effusive activity वाक्य
उदाहरण वाक्य
मोबाइल
- It generated two major effusive activity succeded the caldera formation.
- Effusive activity occurred during the upper Miocene in the area.
- Effusive activity ended with small lava flows of varying composition.
- Volcanic activity at Ciomadul commenced with effusive activity about one million years ago.
- Andesitic effusive activity occurred on the flanks of the caldera before and after its collapse.
- The formation of the Alpha cone was characterized by an alternation of explosive and effusive activity.
- A second phase 137 70ka with large scale effusive activity included the " Pyramidal Peak " Volcano which dammed local rivers with lava flows.
- This effusive activity has been dated 7.59 ?0.03 and 7.6 ?0.02 million years ago.
- The third stage continued this effusive activity as well as rhyolitic domes like Cerro Botijuela and Las Cuevas ( 2.5-2.3 mya ).
- High concentrations of are found in the rock, which may have resulted in the depolymerization of the melt, increasing its fluidity and resulting in effusive activity.
- Another effusive activity generated the Carb�n Qullu lavas " ( Carbon Kollu ) " and finally the Pukara lava dome, whose collapse generated the Thuwas Ventilla pyroclastic flow.
- Other than that, potassium-argon dating has indicated effusive activity between 20 and 14 million years ago with a peak between 12.2 and 3.9 million years ago.
- The middle unit, which is early Amazonian in age, makes up the flanks of the main Alba edifice and records a time of more focused effusive activity consisting of long tube-and channel-fed flows.
- Throughout its history, volcanic activity at Furnas has been essentially explosive but eruptive styles have varied from mild effusive activity to at least two caldera-forming eruptions 30, 000 and 12, 000-10, 000 years ago.
- On the rim of the caldera left by this eruption is a lava dome complex named the Old Complex Unit . 0.3 ?0.1 mya ago effusive activity commenced with the Pre-platform and Platform units that were then followed by a tectonic event that dissected these units.
- The volcano originated as a stratovolcano in the Garigliano rift valley, with a group of eructive mouths spread in a area; later an effusive activity concentrated in the central area, forming a volcanic cone some 1, 800 m-high, mostly formed of tephra and accompanied by minor cones such as the Monte Ofelio at south-west.
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