Hornfels

A variety of Metamorphic

Uncommon

What is Hornfels?

Hornfels is the name of a group of attractive-looking crystalline metamorphic rocks primarily used in architecture as beautification stones — they are used for interior floors, facades, and/or pavings. With the ability to resonate when struck, they were used for making lithopones (musical instruments) back in the 19th century in England.

Uses & Applications

Hornfels is a metamorphic rock that is commonly used as a tough but eye-catching material in the building industry. It can be used to produce paving and curbstones as well as for indoor tiling. This rock can also be ground down to produce aggregate for covering road surfaces.

Healing Properties

Are you looking to increase your mental capability? Hornfels is said to do just that, making you better able to manage difficulties and more courageous when approaching risks. It's also said to bring good luck! Healers believe that this stone diminishes negative emotions, spreading positivity and love throughout your whole body. Using this stone as an amulet may keep evil spirits away.

Hornfels Market Value Calculator

Estimate the market value of Hornfels using size, quality, and finish. This preview calculator is for quick context and is not a formal appraisal.

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Hornfels Localities Map

See where Hornfels is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.

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North ZoneCentral RidgeSouth Basin

Interactive map layers and collecting notes are available in the app.

Key Characteristics

Characteristics of Hornfels

Hornfels have the ability to resonate when struck. Michael Tellinger had described these stones in South Africa also known as "ring-stones" due to their ability to ring like a bell. The Musical Stones of Skiddaw are an example of a lithophone made from hornfels.

Composition of Hornfels

The structure of the hornfels is very characteristic. Very rarely do any of the minerals show crystalline form, but the small grains fit closely together like the fragments of a mosaic; they are usually of nearly equal dimensions. This has been called pflaster or pavement structure from the resemblance to rough pavement work. Each mineral may also enclose particles of the others; in the quartz, for example, small crystals of graphite, biotite, iron oxides, sillimanite or feldspar may appear in great numbers. Often the whole of the grains are rendered semi-opaque in this way. The minutest crystals may show traces of crystalline outlines; undoubtedly they are of new formation and have originated in situ. This leads us to believe that the whole rock has been recrystallized at a high temperature and in the solid state so that there was little freedom for the mineral molecules to build up well-individualized crystals. The regeneration of the rock has been sufficient to efface most of the original structures and to replace the former minerals more-or-less completely by new ones. But crystallization has been hampered by the solid condition of the mass and the new minerals are formless and have been unable to reject impurities, but have grown around them.

Quick Facts

Physical Properties

Color
Black, brown, greenish gray, etc.
Hardness (Mohs)
5
Density
2.5 - 3 g/cm³
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