Solchiaro eruption, Procida Island, Naples, Campania, Italyi
Regional Level Types | |
---|---|
Solchiaro eruption | Lava Field |
Procida Island | Commune |
Naples | Metropolitan City |
Campania | Region |
Italy | Country |
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Key
Latitude & Longitude (WGS84):
40° 44' 41'' North , 14° 1' 5'' East
Latitude & Longitude (decimal):
Locality type:
Age:
0.022 Ma
Geologic Time:
KΓΆppen climate type:
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 ElementsMineral 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!
Select Rock List Type
Alphabetical List Tree DiagramDetailed 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 | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
Group 9 - Silicates | |||
β | Diopside | 9.DA.15 | CaMgSi2O6 |
β | Forsterite | 9.AC.05 | Mg2SiO4 |
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 | Magnetite | 7.2.2.3 | Fe2+Fe3+2O4 |
Group 51 - NESOSILICATES Insular SiO4 Groups Only | |||
Insular SiO4 Groups Only with all cations in octahedral [6] coordination | |||
β | Forsterite | 51.3.1.2 | Mg2SiO4 |
Group 65 - INOSILICATES Single-Width,Unbranched Chains,(W=1) | |||
Single-Width Unbranched Chains, W=1 with chains P=2 | |||
β | Diopside | 65.1.3a.1 | CaMgSi2O6 |
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
O | Oxygen | |
---|---|---|
O | β Forsterite | Mg2SiO4 |
O | β Diopside | CaMgSi2O6 |
O | β Magnetite | Fe2+Fe23+O4 |
Mg | Magnesium | |
Mg | β Forsterite | Mg2SiO4 |
Mg | β Diopside | CaMgSi2O6 |
Si | Silicon | |
Si | β Forsterite | Mg2SiO4 |
Si | β Diopside | CaMgSi2O6 |
Ca | Calcium | |
Ca | β Diopside | CaMgSi2O6 |
Fe | Iron | |
Fe | β Magnetite | Fe2+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.
Other Regions, Features and Areas containing this locality
Eurasian PlateTectonic Plate
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