City | Population |
---|
City | Population |
---|---|
City1 | |
City2 | |
City3 | |
City4 | |
City5 |
Volcanic Explosivity Index
editThe Global Volcanism Program has assigned a Volcanic Explosivity Index (VEI) to all except five of Kīlauea's ninety-five known eruptions of the last 11,700 years. The eruption of 1790 has a VEI of 4. The eruptions of 1820, 1924, 1959 and 1960 have a VEI of 2. The eruptions of 680, 1050, 1490, 1500, 1610, 1868, four eruptions in 1961 and the current eruption since 1983 have a VEI of 1. The other seventy-four eruptions have a VEI of 0.
VEI | Number of Holocene eruptions for which a VEI has been assigned (total=90) |
---|---|
VEI 0 | |
VEI 1 | |
VEI 2 | |
VEI 3 | |
VEI 4 |
According to the Smithsonian Institution's Global Volcanism Program, Vesuvius has had 54 confirmed "eruptive periods" during the Holocene Epoch (the last 11,700 years). A volcanic explosivity index (VEI) has been assigned to all but one of these eruptive periods.
VEI | Number of Holocene eruptions for which a VEI has been assigned (total=53) |
---|---|
VEI 0 | |
VEI 1 | |
VEI 2 | |
VEI 3 | |
VEI 4 | |
VEI 5 |
Location map tests
editDarwin Rise ___location map
edit
Mid-Urals Ring Structure
editLake District ___location map
editMcDonald Islands ___location map
editDanube Canyon ___location map
editCheddar Gorge ___location map
edit
Volcanic Explosivity Index
editThe Global Volcanism Program has assigned a Volcanic Explosivity Index (VEI) to all of Mount Etna's eruptions since January 1955.
VEI | Number of eruptions (total=49) |
---|---|
VEI 0 | |
VEI 1 | |
VEI 2 | |
VEI 3 |
Igneous rocks Template
editMohs hardness of moldavite
editThere seems to be lots of disagreement about the Mohs hardness of moldavite. Here are some of the Mohs hardness values and their sources:
Source | Mohs hardness | Reference | Comments |
---|---|---|---|
Gemdat.org | 5.5 | [1] | |
The Drilling Manual (5th edition)edited by Australian Drilling Industry Training Committee Limited, page 607 | 5.5 | [2] | |
Gemmology by Peter G. Read, page 300 | 5.5 | [3] | |
Gemstones of the World by Walter Schumann, page 246 | 5.5 | [4] | |
Correlation of some physical and chemical properties of moldavites by V. Bouška and P. Povondra, Geochimica et Cosmochimica Acta, Volume 28, 1964, pages 783-791 | between 6.5 and 7 | [5][6] | |
Australian Museum | 6-7 | [7] | Hardness value is actually for tektites; moldavites are a type of tektite |
Geothermal gradient
edit25-30°C per km = 25–30 °C (45–54 °F) (°F per km). Convert from km to mi by multiplying 1.6093 = 40.2–48.3 °C (72–87 °F) (°F per mi).
Hoodoo Mountain - Featured Article review
editIMA Mineral name abbreviations
edithttps://en.wikipedia.org/w/index.php?title=Anorthite&oldid=1055555462
Canary Islands eruptions table
editOrdovician regional series and stages table
editICS series | ICS stage | British series | British stage | North American series | North American stage | Australian series | Australian stage | Chinese series | Chinese stage |
---|---|---|---|---|---|---|---|---|---|
Upper Ordovician | Hirnantian | Ashgill | Hirnantian | Cincinnati | Gamach | Upper Ordovician | Bolinda | Late Ordovician | Hirnantian |
Katian | Rawthey | Richmond | Chientangkiang | ||||||
Cautley | Maysville | Easton | Neichiashan | ||||||
Pusgill | Eden | ||||||||
Caradoc | Strefford | Mohawk | Chatfield | ||||||
Cheney | |||||||||
Sandbian | Burrell | Turin | Gisborne | ||||||
Aureluc | Whiterock | Chazy | |||||||
Middle Ordovician | Darriwilian | Llanvirn | Llandeilo | Middle Ordovician | Darriwiliane | Middle Ordovician | Darriwilian | ||
Abereiddy | Not defined | ||||||||
Dapingian | Arenig | Fenn | Early Ordovician | Yapeen | Dapingian | ||||
Whitland | Ranger | Castlemaine | |||||||
Ibex | Black Hills | Chewton | |||||||
Bendigo | |||||||||
Lower Ordovician | Floian | Moridun | Tule | Lancefield | Lower Ordovician | Floian | |||
Tremadocian | Tremadoc | Migneint | Stairs | Tremadocian | |||||
Cressage | Skullrock |
Canary Islands - Holocene Bar Chart
edit- Apple
- Banana
- Orange
- Tenerife
- La Palma
Tenerife and La Palma comparison
editDuring the last 10,000 years, Tenerife and La Palma have been the two most volcanically active Canary islands. The bar chart compares the number of volcanic eruptions (vertical y-axis) at different stages during this time span (horizontal x-axis).[8]
- Tenerife
- La Palma
Geology of the Canary Islands - Image Gallery
editGeology of the Canary Islands - Volcanic Landforms Table
editExt_Lnk
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Canary Islands Earthquakes - Interactive Map
edit________________________________________________________________________________________________________________
- ^ https://www.gemdat.org/gem-10860.html
- ^ https://books.google.com/books?id=yYu9BwAAQBAJ&pg=PA607&lpg=PA607&dq=moldavite+mohs+hardness&source=bl&ots=aAYjprWB3m&sig=BGbEMkqm-ZKpsYOjOv294MGb5BY&hl=en&sa=X&ved=0ahUKEwjAy7HeguLXAhWFD8AKHe6XDFs4ChDoAQhWMAw#v=onepage&q=moldavite%20mohs%20hardness&f=false
- ^ https://books.google.com/books?id=b-7fBAAAQBAJ&pg=PA319&lpg=PA319&dq=moldavite+hardness&source=bl&ots=qoxtzWZiXu&sig=uBbkyiK8WYrH2SlS0mW9tOD-9hQ&hl=en&sa=X&ved=0ahUKEwiLq-ammuLXAhWjLMAKHbXBB2MQ6AEIMDAB#v=onepage&q=gemmology%20read%20moldavite%20hardness&f=false
- ^ https://books.google.com/books?id=V9PqVxpxeiEC&pg=PA246&lpg=PA246&dq=moldavite+mohs+hardness&source=bl&ots=H_L3QJAqPH&sig=6GhocLRP86RNtoYbMiCipmJ6ky4&hl=en&sa=X&ved=0ahUKEwi-x5DKhuLXAhXsJ8AKHXhiDKk4ChDoAQg5MAY#v=onepage&q=moldavite%20mohs%20hardness&f=false
- ^ http://www.sciencedirect.com/science/article/pii/0016703764900328
- ^ https://scholar.google.com/scholar?hl=en&as_sdt=0%2C5&q=moldavite+hardness&btnG=
- ^ https://australianmuseum.net.au/tektites
- ^ Spain Volcanoes – Holocene Eruptions, Smithsonian Institution Global Volcanism Program, retrieved 13 July 2024; https://volcano.si.edu/volcanolist_countries.cfm?country=Spain