Volcanic eruptions occur mostly in two ways viz.
i) violent and explosive type of eruption of lavas, volcanic dust, volcanic ashes and fragmental materials through a narrow pipe and small opening under the impact of violent gases and
ii) quiet type or fissure eruption along a long fracture or fissure or fault due to weak gases and huge volume of lavas.
Thus on the basis of nature and intensity of eruptions volcanoes are divided into tow types
a) Central eruption type or explosive eruption type
b) Fissure eruption type or quiet eruption type
Volcanoes of Central Eruption type:
Central eruption type or explosive eruption type of volcanoes occur through a central pipe and small opening by breaking and blowing off crustal surface due to violent and explosive gases accumulated deep within the earth. The eruption is so rapid and violent that huge quantity of volcanic materials consisting of lavas, volcanic ashes and dust fragtmental materials etc. are ejected up to thousands of meters in the sky. These materials after falling down accumulate around the volcanic vent and form volcanic cone of various sorts. Such volcanoes are very destructive and are disastrous natural hazards. Explosive volcanoes are further divided into five sub-types on the basis of difference in the intensity of eruption, variations in the ejected volcanic material and the period of the action of volcanic events as given below:
i. Hawaiin type of volcanoes: Such volcanoes erupt quietly due to less viscus lava and non-violent nature of gases. Rounded blisters of hot and glowing mass / ball of lavas (blebs of molten lava) when caught by a strong wind glide in the air like red and glowing hairs. The hawaiin people consider these long and glassy threads of red molten lava as Pele's hair (pele is the Hawaiin goddess of fire). Such volcanoes have been named as Hawaiin type because of the fact that such eruptions are very common occurance on Hawaii island. The eruption of Kilavera volcano of the southern Hawaii island in 1959-60 continued for 7 days (from Nov 14-20, 1959) when about 30 million cubic meter of lava poured out. The intermittent eruptions continued up to Dec 21, 1959, when the volcano became dormant. It again erupted on Jan 13, 1960 and about 100 million cubic meters of lavas were poured out of one km long fissure.
ii. Strombolian type of volcanoes: Such volcanoes, named after Stromboli volcano of Lipari island in the Mediterranean Sea, with moderate intensity. Besides lava, other volcanic materials like pumice, scoria, bombs etc. are also ejected up to grated hight in the sky. These materials again fall down in the volcanic craters. The eruptions are almost rhythmic or nearly continuous in nature but sometime they are interrupted by long intervals.
iii. Vulcanian type of volcanoes: These are named after Vulcano of Lipari island in the Mediterranean Sea. Such volcanoes erupt with great force and intensity. The lavas are so viscous and pasty that these are quickly solidified and hardened between two eruptions and thus they crust over (plug) the volcanic vents. These lava crusts obstructs the escape of violent gases break and shatter the lava crusts into angular fragments and appear in the sky as ash-laden volcanic clouds of dark and often black colour assuming a Convoluted or cauliflower shape.