World Library  
Flag as Inappropriate
Email this Article


Article Id: WHEBN0001253157
Reproduction Date:

Title: Dickite  
Author: World Heritage Encyclopedia
Language: English
Subject: Kaolinite, Phyllosilicates, Illite, Chlorite group, WikiProject Rocks and minerals/Worklist
Collection: Aluminium Minerals, Clay Minerals Group, Monoclinic Minerals, Phyllosilicates
Publisher: World Heritage Encyclopedia


Category Phyllosilicates
Kaolinite-serpentine group
(repeating unit)
Strunz classification 09.ED.05
Dana classification
Crystal symmetry Monoclinic domatic
H-M symbol: (m)
Space group: Cc
Unit cell a = 5.150 Å, b = 8.940 Å, c = 14.424 Å; β = 96.8°; Z=4
Color White, with coloration from impurities
Crystal habit Pseudohexagonal crystals, aggregates of platelets and compact massive
Crystal system Monoclinic
Cleavage Perfect on {001}
Tenacity Flexible but inelastic
Mohs scale hardness 1.5 - 2
Luster Satiny to pearly
Streak White
Diaphaneity Transparent
Specific gravity 2.6
Optical properties Biaxial (+)
Refractive index nα = 1.561 - 1.564 nβ = 1.561 - 1.566 nγ = 1.566 - 1.570
Birefringence δ = 0.005 - 0.006
2V angle Measured: 50° to 80°
References [1][2][3][4][5][6][7][8][9][10][11]

Dickite (Al2Si2O5(OH)4) is a phyllosilicate clay mineral chemically composed of aluminium, silicon, hydrogen and oxygen contributing 20.90%, 21.76%, 1.56%, and 55.78% each respectively. It has the same composition as kaolinite, nacrite, and halloysite, but with a different crystal structure (polymorph). Dickite sometimes contains impurities such as titanium, iron, magnesium, calcium, sodium and potassium.[2]

Dickite occurs with other clays and requires x-ray diffraction for its positive identification. Dickite is an important alteration indicator in hydrothermal systems as well as occurring in soils and shales. It takes its name from Allan Brugh Dick (1833–1926), the Scottish metallurgical chemist who first described it.

Dickite’s type location is in Pant-y-Gaseg, Amlwch, Isle of Anglesey, Wales, UK, where it was first described in 1888.[2] Dickite is scattered across Wales forming occurrences in vein assemblages and as a rock forming mineral. Another occurrence spot, as indicated by Brindley and Porter of the American Mineralogists journal, is the Northerly dickite-bearing zone in Jamaica. The dickite in this zone ranges from indurate breccias containing cream to pinkish and purplish fragments composed largely of dickite with subordinate anatase set in a matrix of greenish dickite, to discrete veins and surface coatings of white, cream and translucent dickite. It appears that dickite in the northerly zone were formed by hot ascending waters from an uncertain origin. Dickite occurrence is well spread among countries like China, Jamaica, France, Germany, UK, USA, Italy, Belgium and Canada.[11]

Dickite has a monoclinic crystal system and its crystal class is domatic (m). This crystal system contains two non-equal axes (a and b) that are perpendicular to each other and a third axis (c) that is inclined with respect to the an axis. The a and c axes lie in a plane. Dickite involves an interlayer bonding with at least 3 identifiable bonds: an ionic type interaction due to net unbalanced charges on the layers, van der waals forces between layers and hydrogen bonds between oxygen atoms on the surface of one layer and hydroxyl groups on the opposing surface. A hydrogen bond, as the term is used here, involves a long range interaction between hydrogen of a hydroxyl group coordinated to a cation and an oxygen atom coordinated to another cation. The reaction is predominantly electrostatic; hence an ionic bonding model is appropriate. Its axial ratio is a=0.576, b=1, c=1.6135.

Dickite has perfect cleavage in the (001) direction. Its color varies from blue, gray, white to colorless. It usually has a dull clay-like texture. Its hardness on the Mohs scale is 1.5-2, basically between talc and gypsum. This is attributed to its loose chemical bonds. It is held with hydrogen bonds, which are otherwise weak. It leaves a white streak and it has a pearly luster. It has a density of 2.6. Dickite is biaxial, its birefringence is between 0.0050-0.0090, its surface relief is low and it has no dispersion. The plane of the optical axis is normal to the plane of symmetry and inclined 160, rear to the normal to (0,0,1).


  • Composition 1
  • Geologic occurrence 2
  • Structure 3
  • Physical properties 4
  • History 5
  • References 6


Al2Si2O5(OH)4 is the chemical formula of dickite. The calculated percent abundances are very close when compared to other kaolin minerals.

Chemical composition of dickite:[6]

  • SiO₂ 46.54%
  • Al₂O₃ 39.50%
  • H₂O 13.96%

Dickite and other kaolin minerals are commonly developed by weathering of feldspars and muscovite.[6] Through its evolution, dickite, a phyllosilicate mineral, maintains the aluminium and silicon elements influencing the formation of hexagonal sheets common to clay minerals. The problem of mistaken identity arises when comparing dickite to other kaolin minerals due to the fact that kaolinite, dickite, and nacrite all have the same formula but different atomic structures. The only way to determine the true identity of the mineral is through powdered x-ray diffraction and optical means.

Geologic occurrence

In 1888 Allan B. Dick discovered what we now know to be dickite. He discovered this mineral in volcanic rock.[10] An extensive study was done on dickite pertaining to its location in Pennsylvanian limestones of southeastern Kansas. According to Richard J. Schroeder and John B. Hayes, dickite distribution is dependent on the following: the stratigraphic alternation of limestones and shales, westward regional dip, thick deposits of highly porous algal limestones, and igneous intrusions. It was found that groundwaters substantially heated along with magmatic waters which made its way up-dip and through the intrusions in the conduit-like algal mounds which allowed the dickite to be deposited in this area and it might be conclusive to say that this trend follows elsewhere in other locations around the world.[8]


The hexagonal network of Si-O tetrahedra along with the superimposed layer of Al-O, OH octahedra make up the kaolin layer found in dickite. Dickite is composed of regular sequences of one, two and six kaolin layers. Analysis of the dickite structure reveals the space group to be C4s-Cc. The a and c axis both lie on the glide plane of symmetry.[9] Dickite’s structure is made up of a shared layer of corner-sharing tetrahedra filled by a plane of oxygens and hydroxyls along with a sheet of edge-sharing octahedra with every third site left empty.[6] An experiment was conducted using a pseudo-hexagonal crystal of dickite to determine the unit cell information and the layers that exist within dickite. It was found that there are six layers within the kaolin layer within dickite. This is evidenced in the following findings. There is an oxygen atom from the all oxygen layer that lies at the center. The atoms of the O layer, the Si layer and the O, (OH) layer are situated for the ideal kaolin layer.[9] X-ray experiments were performed by C. J. Ksanda and Tom F. W. Barth and it was concluded that dickite is composed of tiny layers of cations and anions which are parallel to the a-b plane stacked on top of one another which they found to be exactly as Gruner had described. It was also concluded that the two dimensional arrangement of some of the atoms are not as Gruner described.[5]

Physical properties

The atomic structure of dickite, being very similar to that of kaolinite and other kaolin type minerals, has a very specific arrangement that differs slightly enough to set its physical appearance and other physical properties apart from that of its family members kaolinite and nacrite. In a comparison of the family of minerals through experiments examined by Ross and Kerr the similarities between them are clearly evident and can, depending on the samples, be indistinguishable by optical means.[4]

The hexagonal structure and the stacking of the atoms influence the physical properties in many ways including the color, hardness, cleavage, density, and luster. Another important factor in influencing physical properties of minerals is the presence of bonding between atoms. Within dickite there exists dominant O-H bonding, a type of strong ionic bonding.[9] Dickite takes on the appearance of a white, brown earthy color and is often found embedded in many other minerals such as quartz.


The history of dickite began before it was known by its name that was given by Clarence S. Ross and Paul F. Kerr. In 1888 Allan Dick, a metallurgical chemist, was on the island of Anglesey conducting research on kaolin. He performed various experiments describing the mineral.[7] It was not until 1931 that Ross and Kerr looked closer at the mineral and concluded that it was different from the known minerals of kaolinite and nacrite.


  1. ^ Handbook of Mineralogy
  2. ^ a b c
  3. ^ Webmineral data
  4. ^ a b Dick, Allan B., On Kaolinite: Mineral Mag., vol. 8, pp 15–27, 1888.
  5. ^ a b Ksanda, C. J. and Barth, F.W., Note on the structure of Dickite and other clay minerals: American Mineralogist, vol. 19, pp. 557-575, 1934.
  6. ^ a b c d Cruz, Maria Dolores Ruiz. Genesis and evolution of the kaolin-group minerals during the diagenesis and The beginning of metamorphism.
  7. ^ a b Ross, C.; Kerr, P.F. (1931). "Dickite, a Kaolin Mineral" (PDF). American Mineralogist 15: 34–39. 
  8. ^ a b Schroeder, Richard J., Hayes, John B. (1968) Dickite and Kaolinite in Pennsylvanian Limestones of Southeastern Kansas. Clays and clay minerals, vol. 16, 41-49.
  9. ^ a b c d Newnham, R.E., Brindley, G.W. (1956) The Crystal Structure of Dickite. Acta Crystal, vol. 9, p. 759.
  10. ^ a b Ker, P.F., Main, M.S., Hamilton, P.K. (1951) Occurrence and microscopic examination of reference clay Minerals specimens. Preliminary reports Reference Clay Minerals American Petroleum Institute Research Project 4. Columbia University. New York 1949.
  11. ^ a b Brindley, G. W. and Porter, R. D. (1975) Occurrence of dickite in Jamaica-ordered and disordered varieties: American Mineralogists, vol. 63, pp. 554-562, 1978.
  • Dickite stability PDF
This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.

Copyright © World Library Foundation. All rights reserved. eBooks from World Library are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.