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Nejapa-Miraflores вулкан

fissure vents 360 m / 1,181 ft
Nicaragua, 12.12°N / -86.32°W
Текущее состояние: normal or dormant (1 из 5) | Reports
Nejapa-Miraflores volcano books
Типичный извержения стиль: effusive
Nejapa-Miraflores Вулкан-извержения: 1060 ± 100 years
ВремяМагнитуда / ГлубинаРасстояниеМестоположение
Thu, 22 Oct 2020 (UTC)
2020-10-22 01:56:31 (22 Oct 07:56:31 UTC)M 2.4 / 5 km18 km12 Km Al Suroeste De Mateare, Nicaragua
Thu, 15 Oct 2020 (UTC)
2020-10-14 23:49:47 (15 Oct 05:49:47 UTC)M 1.8 / 7 km11 km9 Km Al Sur De INETER, Managua, Nicaragua
Thu, 10 Sep 2020 (UTC)
2020-09-10 12:32:49 (10 Sep 18:32:49 UTC)M 3.1 / 147 km22 km18 Km al noroeste de Diriamba, Nicaragua
2020-08-09 18:22:35 (10 Aug 00:22:35 UTC)M 2.6 / 10 km13 km5 Km al sureste de INETER, Managua, Nicaragua
Sat, 8 Aug 2020 (UTC)
2020-08-08 01:06:45 (8 Aug 07:06:45 UTC)M 1.4 / 19 km12 km4 Km al norte de INETER, Managua, Nicaragua
Просмотреть все последние землетрясения
Nejapa-Miraflores volcano is an alignment of fissure vents, maars and cinder cones extending from Lake Managua until the western part of Managua city.
About 40 eruptions have occurred from this system during the past 30,000 years, and the most recent one produced Asososca maar about 1250 years ago.

Справочная информация:

from Smithsonian / GVP volcano information:
The N-S-trending Nejapa-Miraflores alignment, located near the western margin of the Nicaraguan graben, cuts through the western part of Nicaragua's capital city, Managua.
This alignment, which has erupted tholeiitic basaltic rocks similar to those from mid-ocean ridges, marks the right-lateral offset of the Nicaraguan volcanic chain. A series of pit craters and fissure vents extends into Lake Managua and is continuous with the volcanic vents on the Chiltepe peninsula.
An area of maars and tuff cones perpendicular to the N-S trend of the lineament forms the scalloped shoreline of Lake Managua. Laguna Tiscapa crater is located several kilometers to the east near the central part of the city of Managua. The elongated Nejapa and Ticoma pit craters are surrounded by small basaltic cinder cones and tuff cones.

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