Volcaniclastics are geologic materials composed of broken fragments (clasts) of volcanic rock.[1] These encompass all clastic volcanic materials, regardless of what process fragmented the rock, how it was subsequently transported, what environment it was deposited in, or whether nonvolcanic material is mingled with the volcanic clasts.[2] The United States Geological Survey defines volcaniclastics somewhat more narrowly, to include only rock composed of volcanic rock fragments that have been transported some distance from their place of origin.[3]
In the broad sense[2][4] of the term, volcaniclastics includes pyroclastic rocks such as the Bandelier Tuff;[5] cinder cones and other tephra deposits; the basal and capping breccia that characterize ʻaʻā lava flows; and lahars and debris flows of volcanic origin.[6]
Volcaniclastics make up more of the volume of many volcanoes than do lava flows. Volcaniclastics may have contributed as much as a third of all sedimentation in the geologic record.[2]
Classification of volcaniclastics
Volcaniclastics are composed of a range of pyroclastic detritus mixed with epiclastic sediments and formed in variable depositional environments.[7][8] Volcaniclastics include pyroclastic rock and tephra; volcanic autoclastic, alloclastic, and epiclastic materials; and fault gouge where faults displace volcanic rock.[2] All are defined below. These can be divided into primary volcaniclastics and secondary volcaniclastics (epivolcaniclastics).[9]
| Primary volcaniclastic deposits (Characteristic clasts must be more than 75% of volume) |
Secondary volcanic deposits (epivolcaniclastic deposits) |
|---|---|
|
Pyroclastic tuff or tephra (Pyroclastic deposit) |
Epiclastic deposits have more than 75% epiclasts in the general case. They are epivolcanicastic deposits if they have recognizable volcanic fragments in any proportion. |
Pyroclastic
Pyroclastic material is composed of rock fragments produced by explosive volcanism and erupted from the vent as individual particles,[1] without reference to the particle origin or the nature of the eruption.[2] These may include particles of country rock entrained within the vent.[10] Accumulations of pyroclastic material that have not been consolidated are described as tephra, while those that have undergone significant consolidation are described as pyroclastic rock.[2][11] Hydroclastic material is a special case of pyroclastic material produced by a variety of processes at magma-water interfaces.[1]
Autoclastic
Autoclastic volcanic material is produced by processes active during movement of solid or semisolid lava. These include rock fragments that are produced within volcanic vents but not extruded,[1] rock fragments produced by motion or gas explosions within volcanic flows, or rock fragments produced by gravitational collapse of lava domes or spines.[2] The characteristic basal and capping breccia of ʻaʻā lava flows[12] are autoclastic volcaniclastics.
Other kinds of volcaniclastic material
Alloclastic volcanic material is formed by fragmentation of existing igneous rock by subsurface igneous activity that may or may not involve magma intrusions. Fault gouge produced by motion along a fault in volcanic rock is also a type of volcaniclastic material.[2]
Epivolcaniclastics
Volcanic epiclastic material (epivolcaniclastics[13]) contains a substantial fraction of epiclasts (rock fragments produced by weathering and erosion) derived from volcanic rock.[2]
Mixed pyroclastic-epiclastic rocks
Deposits containing pyroclastic material that has been reworked in stream or lake environments or mingled with epiclastic material (whether volcanic or nonvolcanic) pose a special difficulty and are among the materials most usefully described simply as volcaniclastic.[14] A more specific classification is problematic for these cases.[11][15][16] The Espinaso Formation of New Mexico is an example of a rock unit that is composed of a complex mixture of pyroclastic and volcanic epiclastic material and so is described simply as volcaniclastic.[17] Another is the Washburn Group of the Yellowstone area, which includes debris flows of reworked volcanic ash and volcanic epiclastic rock.[18]
Mixed pyroclastic-epiclastic deposits may be classified by average clast size and percentage of pyroclastic material.[11]
| Pyroclastic | Tuffites (mixed pyroclastic-epiclastic) |
Epiclastic (volcanic or nonvolcanic) |
Average clast size (mm) |
|---|---|---|---|
| Agglomerate, agglutinate pyroclastic breccia | Tuffaceous conglomerate, tuffaceous breccia | Conglomerate, Breccia | > 64 |
| Lapillistone | 2 – 64 | ||
| Coarse ash tuff | Tuffaceous sandstone | Sandstone | 0.0625 – 2 |
| Fine ash tuff | Tuffaceous siltstone | Siltstone | 0.004 – 0.0625 |
| Tuffaceous mudstone, tuffaceous shale | Mudstone, shale | < 0.004 | |
| 75–100% pyroclasts | 25–75% pyroclasts | 0–25% pyroclasts |
See also
References
- ^ a b c d Fisher, Richard V. (1961). "Proposed classification of volcaniclastic sediments and rocks". Geological Society of America Bulletin. 72 (9): 1409. Bibcode:1961GSAB...72.1409F. doi:10.1130/0016-7606(1961)72[1409:PCOVSA]2.0.CO;2.
- ^ a b c d e f g h i Fisher, Richard V.; Schminke, H.-U. (1984). Pyroclastic rocks. Berlin: Springer-Verlag. ISBN 3540127569.
- ^ "Volcaniclastic". Volcanic Hazards Program. United States Geological Survey. 2012. Retrieved 28 September 2020.
- ^ Vincent, Pierre (2000). Volcaniclastic rocks, from magmas to sediments (PDF). Amsterdam, the Netherlands: Gordon and Breach Science Publishers. p. 1. ISBN 9056992783. Retrieved 28 September 2020.
- ^ Ross, Clarence S.; Smith, Robert L. (1961). "Ash-flow tuffs: Their origin, geologic relations, and identification". USGS Profession Paper Series. Professional Paper (366). doi:10.3133/pp366. hdl:2027/ucbk.ark:/28722/h26b1t.
- ^ Vincent 2000, pp.27-28
- ^ De Ros, L. F., S. Morad, and I. S. Al-Aasm, 1997, Diagenesis of siliciclastic and volcaniclastic sediments in the Cretaceous and Miocene sequences of the NWAfrican margin (DSDP Leg 47A, Site 397): Sedimentary Geology, v. 112, no. 1–2, p. 137–156,
- ^ Olavsd�ottir, J., M. S. Andersen, and L. O. Boldreel, 2015, Reservoir quality of intrabasalt volcaniclastic units onshore Faroe Islands, North Atlantic Igneous Province, northeast Atlantic: AAPG Bulletin, v. 99, no. 3, p. 467– 497,
- ^ Vincent 2000, pp.17-19
- ^ Vincent 2000, p.22
- ^ a b c Schmidt, R. (1981). "Descriptive nomenclature and classification of pyroclastic deposits and fragments: recommendations of the IUGS Subcommission on the Systematics of Igneous Rocks". Geology. 9: 41–43. doi:10.1007/BF01822152. S2CID 128375559. Retrieved 27 September 2020.
- ^ Schmincke, Hans-Ulrich (2003). Volcanism. Berlin: Springer. p. 130. ISBN 9783540436508.
- ^ Vincent 2000, p.19
- ^ Fisher and Schminke 1984, p.90
- ^ Fisher and Schminke 1984, pp. 89-90
- ^ Schmincke, Hans-Ulrich (2003). Volcanism. Berlin: Springer. pp. 137–138. ISBN 9783540436508.
- ^ Kautz, P. F.; Ingersoll, R. V.; Baldridge, W. S.; Damon, P. E.; Shafiqullah, M. (December 1981). "Geology of the Espinaso Formation (Oligocene), North-Central New Mexico". GSA Bulletin. 92 (12_Part_II): 2318–2400. Bibcode:1981GSAB...92.2318K. doi:10.1130/GSAB-P2-92-2318.
- ^ Smedes, H.W.; Prostka, H.J. (1972). "Stratigraphic framework of the Absaroka Volcanic Supergroup in the Yellowstone National Park region". U.S. Geological Survey Professional Paper. Professional Paper. 729-C: C-19. doi:10.3133/pp729C.
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