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VOLCANOES
DISADVANTAGES
LAHARS
Lahars - Also called ash runoff, these are mud
streams composed of pyroclastic materials
saturated with water, the source of which are
snow covers and glaciers that melt during
eruptions, intense rainfall accompanying
eruptions, and crater lakes.
Lahars cause great damage due to their high
transport force and high speed.
PYROCLASTIC AVALANCHES
Pyroclastic Avalanches - also called pyroclastic streams, they are a
turbulent mixture of pyroclastic materials and incandescent gas,
rolling rapidly down the slopes of a volcano. Like fiery clouds,
pyroclastic avalanches cause significant loss of life, damage to
infrastructure, farmland and vegetation.
LAW EFFUSIONS
When the lava temperature drops below
the freezing point, the lava flows, which
can reach a distance of up to 80 km
from the crater, stop. Effusions of lawa
cause damage similar to those caused
by pyroclastic avalanches; they are
rarely dangerous to humans
TSUNAMI
caused by eruptions of both
submarine and land volcanoes;
they are produced by the violent
discharge of pyroclastic materials
into the sea or by volcanic
earthquakes.
EARTHQUAKE
They are much weaker than tectonic quakes.
They are caused by the movement of magma in
the Earth's crust, explosions in a volcanic crater,
lava flows, etc. volcanic processes. These
quakes generally precede an eruption (by
several hours, days or even months) or occur in
its first stages.
ADVANTAGES
SOIL ENRICHMENT
Volcanic eruptions disperse
the ash over wide areas around
the eruption site. And depending
on the chemistry of the magma it
exploded from, this ash will
contain different amounts of
nutrients in the soil.
VOLCANIC
FORMATIONS
In addition to dispersing ash over large
areas of land, volcanoes also push
material to the surface, which can lead to
the formation of new islands. For
example, the entire chain of the
Hawaiian Islands was formed by the
continuous eruption of one volcanic hot
spot. For hundreds of thousands of
years, these volcanoes disrupted the
ocean's surface, becoming habitable
islands, and the rest stopped during long
sea voyages.
VOLCANIC MINERALS
AND STONES
Another benefit to volcanoes is the
precious gems, minerals, and building
materials they provide for eruptions. For
example, stones such as pumice
volcanic ash and perlite (volcanic glass)
are mined for a variety of commercial
purposes. These include acting as an
abrasive in soaps and household
cleaners. Volcanic ash and pumice are
also used as lightweight aggregates in
cement production.
DEGASSING AND
CREATING AN
ATMOSPHERE
the most beneficial aspect of volcanoes is the role they play in
creating a planet's atmosphere. In short, the Earth's
atmosphere began to form after it was formed 4.6 billion
dollars ago, when volcanic degassing led to the formation of
gases collected in the Earth's interior to collect around the
planet's surface. Initially, this atmosphere consisted of
hydrogen sulfide, methane, and 10 to 200 times more carbon
dioxide than today's atmosphere.
THANK YOU FOR
WATCHING THE
PRESENTATION

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VOLCANOES

  • 3. LAHARS Lahars - Also called ash runoff, these are mud streams composed of pyroclastic materials saturated with water, the source of which are snow covers and glaciers that melt during eruptions, intense rainfall accompanying eruptions, and crater lakes. Lahars cause great damage due to their high transport force and high speed.
  • 4. PYROCLASTIC AVALANCHES Pyroclastic Avalanches - also called pyroclastic streams, they are a turbulent mixture of pyroclastic materials and incandescent gas, rolling rapidly down the slopes of a volcano. Like fiery clouds, pyroclastic avalanches cause significant loss of life, damage to infrastructure, farmland and vegetation.
  • 5. LAW EFFUSIONS When the lava temperature drops below the freezing point, the lava flows, which can reach a distance of up to 80 km from the crater, stop. Effusions of lawa cause damage similar to those caused by pyroclastic avalanches; they are rarely dangerous to humans
  • 6. TSUNAMI caused by eruptions of both submarine and land volcanoes; they are produced by the violent discharge of pyroclastic materials into the sea or by volcanic earthquakes.
  • 7. EARTHQUAKE They are much weaker than tectonic quakes. They are caused by the movement of magma in the Earth's crust, explosions in a volcanic crater, lava flows, etc. volcanic processes. These quakes generally precede an eruption (by several hours, days or even months) or occur in its first stages.
  • 9. SOIL ENRICHMENT Volcanic eruptions disperse the ash over wide areas around the eruption site. And depending on the chemistry of the magma it exploded from, this ash will contain different amounts of nutrients in the soil.
  • 10. VOLCANIC FORMATIONS In addition to dispersing ash over large areas of land, volcanoes also push material to the surface, which can lead to the formation of new islands. For example, the entire chain of the Hawaiian Islands was formed by the continuous eruption of one volcanic hot spot. For hundreds of thousands of years, these volcanoes disrupted the ocean's surface, becoming habitable islands, and the rest stopped during long sea voyages.
  • 11. VOLCANIC MINERALS AND STONES Another benefit to volcanoes is the precious gems, minerals, and building materials they provide for eruptions. For example, stones such as pumice volcanic ash and perlite (volcanic glass) are mined for a variety of commercial purposes. These include acting as an abrasive in soaps and household cleaners. Volcanic ash and pumice are also used as lightweight aggregates in cement production.
  • 12. DEGASSING AND CREATING AN ATMOSPHERE the most beneficial aspect of volcanoes is the role they play in creating a planet's atmosphere. In short, the Earth's atmosphere began to form after it was formed 4.6 billion dollars ago, when volcanic degassing led to the formation of gases collected in the Earth's interior to collect around the planet's surface. Initially, this atmosphere consisted of hydrogen sulfide, methane, and 10 to 200 times more carbon dioxide than today's atmosphere.
  • 13. THANK YOU FOR WATCHING THE PRESENTATION