Noun:

আন্ডেসাইট,

andesitic শব্দের বাংলা অর্থ এর উদাহরণ:

খনিজ অলিভিন, এওগিট এবং প্লাগইওক্লেস অন্তর্ভুক্ত. অগ্নিয়গিরিজাত শিলা আন্ডেসাইট বিশ্বজুড়ে সব আগ্নেয়গিরিতে পাওয়া যাবে, সেন্ট্রাল আমেরিকা সহ এবং দক্ষিণ ।

andesitic's Usage Examples:

The average composition of the continental crust is andesitic.

low-silica basaltic ash, and tuffs are likewise described as rhyolitic, andesitic, basaltic, and so on.

The main composition of the volcano is andesitic and dacitic.

The volcanoes, together with the Cumbal are andesitic in rock type.

The Nevado del Tolima is a Late Pleistocene to recently active andesitic stratovolcano located in the Tolima department, Colombia.

There are several recorded eruptions of this basaltic-andesitic stratovolcano prior to a spectacular lateral collapse which took place.

color (generally dark brown, black or purplish red), and basaltic or andesitic in composition.

Since viscous basaltic and andesitic domes weather fast and easily break apart by further input of fluid lava.

The volcano has erupted rhyolites and dacites and some andesitic lava flows on a ridge above Baeza.

Nevado del Ruiz Nevado del Tolima Puracé Doña Juana Galeras Puracé is an andesitic stratovolcano located in the Puracé National Natural Park in the Cauca.

Tenorio Volcano (Spanish: Volcán Tenorio) is an inactive andesitic stratovolcano in north-western Costa Rica.

In addition, the relative abundance of VOCs varies within basaltic, andesitic, and rhyolitic magma chambers, leading to some volcanoes being exceedingly.

The Miravalles Volcano is an andesitic stratovolcano in Costa Rica.

The dominantly andesitic-dacitic volcano is cut by two nested calderas, the larger 6–7 km in diameter.

Lauca is a 5,140 metres (16,860 ft) high andesitic stratovolcano in the Central Volcanic Zone of the Andes on the Altiplano in northern Chile.

It exposes rocks from an andesitic Precambrian volcano, similar to the 1995 Montserrat eruption, about 570.

volcano has an elevation of 1662 m and its summit is formed by three andesitic lava domes.

The Tecuamburro is an andesitic stratovolcano which formed approximately 38,000 years ago inside a horseshoe-shaped.

Oxidized andesitic scoria deposits covering the upper part of the young cone gives it a distinctive.

between thick and thin lithosphere, and is probably supplied by a pool of andesitic and rhyolitic magma.