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Solchiaro eruption, Procida Island, Naples, Campania, Italyi
Regional Level Types
Solchiaro eruptionLava Field
Procida IslandCommune
NaplesMetropolitan City
CampaniaRegion
ItalyCountry

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Latitude & Longitude (WGS84):
40° 44' 41'' North , 14° 1' 5'' East
Latitude & Longitude (decimal):
Locality type:
Age:
0.022 Ma
Geologic Time:


The Solchiaro eruption (< 22 ka) is the last volcanic event on Procida Island. Following the Solchiaro eruption, no further volcanic activity has been recorded on Procida, and the island has no fumaroles and shows little seismic activity. Procida is covered by the products of later eruptions from nearby Phlegrean Fields (Campi Flegrei) and Ischia, and the products of Procida eruptions are exposed along the mainland coast, interbedded with Phlegrean Fields (Campi Flegrei) and Ischia products.

The Solchiaro eruption built a tuff ring; the maximum thickness of the Solchiaro deposits is 60 m, with a basal diameter of 2.4 km. Solchiaro outcrops are abundant along most of the coast of Procida. Proximal Solchiaro deposits are stratified and lithified yellow tuffs with bomb sags and deep erosive channels, whereas distal deposits are gray and range from partially lithified to unlithified tuffs.

Select Mineral List Type

Standard Detailed Strunz Dana Chemical Elements

Mineral List


3 valid minerals.

Rock Types Recorded

Note: this is a very new system on mindat.org and data is currently VERY limited. Please bear with us while we work towards adding this information!

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Alphabetical List Tree Diagram

Detailed Mineral List:

β“˜ 'Albite-Anorthite Series'
Reference: Bonechi, B. (2020) Influence of Pre-Existing Nuclei on the Crystallization Kinetics of Primitive Alkaline Magmas: Insights on the Deep Feeding System of the Campi Flegrei Volcanic District. Minerals 10, 234.
β“˜ 'Alkali Feldspar'
Reference: Bonechi, B. (2020) Influence of Pre-Existing Nuclei on the Crystallization Kinetics of Primitive Alkaline Magmas: Insights on the Deep Feeding System of the Campi Flegrei Volcanic District. Minerals 10, 234.
β“˜ 'Clinopyroxene Subgroup'
Reference: Bonechi, B. (2020) Influence of Pre-Existing Nuclei on the Crystallization Kinetics of Primitive Alkaline Magmas: Insights on the Deep Feeding System of the Campi Flegrei Volcanic District. Minerals 10, 234.
β“˜ Diopside
Formula: CaMgSi2O6
Reference: Bonechi, B. (2020) Influence of Pre-Existing Nuclei on the Crystallization Kinetics of Primitive Alkaline Magmas: Insights on the Deep Feeding System of the Campi Flegrei Volcanic District. Minerals 10, 234.
β“˜ 'Fayalite-Forsterite Series'
Reference: Bonechi, B. (2020) Influence of Pre-Existing Nuclei on the Crystallization Kinetics of Primitive Alkaline Magmas: Insights on the Deep Feeding System of the Campi Flegrei Volcanic District. Minerals 10, 234.
β“˜ Forsterite
Formula: Mg2SiO4
Reference: Bonechi, B. (2020) Influence of Pre-Existing Nuclei on the Crystallization Kinetics of Primitive Alkaline Magmas: Insights on the Deep Feeding System of the Campi Flegrei Volcanic District. Minerals 10, 234.
β“˜ 'Glass'
Reference: Bonechi, B. (2020) Influence of Pre-Existing Nuclei on the Crystallization Kinetics of Primitive Alkaline Magmas: Insights on the Deep Feeding System of the Campi Flegrei Volcanic District. Minerals 10, 234.
β“˜ Magnetite
Formula: Fe2+Fe3+2O4
Reference: Bonechi, B. (2020) Influence of Pre-Existing Nuclei on the Crystallization Kinetics of Primitive Alkaline Magmas: Insights on the Deep Feeding System of the Campi Flegrei Volcanic District. Minerals 10, 234.

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
β“˜Magnetite4.BB.05Fe2+Fe3+2O4
Group 9 - Silicates
β“˜Diopside9.DA.15CaMgSi2O6
β“˜Forsterite9.AC.05Mg2SiO4
Unclassified Minerals, Rocks, etc.
β“˜'Albite-Anorthite Series'-
β“˜'Alkali Feldspar'-
β“˜'Clinopyroxene Subgroup'-
β“˜'Fayalite-Forsterite Series'-
β“˜'Glass'-

List of minerals arranged by Dana 8th Edition classification

Group 7 - MULTIPLE OXIDES
AB2X4
β“˜Magnetite7.2.2.3Fe2+Fe3+2O4
Group 51 - NESOSILICATES Insular SiO4 Groups Only
Insular SiO4 Groups Only with all cations in octahedral [6] coordination
β“˜Forsterite51.3.1.2Mg2SiO4
Group 65 - INOSILICATES Single-Width,Unbranched Chains,(W=1)
Single-Width Unbranched Chains, W=1 with chains P=2
β“˜Diopside65.1.3a.1CaMgSi2O6
Unclassified Minerals, Mixtures, etc.
β“˜'Albite-Anorthite Series'-
β“˜'Alkali Feldspar'-
β“˜'Clinopyroxene Subgroup'-
β“˜'Fayalite-Forsterite Series'-
β“˜'Glass'-

List of minerals for each chemical element

OOxygen
Oβ“˜ ForsteriteMg2SiO4
Oβ“˜ DiopsideCaMgSi2O6
Oβ“˜ MagnetiteFe2+Fe23+O4
MgMagnesium
Mgβ“˜ ForsteriteMg2SiO4
Mgβ“˜ DiopsideCaMgSi2O6
SiSilicon
Siβ“˜ ForsteriteMg2SiO4
Siβ“˜ DiopsideCaMgSi2O6
CaCalcium
Caβ“˜ DiopsideCaMgSi2O6
FeIron
Feβ“˜ MagnetiteFe2+Fe23+O4

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Bonechi, B. (2020) Influence of Pre-Existing Nuclei on the Crystallization Kinetics of Primitive Alkaline Magmas: Insights on the Deep Feeding System of the Campi Flegrei Volcanic District. Minerals 10, 234.

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