{{short description|Indicator of spread of volcanic ejecta}} '''Dispersal index''' is a parameter in volcanology. The dispersal index <math>D</math> was defined by George P. L. Walker in 1973 as the surface area covered by an ash or tephra fall, where the thickness is equal or more than 1/100 of the thickness of the fall at the vent.{{sfn|Pyle|1989|p=10}} An eruption with a low dispersal index leaves most of its products close to the vent, forming a cone; an eruption with a high dispersal index forms thinner sheet-like deposits which extends to larger distances from the vent.{{sfn|Fierstein|Houghton|Wilson|Hildreth|1997|p=215}} A dispersal index of {{convert|500|km2}} or more of coarse pumice is one proposed definition of a Plinian eruption.{{sfn|Walker|1980|p=88}} Likewise, a dispersal index of {{convert|50000|km2}} has been proposed as a cutoff for an ultraplinian eruption.{{sfn|Walker|1980|p=91}} The definition of 1/100 of the near-vent thickness was partially dictated by the fact that most tephra deposits are not well preserved at larger distances.<ref name="BonadonnaErnst1998" />
Originally, the dispersal index was considered a function of the height of the eruption column. Later, a role for the size of the tephra and ash particles was identified,{{sfn|Pyle|1989|p=10}} with coarser fall deposits covering smaller surfaces than finer deposits generated by a column of the same height.{{sfn|Walker|1980|p=88}} For example, a deposit with a dispersal index of {{convert|500|km2}} can be formed by a column with heights of {{convert|14|-|18|km2}}.{{sfn|Sparks|Bursik|Ablay|Thomas|1992|p=690}} Thus, Walker's idea of the column height alone separating a cone forming eruption and an eruption generating a sheet-like deposit was later considered oversimplified.{{sfn|Pyle|1989|p=11}} An additional complicating factor is that fine particles are prone to aggregating and thus falling out more quickly from the column.{{sfn|Sparks|Bursik|Ablay|Thomas|1992|p=694}} Further problems arise when the maximum thickness has to be determined.<ref name="HildrethDrake1992" />
The height of the eruption column, the presence and behaviour of water, the speed and direction of the wind as well as the sizes of the various tephra particles influence the fallout patterns of an ash cloud.{{sfn|Sparks|Bursik|Ablay|Thomas|1992|p=685}}
The dispersal index for volcanic eruptions ranges from <{{convert|1|km2}} and {{convert|1|-|1000|km2}}.{{sfn|Walker|1980|p=88}} A number of basaltic phreatomagmatic deposits, frequently associated with tuff rings, have a dispersal index of less than {{convert|50|km2}}.<ref name="SelfSparks1978" />
{| class="wikitable sortable" |- ! Volcano !! Eruption !! Age !! Dispersal index !! Source |- | Taupō|| Hatepe eruption || 1820 BP || {{convert|100000|km2}} || {{sfn|Walker|1980|p=88}} |- | Taupō || Oruanui eruption || ~20000 BP || >{{convert|100000|km2}} || <ref name="SelfSparks1978" /> |- | Taupō || Hinemaiaia tephra || 4500 years ago || {{convert|40000|km2}} || <ref name="Lowe1986" /> |- | Kelut || || 1990 || {{convert|2000|km2}} || <ref name="Bourdier1997" /> |- | Rinjani || 1257 Samalas eruption, P1 phase || 1257 || {{convert|7500|km2}} || <ref name="Vidal2015" /> |- | Rinjani || 1257 Samalas eruption, P3 phase || 1257 || {{convert|110500|km2}} || <ref name="Vidal2015" /> |- | Mount Pelée || P1 eruption || 650 BP || {{convert|900|km2}} || <ref name="Traineau1989" /> |- | Mount Pelée || P2 eruption || 1670 BP || {{convert|800|km2}} || <ref name="Traineau1989" /> |- | Mount Pelée || P3 eruption || 2010 BP || {{convert|1000|km2}} || <ref name="Traineau1989" /> |- | Rabaul || Vulcan || 1937 || {{convert|40|km2}} || <ref name="Mckee1985" /> |- | Okataina Volcanic Complex || Whakatane tephra || ~ 5500 BP || ~{{convert|200000|km2}} || <ref name="HoltLowe2011" /> |- | Agua de Pau || Fogo A || 5000 BP || {{convert|1500|km2}} || <ref name="BursikSparks1992" /> |- | Hekla || || 1991 || {{convert|460|km2}} || <ref name="Larsen2017" /> |- | Sakurajima || Taisho || 1914 || {{convert|539|km2}} || <ref name="Todde2017" /> |- | Mono Craters || || 4th century AD || {{convert|1800|km2}} ||<ref name="Yang2016" /> |}
A related measure is the '''thickness half-distance''' <math>b_t</math>,{{sfn|Sparks|Bursik|Ablay|Thomas|1992|p=685}} which defines the distance over which the thickness of a deposit halves.{{sfn|Pyle|1989|p=2}} These values are related with each other over <math display="inline">D=\frac{\pi b_t^2 ln(0.01)^2} {ln(0.5)^2}</math> for circular deposits.
== References ==
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Category:Volcanology Category:Tephra