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Dacite

Dacite

A species of Igneous

Dacite is a relatively common volcanic rock that can be found in several different hues. Ancient people sometimes used dacite in place of flint to create spears or arrowheads. The rock’s name is derived from “Dacia”, the ancient Roman province near modern Romania, where it was first described. Today, the stone is crushed and used as filler in construction projects.

Hardness
Hardness:

6 - 7

Density
Density:

2.5 - 2.8 g/cm³

General Info About Dacite

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Physical Properties of Dacite

Texture
Aphanitic, Porphyritic
Colors
Bluish-grey, brown, light to dark grey, white, yellow, etc.
Magnetism
Potentially Magnetic
Grain Size
Fine to coarse grained
Hardness
6 - 7 , Hard
Density
2.5 - 2.8 g/cm³, Normal Weight
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Chemical Properties of Dacite

Silica (SiO2) Content
63%-69%

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Rarity
Uncommon

Characteristics of Dacite

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Formation of Dacite

Dacite usually forms as an intrusive rock such as a dike or sill. Examples of this type of dacite outcrop are found in northwestern Montana and northeastern Bulgaria. Nevertheless, because of the moderately high silica content, dacitic magma is quite viscous and therefore prone to explosive eruption. A notorious example of this is Mount St. Helens in which dacite domes formed from previous eruptions. Pyroclastic flows may also be of dacitic composition as is the case with the Fish Canyon Tuff of La Garita Caldera.

Composition of Dacite

Dacite consists mostly of plagioclase feldspar with biotite, hornblende, and pyroxene (augite and/or enstatite). It has quartz as some rounded, corroded phenocrysts, or as an element of the ground-mass.

Cultural Significance of Dacite

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Uses of Dacite

Dacite can be used as a filler rock when paving and constructing roads, though it is not a popular choice due to its high silica content that may easily damage or weather. It may also be used for decorative purposes or stone carvings.

Distribution of Dacite

Dacite is relatively common and occurs in various tectonic and magmatic contexts: In oceanic volcanic series. Examples: Iceland (Heiðarsporður ridge), Juan de Fuca Ridge In limestone-alkaline and tholeiitic volcanic series of the subduction zones of island arcs and active continental margins. Examples of dacitic magmatism in island arcs are Japan, the Philippines, the Aleutians, the Antilles, the Sunda Arc (Mount Batur), Tonga and the South Sandwich Islands. Examples of dacitic magmatism in active continental margins are the Cascade Range, Guatemala and the Andes (Ecuador and Chile). In continental volcanic series, often in association with tholeiitic basalts and intermediary rocks. Sites of dacite in Europe are Germany (Weiselberg in the Saarland), Greece (Nisyros and Thera), Italy (in Bozen quartz porphyry, and Sardinia), Austria (Styrian Volcano Arc), Romania (Transylvania), Scotland (Argyll), Slovakia, Spain (El Hoyazo near Almería), France (Massif de l'Esterel) and Hungary (Csódi Hill). Sites outside Europe include Iran, Morocco, New Zealand (volcanic region of Taupo), Turkey, USA and Zambia. Dacite is found extraterrestrially at Nili Patera caldera of Syrtis Major Planum on Mars.

Common Questions People Also Ask

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