from one another. Minerals are inorganic compounds with crystalline forms that exist naturally. As a result, becoming a crystal is necessary for becoming a mineral. Nevertheless, all minerals can be considered to form crystals.

We’ve produced a list of some of the most fascinating minerals among the world’s around 4000 naturally occurring minerals. So let us have a watch at 18 of the most stunning crystals and minerals for your viewing pleasure.

Crystals of olivenite

Credit: Tóth László

Olivenite is a copper arsenate mineral with a monoclinic crystallization structure. Conichalcite was used to create the item in this shot. In transmitted light, it is an olive-green hue that ranges in tone from yellow or brown to grey-green, greyish-white, or pale green. Olivenite is most typically found as globular clusters of acicular crystals, with these fibrous forms having a smooth gloss; it can also be lamellar or soft and earthy in appearance.

Stone of agate

Credit: CrystalWerkz (pinterest)

Agate is a prominent stone structure in the chalcedony group that belongs to the quartz family. This rock formation is found in the volcanic rocks worldwide, where they fill veins and crevices. Agate also comes in a range of colours. A lace-like pattern with shapes like eyes, spirals, bands, and zigzags can be seen in Lace agate. The stone is a member of the Agate family and is commonly red and white in hue. Although it can also be yellow or grey in appearance. Brazil, India, and the United States are now the world’s top agate producers.

Agate (Grape)

Credit: @amarisland

The scientific name for this material is Botryoidal Purple Chalcedony, whereas the marketing term is Grape Agate. Botryoidal refers to circular, tiny sphere-shaped crystals that have grown together spontaneously. The term “Grape Agate” refers to the purple hue of the stones and the fact that they are found in clusters that resemble grape bunches. These “grapes” are small, ranging from 2 to 8 mm across, and come in various hues, including white, grey, green, and blue.

Fluorite rainbow

Credit: Ryan Gooding

Fluorite (sometimes known as fluorspar) is a calcium fluoride mineral. Fluorite is colourless and transparent in visible and ultraviolet light, but impurities cause it to appear as a multicoloured mineral. Rainbow Fluorite is a colourful crystal combining hues in Fluorite crystals, such as purple, blue, green, transparent, and yellow. It has a striped appearance and fluctuates in transparency from translucent to opaque.

Apophyllite found on Stilbite host

Credit: Mineral Wonders

Apophyllite is a phyllosilicate mineral group. It comes from the Greek word “Apophylliso,” which means “it flakes off,” referring to the tendency of this class to flake apart when heated owing to water loss. Apophyllite is typically found in basalt or other volcanic rock vesicles as secondary minerals. Samples of this mineral are found in Jalgaon, India, the Harz Mountains of Germany, Mont Saint-Hilaire, Kongsberg, Norway, and Canada.


Credit: Tóth László

Clinoclase is an uncommon secondary copper mineral that forms acicular crystals over copper sulfide deposits in the cracked weathering zone. Concerning the inclined cleavage planes, it is termed after the Greek terms “Klino”, which means “incline”, and “Plasma”, which means “fraction.” Clinoclase is a vitreous, transparent dark blue to dark greenish-blue or greenish-black material that looks blue-green in transmitted light. The material is needle-like or tabular as rosettes and radial fibrous round aggregates as crusts, coatings, and crystals.

Agate of the Red Fox

Red Fox Agate is an uncommon and geologically distinct geode thought to be of volcanic origin from a distant section of the Argentinean Andes. Botryoidal Hematite makes up the inner bubbling surface, encircled with agate. The crystal’s outer layer is UV reactive, and when exposed to fluorescent lights, it glows a lime green hue.


Credit: László Kupi (finemineralphotography)

Aragonite is a carbonate mineral and one of nature’s three most prevalent crystal forms of calcium carbonate. Under fluorescent light, the sculpture in the photo exhibits Aragonite sprays in clay. It is normally found in Molina de Aragón, in the Region of Guadalajara, Castilla-La Mancha, Spain, and was named for it in 1797. Biological and physical activities, such as precipitation from fresh and saltwater ecosystems, contribute to its formation. Aragonite can be columnar or fibrous and can also come in spreading helictite forms known as flos-ferri (“iron flowers”).


Credit: Chinellato Matteo

Malachite is a kind that occurs in the oxidation region atop copper mines at shallow depths on the Earth. It is seldom discovered as a crystal, but when it is, the crystals are often acicular to tabular in form, brilliant green in colour, transparent, and lustrous. Malachite is a prominent pigment that has been used for thousands of years. This mineral may readily be crushed into a fine powder, making it the ideal resource for making powdered pigments. It was one of the first recognized green pigments for artwork use, and its hue does not fade with time or light exposure.

A cluster of smoky quartz

Credit: Chinellato Matteo

Smoky quartz is a dark kind of quartz that comes in various colours, from light grey to yellowish-brown to impenetrable black. It may be found in multiple places worldwide, but mainly in Brazil, Scotland (UK), and sections of the Swiss Alps, Australia, and Madagascar. Smoky quartz crystals range in clarity from very transparent to practically opaque brownish-grey to black. The inclusion of sodium and aluminium in its composition and the radiation of pale quartz, whereas the crystal is still growing in a semi-aqueous solution, give it its colour.

Veszelyite (green)

Veszelyite is an uncommon secondary copper and zinc mineral found in base metal deposits’ oxidation zones. Veszelyite crystals are commonly emerald-green, blue, or a combination of the two colours. They can be found in the form of tiny, glossy clusters spread over other minerals or crusts. They can occasionally be found as thick crystal aggregations. Veszelyite formations were discovered irregularly scattered throughout the Hemimorphite zone of the Palabanda Quarry in the Bouenza Department of the Republic of the Congo.

Radial Annabergite Crystals

Credit: Tóth László

Annabergite is an ascorbate mineral made up of a hydrous nickel arsenate that crystallizes mono clinically and is isomorphic with vivianite and erythrite. In 1852, Henry J. Brooke and William Hallowes Miller named it after Annaberg, Saxony, Germany, one of the co-type locations. Annabergite is a brilliant green mineral that can also be light grey, apple green, or white. When rich in cobalt, it can also be pale rose-red. Its distinctive hue may be easily identified, and it was once used to locate nickel-bearing ore veins. Other nickel minerals typically have a green alteration layer on them.


Wulfenite is a lead molybdate mineral that often appears as thin columnar crystals with a rectangular or octagonal form and a relatively small mid-section. It can also be found in the form of earthy, granular masses. Crystals can be brittle and delicate, and platy aggregates are common. Wulfenite’s hue ranges from brilliant orange-red to yellow-orange to brown, with the latter being the most common. It is sometimes called “yellow lead ore” in its yellow state. Wulfenite is named after Austrian mineralogist Franz Xavier von Wulfen (1728-1805).

Tourmaline (with Lepidolite)

A broad array of boron silicate minerals make up tourmaline. Although these minerals have a similar crystal structure and physical qualities, their chemical compositions are quite different. As a result, tourmaline comes in a broader range of hues and colour schemes than any other mineral. During the hydrothermal activity, large, well-formed crystals of tourmaline may develop in cavities and fractures, implying that when hot fluids and vapours transport the elements needed to make tourmaline into pockets, voids, and fractures, this creates an open environment for crystal formation.

Beryl (Red)

Credit: Arkenstone

The red hue of red beryl comes from trace levels of manganese. It is a short form of beryl. According to the Utah Geological Survey, one red beryl crystal is found for every 150,000 gem-quality diamonds. The creation of red beryl necessitates a particular geochemical environment, making it an uncommon mineral. To form red beryl, the elements beryllium, manganese, aluminium, silicon, and oxygen must all be present in sufficient quantities to include minerals; second, a source of manganese must be available at the same time and in the exact location; and third, the appropriate geochemical circumstances must prevail for beryllium, manganese, aluminium, silicon, and oxygen to crystallize into red beryl.


Credit: Arkenstone

Dioptase is a rare mineral found mainly in deserts that occurs as a subsequent mineral in the oxidation zone of copper sulfide mineral deposits. It ranges in hue from dazzling emerald-green to bluish-green, has a vitreous to sub-adamantine sheen, and is clear to translucent. Because this copper cyclosilicate mineral is so delicate, specimens must be cautiously handled. As a result, ultrasonic cleaning should never be used on it. Otherwise, the peaceful gem would fracture. Dioptase can also be used in painting as a ground pigment.

Obsidian Rainbow

Credit: Quinn Street

Rainbow Obsidian, also known as Heaven’s Eye, is a black or deep brown obsidian generated when molten lava flows to the surface from the Earth’s core and freezes into a stunning

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