Ver JSON completo
{
"content_url": "https://en.wikipedia.org/wiki/Fissure_vent",
"extract": "A fissure vent, also known as a volcanic fissure, eruption fissure or simply a fissure, is a linear volcanic vent through which lava erupts, usually without any explosive activity. The vent is often a few metres wide and may be many kilometres long. Fissure vents can cause large flood basalts which run first in lava channels and later in lava tubes. After some time, the eruption tends to become focused at one or more spatter cones. Volcanic cones and their craters that are aligned along a fissure form a crater row. Small fissure vents may not be easily discernible from the air, but the crater rows or the canyons built up by some of them are.",
"language": "en",
"normalizedtitle": "Fissure vent",
"page_title": "Fissure_vent",
"pageid": 5814507,
"raw": {
"pages": [
{
"content_urls": {
"desktop": {
"edit": "https://en.wikipedia.org/wiki/Fissure_vent?action=edit",
"page": "https://en.wikipedia.org/wiki/Fissure_vent",
"revisions": "https://en.wikipedia.org/wiki/Fissure_vent?action=history",
"talk": "https://en.wikipedia.org/wiki/Talk:Fissure_vent"
},
"mobile": {
"edit": "https://en.wikipedia.org/wiki/Fissure_vent?action=edit",
"page": "https://en.wikipedia.org/wiki/Fissure_vent",
"revisions": "https://en.wikipedia.org/wiki/Special:History/Fissure_vent",
"talk": "https://en.wikipedia.org/wiki/Talk:Fissure_vent"
}
},
"description": "Linear volcanic vent through which lava erupts",
"description_source": "local",
"dir": "ltr",
"displaytitle": "\u003cspan lang=\"en\" dir=\"ltr\"\u003e\u003cspan class=\"mw-page-title-main\"\u003eFissure vent\u003c/span\u003e\u003c/span\u003e",
"extract": "A fissure vent, also known as a volcanic fissure, eruption fissure or simply a fissure, is a linear volcanic vent through which lava erupts, usually without any explosive activity. The vent is often a few metres wide and may be many kilometres long. Fissure vents can cause large flood basalts which run first in lava channels and later in lava tubes. After some time, the eruption tends to become focused at one or more spatter cones. Volcanic cones and their craters that are aligned along a fissure form a crater row. Small fissure vents may not be easily discernible from the air, but the crater rows or the canyons built up by some of them are.",
"extract_html": "\u003cp\u003eA \u003cb\u003efissure vent\u003c/b\u003e, also known as a \u003cb\u003evolcanic fissure\u003c/b\u003e, \u003cb\u003eeruption fissure\u003c/b\u003e or simply a \u003cb\u003efissure\u003c/b\u003e, is a linear volcanic vent through which lava erupts, usually without any explosive activity. The vent is often a few metres wide and may be many kilometres long. Fissure vents can cause large flood basalts which run first in lava channels and later in lava tubes. After some time, the eruption tends to become focused at one or more spatter cones. Volcanic cones and their craters that are aligned along a fissure form a \u003cb\u003ecrater row\u003c/b\u003e. Small fissure vents may not be easily discernible from the air, but the crater rows or the canyons built up by some of them are.\u003c/p\u003e",
"lang": "en",
"namespace": {
"id": 0,
"text": ""
},
"normalizedtitle": "Fissure vent",
"originalimage": {
"height": 449,
"source": "https://upload.wikimedia.org/wikipedia/commons/a/a4/Volcano_q.jpg",
"width": 678
},
"pageid": 5814507,
"revision": "1326522084",
"thumbnail": {
"height": 219,
"source": "https://upload.wikimedia.org/wikipedia/commons/thumb/a/a4/Volcano_q.jpg/330px-Volcano_q.jpg",
"width": 330
},
"tid": "44800ed8-d4ef-11f0-95df-d4450da7b0a5",
"timestamp": "2025-12-09T11:07:36Z",
"title": "Fissure_vent",
"titles": {
"canonical": "Fissure_vent",
"display": "\u003cspan lang=\"en\" dir=\"ltr\"\u003e\u003cspan class=\"mw-page-title-main\"\u003eFissure vent\u003c/span\u003e\u003c/span\u003e",
"normalized": "Fissure vent"
},
"type": "standard",
"wikibase_item": "Q2143039"
},
{
"content_urls": {
"desktop": {
"edit": "https://en.wikipedia.org/wiki/Michoac%C3%A1n?action=edit",
"page": "https://en.wikipedia.org/wiki/Michoac%C3%A1n",
"revisions": "https://en.wikipedia.org/wiki/Michoac%C3%A1n?action=history",
"talk": "https://en.wikipedia.org/wiki/Talk:Michoac%C3%A1n"
},
"mobile": {
"edit": "https://en.wikipedia.org/wiki/Michoac%C3%A1n?action=edit",
"page": "https://en.wikipedia.org/wiki/Michoac%C3%A1n",
"revisions": "https://en.wikipedia.org/wiki/Special:History/Michoac%C3%A1n",
"talk": "https://en.wikipedia.org/wiki/Talk:Michoac%C3%A1n"
}
},
"coordinates": {
"lat": 19.21,
"lon": -101.91
},
"description": "State of Mexico",
"description_source": "local",
"dir": "ltr",
"displaytitle": "\u003cspan lang=\"en\" dir=\"ltr\"\u003e\u003cspan class=\"mw-page-title-main\"\u003eMichoac\u00e1n\u003c/span\u003e\u003c/span\u003e",
"extract": "Michoac\u00e1n, formally Michoac\u00e1n de Ocampo, officially the Free and Sovereign State of Michoac\u00e1n de Ocampo, is one of the 31 states which, together with Mexico City, compose the Federal Entities of Mexico. The state is divided into 113 municipalities and its capital city is Morelia. The city was named after Jos\u00e9 Mar\u00eda Morelos, a native of the city and one of the main heroes of the Mexican War of Independence.",
"extract_html": "\u003cp\u003e\u003cb\u003eMichoac\u00e1n\u003c/b\u003e, formally \u003cb\u003eMichoac\u00e1n de Ocampo\u003c/b\u003e, officially the \u003cb\u003eFree and Sovereign State of Michoac\u00e1n de Ocampo\u003c/b\u003e, is one of the 31 states which, together with Mexico City, compose the Federal Entities of Mexico. The state is divided into 113 municipalities and its capital city is Morelia. The city was named after Jos\u00e9 Mar\u00eda Morelos, a native of the city and one of the main heroes of the Mexican War of Independence.\u003c/p\u003e",
"lang": "en",
"namespace": {
"id": 0,
"text": ""
},
"normalizedtitle": "Michoac\u00e1n",
"originalimage": {
"height": 1440,
"source": "https://upload.wikimedia.org/wikipedia/commons/8/8d/Cerro_Patamban.jpg",
"width": 2048
},
"pageid": 195805,
"revision": "1358648796",
"thumbnail": {
"height": 232,
"source": "https://upload.wikimedia.org/wikipedia/commons/thumb/8/8d/Cerro_Patamban.jpg/330px-Cerro_Patamban.jpg",
"width": 330
},
"tid": "dc9389c1-646f-11f1-8b4e-eb7520fa10a4",
"timestamp": "2026-06-10T01:58:23Z",
"title": "Michoac\u00e1n",
"titles": {
"canonical": "Michoac\u00e1n",
"display": "\u003cspan lang=\"en\" dir=\"ltr\"\u003e\u003cspan class=\"mw-page-title-main\"\u003eMichoac\u00e1n\u003c/span\u003e\u003c/span\u003e",
"normalized": "Michoac\u00e1n"
},
"type": "standard",
"wikibase_item": "Q79861"
},
{
"content_urls": {
"desktop": {
"edit": "https://en.wikipedia.org/wiki/Cinder_cone?action=edit",
"page": "https://en.wikipedia.org/wiki/Cinder_cone",
"revisions": "https://en.wikipedia.org/wiki/Cinder_cone?action=history",
"talk": "https://en.wikipedia.org/wiki/Talk:Cinder_cone"
},
"mobile": {
"edit": "https://en.wikipedia.org/wiki/Cinder_cone?action=edit",
"page": "https://en.wikipedia.org/wiki/Cinder_cone",
"revisions": "https://en.wikipedia.org/wiki/Special:History/Cinder_cone",
"talk": "https://en.wikipedia.org/wiki/Talk:Cinder_cone"
}
},
"description": "Steep hill of pyroclastic fragments around a volcanic vent",
"description_source": "local",
"dir": "ltr",
"displaytitle": "\u003cspan lang=\"en\" dir=\"ltr\"\u003e\u003cspan class=\"mw-page-title-main\"\u003eCinder cone\u003c/span\u003e\u003c/span\u003e",
"extract": "A cinder cone or scoria cone is a steep, conical landform of loose pyroclastic fragments, such as volcanic ash, clinkers, or scoria that has been built around a volcanic vent. The pyroclastic fragments are formed by explosive eruptions or tall Hawaiian-style lava fountains from a single, typically cylindrical, vent.",
"extract_html": "\u003cp\u003eA \u003cb\u003ecinder cone\u003c/b\u003e or \u003cb\u003escoria cone\u003c/b\u003e is a steep, conical landform of loose pyroclastic fragments, such as volcanic ash, clinkers, or scoria that has been built around a volcanic vent. The pyroclastic fragments are formed by explosive eruptions or tall Hawaiian-style lava fountains from a single, typically cylindrical, vent.\u003c/p\u003e",
"lang": "en",
"namespace": {
"id": 0,
"text": ""
},
"normalizedtitle": "Cinder cone",
"originalimage": {
"height": 237,
"source": "https://upload.wikimedia.org/wikipedia/commons/1/10/Cinder_cone_diagram.gif",
"width": 400
},
"pageid": 10964778,
"revision": "1348632841",
"thumbnail": {
"height": 196,
"source": "https://upload.wikimedia.org/wikipedia/commons/thumb/1/10/Cinder_cone_diagram.gif/330px-Cinder_cone_diagram.gif",
"width": 330
},
"tid": "85fd20f7-3752-11f1-97b5-a7fa622c83f5",
"timestamp": "2026-04-13T16:05:00Z",
"title": "Cinder_cone",
"titles": {
"canonical": "Cinder_cone",
"display": "\u003cspan lang=\"en\" dir=\"ltr\"\u003e\u003cspan class=\"mw-page-title-main\"\u003eCinder cone\u003c/span\u003e\u003c/span\u003e",
"normalized": "Cinder cone"
},
"type": "standard",
"wikibase_item": "Q1806785"
},
{
"content_urls": {
"desktop": {
"edit": "https://en.wikipedia.org/wiki/Par%C3%ADcutin?action=edit",
"page": "https://en.wikipedia.org/wiki/Par%C3%ADcutin",
"revisions": "https://en.wikipedia.org/wiki/Par%C3%ADcutin?action=history",
"talk": "https://en.wikipedia.org/wiki/Talk:Par%C3%ADcutin"
},
"mobile": {
"edit": "https://en.wikipedia.org/wiki/Par%C3%ADcutin?action=edit",
"page": "https://en.wikipedia.org/wiki/Par%C3%ADcutin",
"revisions": "https://en.wikipedia.org/wiki/Special:History/Par%C3%ADcutin",
"talk": "https://en.wikipedia.org/wiki/Talk:Par%C3%ADcutin"
}
},
"coordinates": {
"lat": 19.49305556,
"lon": -102.25111111
},
"description": "Dormant volcano in Michoac\u00e1n, Mexico",
"description_source": "local",
"dir": "ltr",
"displaytitle": "\u003cspan lang=\"en\" dir=\"ltr\"\u003e\u003cspan class=\"mw-page-title-main\"\u003ePar\u00edcutin\u003c/span\u003e\u003c/span\u003e",
"extract": "Par\u00edcutin is a cinder cone volcano located in the Mexican state of Michoac\u00e1n, near the city of Uruapan and about 322 kilometers (200\u00a0mi) west of Mexico City. The volcano surged suddenly from the cornfield of local farmer Dionisio Pulido in 1943, attracting both popular and scientific attention.",
"extract_html": "\u003cp\u003e\u003cb\u003ePar\u00edcutin\u003c/b\u003e is a cinder cone volcano located in the Mexican state of Michoac\u00e1n, near the city of Uruapan and about 322 kilometers (200\u00a0mi) west of Mexico City. The volcano surged suddenly from the cornfield of local farmer Dionisio Pulido in 1943, attracting both popular and scientific attention.\u003c/p\u003e",
"lang": "en",
"namespace": {
"id": 0,
"text": ""
},
"normalizedtitle": "Par\u00edcutin",
"originalimage": {
"height": 2018,
"source": "https://upload.wikimedia.org/wikipedia/commons/a/a8/Paricutin.jpg",
"width": 3112
},
"pageid": 358810,
"revision": "1355489942",
"thumbnail": {
"height": 214,
"source": "https://upload.wikimedia.org/wikipedia/commons/thumb/a/a8/Paricutin.jpg/330px-Paricutin.jpg",
"width": 330
},
"tid": "5eda1089-5596-11f1-94db-48bfe7877efb",
"timestamp": "2026-05-22T04:26:15Z",
"title": "Par\u00edcutin",
"titles": {
"canonical": "Par\u00edcutin",
"display": "\u003cspan lang=\"en\" dir=\"ltr\"\u003e\u003cspan class=\"mw-page-title-main\"\u003ePar\u00edcutin\u003c/span\u003e\u003c/span\u003e",
"normalized": "Par\u00edcutin"
},
"type": "standard",
"wikibase_item": "Q231620"
}
],
"text": "A fissure opened in a cornfield in the Mexican state of Michoac\u00e1n and continued to erupt for nine years, forming the cinder cone Par\u00edcutin .",
"year": 1943
},
"text": "A fissure opened in a cornfield in the Mexican state of Michoac\u00e1n and continued to erupt for nine years, forming the cinder cone Par\u00edcutin .",
"thumbnail": "https://upload.wikimedia.org/wikipedia/commons/thumb/a/a4/Volcano_q.jpg/330px-Volcano_q.jpg",
"type": "selected",
"year": 1943
}
