Item talk:Q56614: Difference between revisions
From geokb
(Wrote fresh schema.org document to item wiki page) |
(Update item cache) |
||
Line 1: | Line 1: | ||
{"@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Geologic map of the southern flank of Mauna Loa Volcano, Island of Hawai\u2018i, Hawaii", "identifier": [{"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "sim2932C", "url": "https://pubs.usgs.gov/publication/sim2932C"}, {"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70206310}, {"@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/sim2932C", "url": "https://doi.org/10.3133/sim2932C"}], "inLanguage": "en", "isPartOf": [{"@type": "CreativeWorkSeries", "name": "Scientific Investigations Map"}], "datePublished": "2020", "dateModified": "2024-05-23", "abstract": "On the Island of Hawai\u02bbi, Mauna Loa, the largest volcano on Earth, has erupted 33 times since written descriptions became available in 1832. Some eruptions began with only brief seismic unrest, whereas others followed several months to a year of increased seismicity. Once underway, its eruptions can produce lava flows that may reach the sea in less than 24 hours, severing roads and utilities. In terms of eruption frequency, pre-eruption warning, and rapid flow emplacement, Mauna Loa has great volcanic-hazard potential for the Island of Hawai\u2018i. Volcanic hazards on Mauna Loa may be anticipated, and risk substantially mitigated, by documenting the past activity to refine our knowledge of the hazards and by alerting the public and local government officials of our findings and their implications for hazards assessments and risk.Although most Mauna Loa eruptions begin in the summit area at 12,000 feet (ft) elevation, the Southwest Rift Zone (SWRZ) was the source of at least 10 flank eruptions since 1843. The SWRZ extends from the summit towards Kalae (South Point) at sea level. The lowermost part of this rift zone, marked by Pu\u2018u\u02bboke\u2018oke\u2018o to the north at 6,874 ft elevation and extending to the sea, makes up the lower SWRZ. The community of Hawaiian Ocean View Estates, with a population of about 2,500, is the largest in the region. The subdivision is built entirely on flows erupted from southern Mauna Loa, and some source vents are located within the subdivision. Approximately 25 percent of the subdivision is within Hazard Zone 1.From east to west, the map covers the area from Punalu\u2018u to Miloli\u2018i and, from north to south, extends from north of Pu\u2018u\u02bboke\u2018oke\u2018o to Kalae (South Point). The map encompasses 1,163 square kilometers of the southwest flank of Mauna Loa, from 7,325 ft elevation to sea level. It shows the distribution of eruptive units (flows), which are separated into 16 age groups, ranging from more than 100,000 years before present to A.D. 1950.Lava erupted from the SWRZ typically flows to the west, east, or south (depending upon vent location relative to the rift crest) and generally produces narrow flow lobes. Both morphologic lava flow types\u2014\u2018a\u2018\u0101 and p\u0101hoehoe\u2014are present. In general, the northern part of the mapped area is dominated by flows from the middle SWRZ, whereas the southern part contains flows from the lower SWRZ and includes areas adjacent to, and downslope of, the rift zone. The exceptions are flows that originated from the upper SWRZ in the northeastern part of the Punaluu quadrangle.", "description": "Pamphlet: iv, 28 p.; 2 Sheets: 51.88 x 39.18 inches and 38.20 x 38.05 inches; Read Me; Metadata; Database; 1 Appendix", "publisher": {"@type": "Organization", "name": "U.S. Geological Survey"}, "author": [{"@type": "Person", "name": "Trusdell, Frank A. trusdell@usgs.gov", "givenName": "Frank A.", "familyName": "Trusdell", "email": "trusdell@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-0681-0528", "url": "https://orcid.org/0000-0002-0681-0528"}, "affiliation": [{"@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center"}]}, {"@type": "Person", "name": "Lockwood, John P.", "givenName": "John P.", "familyName": "Lockwood", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-6562-0222", "url": "https://orcid.org/0000-0002-6562-0222"}}], "funder": [{"@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center"}], "spatialCoverage": [{"@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/ | { | ||
"USGS Publications Warehouse": { | |||
"schema": { | |||
"@context": "https://schema.org", | |||
"@type": "CreativeWork", | |||
"additionalType": "USGS Numbered Series", | |||
"name": "Geologic map of the southern flank of Mauna Loa Volcano, Island of Hawai\u2018i, Hawaii", | |||
"identifier": [ | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "USGS Publications Warehouse IndexID", | |||
"value": "sim2932C", | |||
"url": "https://pubs.usgs.gov/publication/sim2932C" | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "USGS Publications Warehouse Internal ID", | |||
"value": 70206310 | |||
}, | |||
{ | |||
"@type": "PropertyValue", | |||
"propertyID": "DOI", | |||
"value": "10.3133/sim2932C", | |||
"url": "https://doi.org/10.3133/sim2932C" | |||
} | |||
], | |||
"inLanguage": "en", | |||
"isPartOf": [ | |||
{ | |||
"@type": "CreativeWorkSeries", | |||
"name": "Scientific Investigations Map" | |||
} | |||
], | |||
"datePublished": "2020", | |||
"dateModified": "2024-05-23", | |||
"abstract": "On the Island of Hawai\u02bbi, Mauna Loa, the largest volcano on Earth, has erupted 33 times since written descriptions became available in 1832. Some eruptions began with only brief seismic unrest, whereas others followed several months to a year of increased seismicity. Once underway, its eruptions can produce lava flows that may reach the sea in less than 24 hours, severing roads and utilities. In terms of eruption frequency, pre-eruption warning, and rapid flow emplacement, Mauna Loa has great volcanic-hazard potential for the Island of Hawai\u2018i. Volcanic hazards on Mauna Loa may be anticipated, and risk substantially mitigated, by documenting the past activity to refine our knowledge of the hazards and by alerting the public and local government officials of our findings and their implications for hazards assessments and risk.Although most Mauna Loa eruptions begin in the summit area at 12,000 feet (ft) elevation, the Southwest Rift Zone (SWRZ) was the source of at least 10 flank eruptions since 1843. The SWRZ extends from the summit towards Kalae (South Point) at sea level. The lowermost part of this rift zone, marked by Pu\u2018u\u02bboke\u2018oke\u2018o to the north at 6,874 ft elevation and extending to the sea, makes up the lower SWRZ. The community of Hawaiian Ocean View Estates, with a population of about 2,500, is the largest in the region. The subdivision is built entirely on flows erupted from southern Mauna Loa, and some source vents are located within the subdivision. Approximately 25 percent of the subdivision is within Hazard Zone 1.From east to west, the map covers the area from Punalu\u2018u to Miloli\u2018i and, from north to south, extends from north of Pu\u2018u\u02bboke\u2018oke\u2018o to Kalae (South Point). The map encompasses 1,163 square kilometers of the southwest flank of Mauna Loa, from 7,325 ft elevation to sea level. It shows the distribution of eruptive units (flows), which are separated into 16 age groups, ranging from more than 100,000 years before present to A.D. 1950.Lava erupted from the SWRZ typically flows to the west, east, or south (depending upon vent location relative to the rift crest) and generally produces narrow flow lobes. Both morphologic lava flow types\u2014\u2018a\u2018\u0101 and p\u0101hoehoe\u2014are present. In general, the northern part of the mapped area is dominated by flows from the middle SWRZ, whereas the southern part contains flows from the lower SWRZ and includes areas adjacent to, and downslope of, the rift zone. The exceptions are flows that originated from the upper SWRZ in the northeastern part of the Punaluu quadrangle.", | |||
"description": "Pamphlet: iv, 28 p.; 2 Sheets: 51.88 x 39.18 inches and 38.20 x 38.05 inches; Read Me; Metadata; Database; 1 Appendix", | |||
"publisher": { | |||
"@type": "Organization", | |||
"name": "U.S. Geological Survey" | |||
}, | |||
"author": [ | |||
{ | |||
"@type": "Person", | |||
"name": "Trusdell, Frank A. trusdell@usgs.gov", | |||
"givenName": "Frank A.", | |||
"familyName": "Trusdell", | |||
"email": "trusdell@usgs.gov", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "ORCID", | |||
"value": "0000-0002-0681-0528", | |||
"url": "https://orcid.org/0000-0002-0681-0528" | |||
}, | |||
"affiliation": [ | |||
{ | |||
"@type": "Organization", | |||
"name": "Volcano Science Center", | |||
"url": "https://www.usgs.gov/centers/volcano-science-center" | |||
} | |||
] | |||
}, | |||
{ | |||
"@type": "Person", | |||
"name": "Lockwood, John P.", | |||
"givenName": "John P.", | |||
"familyName": "Lockwood", | |||
"identifier": { | |||
"@type": "PropertyValue", | |||
"propertyID": "ORCID", | |||
"value": "0000-0002-6562-0222", | |||
"url": "https://orcid.org/0000-0002-6562-0222" | |||
} | |||
} | |||
], | |||
"funder": [ | |||
{ | |||
"@type": "Organization", | |||
"name": "Volcano Science Center", | |||
"url": "https://www.usgs.gov/centers/volcano-science-center" | |||
} | |||
], | |||
"spatialCoverage": [ | |||
{ | |||
"@type": "Place", | |||
"additionalType": "country", | |||
"name": "United States", | |||
"url": "https://geonames.org/4074035" | |||
}, | |||
{ | |||
"@type": "Place", | |||
"additionalType": "state", | |||
"name": "Hawaii" | |||
}, | |||
{ | |||
"@type": "Place", | |||
"additionalType": "unknown", | |||
"name": "Southern flank of Mauna Loa Volcano" | |||
}, | |||
{ | |||
"@type": "Place", | |||
"geo": [ | |||
{ | |||
"@type": "GeoShape", | |||
"additionalProperty": { | |||
"@type": "PropertyValue", | |||
"name": "GeoJSON", | |||
"value": { | |||
"type": "FeatureCollection", | |||
"features": [ | |||
{ | |||
"type": "Feature", | |||
"properties": {}, | |||
"geometry": { | |||
"type": "Polygon", | |||
"coordinates": [ | |||
[ | |||
[ | |||
-155.950927734375, | |||
18.869904894964883 | |||
], | |||
[ | |||
-155.4400634765625, | |||
18.869904894964883 | |||
], | |||
[ | |||
-155.4400634765625, | |||
19.267072569005542 | |||
], | |||
[ | |||
-155.950927734375, | |||
19.267072569005542 | |||
], | |||
[ | |||
-155.950927734375, | |||
18.869904894964883 | |||
] | |||
] | |||
] | |||
} | |||
} | |||
] | |||
} | |||
} | |||
}, | |||
{ | |||
"@type": "GeoCoordinates", | |||
"latitude": 19.068488731985212, | |||
"longitude": -155.69549560546875 | |||
} | |||
] | |||
} | |||
] | |||
} | |||
} | |||
} |
Latest revision as of 23:07, 14 August 2024
{
"USGS Publications Warehouse": { "schema": { "@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Geologic map of the southern flank of Mauna Loa Volcano, Island of Hawai\u2018i, Hawaii", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "sim2932C", "url": "https://pubs.usgs.gov/publication/sim2932C" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70206310 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/sim2932C", "url": "https://doi.org/10.3133/sim2932C" } ], "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Scientific Investigations Map" } ], "datePublished": "2020", "dateModified": "2024-05-23", "abstract": "On the Island of Hawai\u02bbi, Mauna Loa, the largest volcano on Earth, has erupted 33 times since written descriptions became available in 1832. Some eruptions began with only brief seismic unrest, whereas others followed several months to a year of increased seismicity. Once underway, its eruptions can produce lava flows that may reach the sea in less than 24 hours, severing roads and utilities. In terms of eruption frequency, pre-eruption warning, and rapid flow emplacement, Mauna Loa has great volcanic-hazard potential for the Island of Hawai\u2018i. Volcanic hazards on Mauna Loa may be anticipated, and risk substantially mitigated, by documenting the past activity to refine our knowledge of the hazards and by alerting the public and local government officials of our findings and their implications for hazards assessments and risk.Although most Mauna Loa eruptions begin in the summit area at 12,000 feet (ft) elevation, the Southwest Rift Zone (SWRZ) was the source of at least 10 flank eruptions since 1843. The SWRZ extends from the summit towards Kalae (South Point) at sea level. The lowermost part of this rift zone, marked by Pu\u2018u\u02bboke\u2018oke\u2018o to the north at 6,874 ft elevation and extending to the sea, makes up the lower SWRZ. The community of Hawaiian Ocean View Estates, with a population of about 2,500, is the largest in the region. The subdivision is built entirely on flows erupted from southern Mauna Loa, and some source vents are located within the subdivision. Approximately 25 percent of the subdivision is within Hazard Zone 1.From east to west, the map covers the area from Punalu\u2018u to Miloli\u2018i and, from north to south, extends from north of Pu\u2018u\u02bboke\u2018oke\u2018o to Kalae (South Point). The map encompasses 1,163 square kilometers of the southwest flank of Mauna Loa, from 7,325 ft elevation to sea level. It shows the distribution of eruptive units (flows), which are separated into 16 age groups, ranging from more than 100,000 years before present to A.D. 1950.Lava erupted from the SWRZ typically flows to the west, east, or south (depending upon vent location relative to the rift crest) and generally produces narrow flow lobes. Both morphologic lava flow types\u2014\u2018a\u2018\u0101 and p\u0101hoehoe\u2014are present. In general, the northern part of the mapped area is dominated by flows from the middle SWRZ, whereas the southern part contains flows from the lower SWRZ and includes areas adjacent to, and downslope of, the rift zone. The exceptions are flows that originated from the upper SWRZ in the northeastern part of the Punaluu quadrangle.", "description": "Pamphlet: iv, 28 p.; 2 Sheets: 51.88 x 39.18 inches and 38.20 x 38.05 inches; Read Me; Metadata; Database; 1 Appendix", "publisher": { "@type": "Organization", "name": "U.S. Geological Survey" }, "author": [ { "@type": "Person", "name": "Trusdell, Frank A. trusdell@usgs.gov", "givenName": "Frank A.", "familyName": "Trusdell", "email": "trusdell@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-0681-0528", "url": "https://orcid.org/0000-0002-0681-0528" }, "affiliation": [ { "@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center" } ] }, { "@type": "Person", "name": "Lockwood, John P.", "givenName": "John P.", "familyName": "Lockwood", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-6562-0222", "url": "https://orcid.org/0000-0002-6562-0222" } } ], "funder": [ { "@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center" } ], "spatialCoverage": [ { "@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/4074035" }, { "@type": "Place", "additionalType": "state", "name": "Hawaii" }, { "@type": "Place", "additionalType": "unknown", "name": "Southern flank of Mauna Loa Volcano" }, { "@type": "Place", "geo": [ { "@type": "GeoShape", "additionalProperty": { "@type": "PropertyValue", "name": "GeoJSON", "value": { "type": "FeatureCollection", "features": [ { "type": "Feature", "properties": {}, "geometry": { "type": "Polygon", "coordinates": [ [ [ -155.950927734375, 18.869904894964883 ], [ -155.4400634765625, 18.869904894964883 ], [ -155.4400634765625, 19.267072569005542 ], [ -155.950927734375, 19.267072569005542 ], [ -155.950927734375, 18.869904894964883 ] ] ] } } ] } } }, { "@type": "GeoCoordinates", "latitude": 19.068488731985212, "longitude": -155.69549560546875 } ] } ] } }
}