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Goethite
Goethite
Goethite
Goethite

Goethite

Goethite

A species of Diaspore Group, Also known as Limonite, Braun-Eisenstein, Brown Iron Ore, Chileit (of Breithaupt), Ehrenwerthite (of Cornu), Götheite, Mesabite, Yanthosiderite, Needle Ironstone

The primary interest in goethite is as an ore of iron; it is otherwise not very attractive as a mineral specimen. High concentrations of goethite have been found in the United States; other, less significant finds have been spotted in Mexico and Canada.

Hardness
Hardness:

5 - 5.5

Density
Density:

4.18 g/cm³

General Info About Goethite

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Physical Properties of Goethite

Luster
Metallic, Silky, Adamantine
Diaphaneity
Opaque
Colors
Brownish black, yellow-brown, reddish brown
Magnetism
Magnetic
Tenacity
Brittle
Cleavage
Perfect
Fracture
Uneven
Streak
Yellowish brown, orange-yellow, ocher-yellow
Crystal System
Orthorhombic
Hardness
5 - 5.5 , Soft
Density
4.18 g/cm³, Obviously Heavy Weight
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Chemical Properties of Goethite

Chemical Classification
Oxides
Formula
α-Fe3+O(OH)
Elements listed
Fe, H, O
Common Impurities
Mn

Optical Properties of Goethite

Refractive Index
2.26-2.398
Birefringence
0.138
Pleochroism
Visible
Optical Character
Biaxial negative

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Rarity
Uncommon

Characteristics of Goethite

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Formation of Goethite

Goethite often forms through the weathering of other iron-rich minerals, and thus is a common component of soils, concentrated in laterite soils. nanoparticulate authigenic goethite is a common diagenetic iron oxyhydroxide in both marine and lake sediments. The formation of goethite is marked by the oxidation state change of Fe (ferrous) to Fe (ferric), which allows for goethite to exist at surface conditions. Because of this oxidation state change, goethite is commonly seen as a pseudomorph. As iron-bearing minerals are brought to the zone of oxidation within the soil, the iron turns from iron(II) to iron(III), while the original shape of the parent mineral is retained. Examples of common goethite pseudomorphs are: goethites after pyrite, goethite, siderite, and marcasite, though any iron(II)-bearing mineral could become a goethite pseudomorph if proper conditions are met. It may also be precipitated by groundwater or in other sedimentary conditions, or form as a primary mineral in hydrothermal deposits. Goethite has also been found to be produced by the excretion processes of certain bacteria types.

Composition of Goethite

Goethite is an iron oxyhydroxide containing ferric iron. It is the main component of rust and bog iron ore. Goethite's hardness ranges from 5.0 to 5.5 on the Mohs Scale, and its specific gravity varies from 3.3 to 4.3. The mineral forms prismatic needle-like crystals ("needle iron ore") but is more typically massive. Feroxyhyte and lepidocrocite are both polymorphs of the iron oxyhydroxide FeO(OH) which are stable at the pressure and temperature conditions of the Earth's surface. Although they have the same chemical formula as goethite, their different crystalline structures make them distinct minerals. Additionally, goethite has several high-pressure and high-temperature polymorphs, which may be relevant to the conditions of the Earth's interior. These include ε-FeOOH, which has an orthorhombic crystal structure, a cubic pyrite-type polymorph with or without losing hydrogen and an ultradense hexagonal structure.

Cultural Significance of Goethite

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Uses of Goethite

Goethite is a diaspore mineral which has been used for hundreds of years as a source for brown and yellow ochre paint. It is also important as an iron ore, from which iron can be extracted. Some particularly beautiful and rare types are desired by collectors, or cut into cabochons for use in jewelry.

The Meaning of Goethite

Goethite's oldest use comes from the ancient Phrygia. A body was found in a royal tomb believed to the father of King Midas. The burial shroud was colored with a dye containing goethite, making the shroud look golden. Historians conjecture that King Midas' golden touch legend may have started from Phrygian royalty wearing such golden-colored clothes.

Distribution of Goethite

Goethite is found all over the planet, usually in the form of concretions, stalactitic formations, oolites (a form consisting of tiny round grains cemented together), reniform (kidney shapes) or botryoidal (globular, like bunches of grapes) accumulations. It is also a very common pseudomorph. It is frequently encountered in the swampy areas at the head of spring waters ('bog iron'), on cave floors, and on the bottom of lakes and small creeks. The boxworks or gossan resulting from the oxidation of sulfide ore deposits is formed of goethite along with other iron oxides and quartz. Significant deposits of goethite are found in England, Australia, Cuba, and Michigan, Minnesota, Missouri, Colorado, Alabama, Georgia, Virginia, and Tennessee, and Florida caves in the United States. Deposits significant in location, if not in abundance, have been found in the Martian crater Gusev by NASA's Spirit rover, providing strong evidence for the presence of liquid water on the planet in an earlier stage of its evolution. In 2001, John Emsley, in his book "Nature's Building blocks", reported that limpet's teeth are made of goethite (pg. 210). In 2015 it was reported that limpet's teeth have goethite fibres in them, which accounts for their extreme tensile strength.

Etymology of Goethite

It was first described in 1806 based on samples found in the Hollertszug Mine in Herdorf, Germany. The mineral was named after the German polymath and poet Johann Wolfgang von Goethe (1749–1832).

Healing Properties of Goethite

Goethite is an excellent stone to help with feelings of grief, as this stone's strong vibration can help heal emotional wounds. It has a deep connection to earth and will provide grounding especially for those who are driving in a car all day. Meditating with the stone opens the door to positive energy and if allowed it will fill one's heart with love and passion.
Chakras
Root, Sacral, Third Eye

Common Questions People Also Ask

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