Ella Vassina
Presentation for pupils of the senior group on the topic "Volcano"

Target:

Introduce children to nature volcano.

Tasks:

1- to promote the development of cognitive activity in children, the desire for independent knowledge and reflection;

2- improve the ability to work with various materials, show a desire for transformation, be creative in solving problems.

"I spit fire and lava,

I am a dangerous giant

I am glorious with bad fame,

What is my name?"

On a spaceship you can get into space, from where our planet is clearly visible. It is very large and looks like a ball.

Deep below us, inside our planet, the earth is so hot it looks like porridge.

Our Earth has water (seas, rivers and oceans) and land (she's dry). We live on land. On land there are high mountains. Have you seen mountains? The dry land is solid. But this is only from above, and deep inside the Earth it is so hot that even stones melt.

Word « VOLCANO» means in Latin "the fire" and "flame". So named

one of the ancient Russian gods - the god of fire and blacksmithing.

Volcanoes there are erupting

on the land…

There are also underwater...

"Sleepers" volcanoes little different from other mountains.

But sometimes they "wake up" and then, the strong begins

underground roar, from their peaks bursts of flame, ashes, red-hot

stones, volcanic bombs.

At the eruption volcano magma comes to the surface, it is also

called LAVA.

The channel through which magma rises is called

vent volcano.

Pieces of frozen lava - pumice. Look how interesting she is. There are air bubbles inside this stone. This is because the lava boiled and seethed, and then froze like that.

Volcanoes look beautiful but they are very dangerous. After all, fiery lava porridge,

pouring out of the mountain, it can destroy the cities where people live, set fires.

Scientists who monitor the state volcanoes and can often predict the start of their eruptions called volcanologists.

Where fire flies from the mountain,

And smoke from all sides

There's a dangerous hooligan

re-awakened (Volcano)

On that big mountain

The character is quiet for the time being.

But it might happen...

Explode, smoke (Volcano)

From a dream the mountain woke up

Boiled, boiled.

And from the cap shot up

Lots of smoke, soot, ash.

Lava pours like honey, thick.

What is the name of the mountain (Volcano)

Related publications:

Synopsis of direct educational activities in the educational field "Artistic and aesthetic development" with children 5-6.

• Volcanic eruptions remind us of the formidable and indomitable forces that are hidden in the bowels of the Earth.

• The mystery of the causes of volcanism has always aroused fear and keen interest among people, and the tragic consequences of eruptions forced them to explore this element.

• Volcano formation

• When a magma chamber forms in the bowels of the Earth, molten liquid magma presses down on the tectonic plate with such force that it begins to crack. Magma rushes upward along cracks and faults, melting through the rock and expanding the cracks. This is how the exit channel is formed. It passes in the center of the volcano, along it molten magma pours out from the vent of the volcano outward in the form of fiery liquid lava. The products of the eruption - pumice, lava, tuffs - settle on the slopes of the volcano, forming a cone. At the top of the volcano is a depression - a crater. At the bottom of the crater, you can see the vent of the volcano - the opening of the outlet channel, through which ash, hot gases and water vapor, lava and rock fragments erupt. Volcano vents can be gaping - empty or filled with molten lava. If the lava solidifies in the vent, then a solid plug is formed, which can only be broken by a strong volcanic eruption, and a powerful explosion occurs.

• Types of volcanoes

• active volcanoes

• Volcanoes spew molten rock, ash, gases, and rocks from time to time. This is because deep below them is a magma chamber, similar to a huge furnace, in which rock is melted, turning into fiery liquid lava.

• Those volcanoes are also considered active, the eruptions of which have been preserved any evidence in the history of mankind.

• Extinct volcanoes

• Extinct volcanoes were active only in prehistoric times. The hearth beneath them has long been extinguished, and they themselves are so badly destroyed that only geologists' studies reveal traces of ancient volcanic activity.

• dormant volcanoes

• Sleeping volcanoes have not erupted in historical time, but at any moment their catastrophic eruption may begin, because the magma chamber under them has not died out. Sleeping volcanoes show signs of life: they can smoke, smoke comes out of their crater, gases and steam are released from cracks in the mountain, hot springs beat. The longer a dormant volcano is at rest, the more dangerous it is: the power of its explosive awakening can be catastrophic.

• Eruption types

• explosive eruptions

• A volcano explosion occurs when volcanic gases are released from thick magma. During such eruptions, the tops of the mountains are destroyed and millions of tons of ash are thrown into the sky to a great height.
• Ashes, gases and steam rise into the sky for tens of kilometers in the form of curly clouds.

• Effusive eruptions

• During an effusive volcanic eruption, liquid lava spreads freely with the formation of lava flows and covers

• extrusive eruptions

• A huge amount of burning gases and red-hot lava dust are ejected from the crater of the volcano. Spreading around the volcano with great speed, this scorching cloud instantly burns everything over a very large area.

• Eruption products

• Everything that comes out of the bowels of the Earth during volcanic eruptions is called eruption products.

• They are liquid, solid and gaseous.

• The liquid products of the eruption include lava.

• Lava is magma that has erupted onto the surface of the earth

• Types of lava flow.

• It has a smooth or slightly wrinkled surface and is composed of liquid lava. Solidifying, such lava forms a flat, smooth surface, sometimes with long wriggling wrinkles in the form of snakes and thick ropes, ropes. It is often called “rope lava”.

• It has an uneven surface with cracks. Such lava is very thick and viscous, so the flow moves slowly. When the lava begins to cool, it cracks into pieces, but they continue to move like clockwork on the hot lava that has not yet had time to cool. The upper hardened layer of lava resembles piles of slag, which is formed from the combustion of coal.

• Lava flow "ah-ah"

• Lava flow "pa-hoe-hoe"

• pyroclasts

• Fragments of rocks that are scattered by gases during volcanic eruptions are called pyroclasts

• Volcanic gases

• Volcanic phenomena are associated with the action of gases. If the magma is very liquid, the gases are released unhindered and do not threaten to explode. Gases can foam even viscous magma, forming porous pumice, spray magma into small particles - volcanic ash and sand - and, combining with them, form a deadly scorching cloud.
• And finally, gases can scatter rock fragments hundreds of meters from the mouth of a volcano.

• Volcanoes in Kamchatka

• Volcano Nameless

• Bezymyanny volcano is located near Klyuchevaya Sopka. He was considered extinct, and the power of his awakening was gigantic. On March 30, 1956, a terrible explosion demolished the entire upper part of the volcano. Clouds of ash shot up almost 40 km, from

• A powerful jet of hot gas, volcanic sand and ash escaped from the vent, which burned out all the vegetation for 25 km around the volcano. A lava dome began to grow from the craters. Now the base of this dome is 750 m, and the height is 320 m. Fortunately, despite all the fury of the eruption, no one died - not a single living soul was during the hours of the eruption within a radius of 45 km from the volcano.

• Tolbachinskaya Sopka

• Tolbachik Volcano is a very active volcano. At its summit, 3,085 meters high, there was a huge caldera with a crater 300 meters in diameter and 150 meters deep. From time to time, a small lake of red-hot lava appeared in the crater. In 1975-1976, an Icelandic-type fissure eruption occurred. It continued continuously for 520 days.

• In a very short time, many cracks more than a kilometer long were formed. All this was accompanied by flooding and gushing of lava. During the eruption of Tolbachik, two cubic kilometers of volcanic products were ejected from the depths of the Earth to the surface. This is the largest known volcanic eruptions in Kamchatka and the Kuril Islands.

• Volcano in the Philippines

• Mayon Volcano, the most active on the island of Luzon. On October 23, 1776, he caused the death of 2,000 people when a huge amount of lava was thrown out of his crater.

• Volcano Mayon

• Mayon's longest eruption was observed in 1897. It lasted from 23 to 30 June and claimed 400 lives.

• Volcanoes of the Mediterranean

• Volcano Stromboli

• In southern Italy, near the island of Vulcano. The volcano island of Stromboli is located. It has a very restless character, and it has been operating for several millennia almost without interruption. From time to time explosions occur in its crater, and hot slag and volcanic bombs fly upwards for tens, and sometimes hundreds of meters, but lava usually does not flow from it.

• One of the most powerful eruptions of Stromboli was noted in 1930, and at the beginning of the fifteenth century there were already seven of them.

• Volcanoes of the Atlantic

• In the south of Iceland is the volcanic mountain range of Laki, in which there are more than a hundred cones.
• The ridge reaches a height of 818 m and a length of 25 km.

• June 8, 1783.
• Not far from the town of Vatnajo-kull in the southeast of Iceland, a powerful eruption of the Laki volcano began. It lasted 8 months, the length of the flow of lava erupted into the light was almost 70 kilometers, and the volume of this mass, moving at a speed of over 45 km / h, was 12,000 cubic meters and occupied an area of ​​579 square kilometers.

• Volcano Lucky

• Volcanoes of Africa

• Mount Kilimanjaro

• Kilimanjaro is a volcanic mountain range in eastern Africa.
• The array consists of three peaks - Kibo, Mawenzi and Shira. The Mawenzi and Shira volcanoes have long gone extinct, and Kibo continues to smoke with volcanic gases through holes in the slopes.

• Volcanoes of the Pacific

• Volcano St. Helens

• In North America, in the Cordillera, Mount St. Helens is perhaps the lowest among other peaks - its height is only 2950 meters.
• On March 20, 1980, four powerful tremors shook the area, and on March 27, 47 tremors with a force of up to three points. At noon of the same day, a deafening explosion was heard near the very top.
• This monstrous explosion claimed the lives of 62 people.

Working with a geographic map

• Show the following volcanoes on the map:
• Nameless, Tolbachinskaya Sopka, Mayon, Stromboli, Lucky, Kilimanjaro, St. Helens
• Show on the map the volcanoes that have erupted in the past year

• Questions about the material covered

• 1. What are volcanoes?

• 3. What types of eruptions do you know?

• 5. What are the products of an eruption?

• 2.How are volcanoes formed?

• 4. Give a brief description of each type of eruptions.

Technological map Task 1

I want to know

What is a volcano ?

• Volcano- (from Latin vulcanus - fire, flame), a conical mountain, from the neck of which hot gases, steam, ash, rock fragments are ejected, as well as powerful streams of red-hot lava that spread over the surface of the earth.
• A volcano is a geological formation on the surface of the earth's crust or the crust of another planet, where magma comes to the surface, forming lava, volcanic gases, and stones.
• Volcanoes are mountains of a conical shape, composed of the products of their eruption.

Technological map Task 2.

A volcano is………………………………………………………………………………………...

…………………………………………………………………………………………………… ...

………………………………………………………………………………………………… .....

The structure of the volcano

• A magma chamber is a place under the earth's crust

where magma collects.

• The vent of a volcano is a channel through which magma rises.
• A volcano crater is a bowl-shaped depression on the top of a mountain.
• Lava is erupted magma.

Technological map Task 3 Complete the scheme "Structure of the volcano"

Eruption- this is the exit to the surface of the planet of the molten substance of the earth's crust and mantle of the Earth, called magma .

Historic catastrophe of volcanic origin

K. Bryullov "The Last Day of Pompeii"

Causes of volcanic eruptions

Earthquake;

Pressure drop in the magma chamber. And with a sudden decrease in pressure, the magma melts, the gases expand and rush out.

Signs of a volcanic eruption

Volcanic eruption is almost always predictable. The most characteristic signs of the "awakening" of the volcano are:

• - increased gas output and

mineral waters on it

• - temperature rise;
• - underground noise.

Types of volcanic eruptions

If gases are released from the magma relatively quietly, then it pours out to the surface, forming lava flows. This eruption is called effusive.

If the gases are released quickly, the magmatic melt seems to flash up instantly and it is torn apart by expanding gas bubbles.

There is a powerful

explosive eruption,

which received

title explosive.

If the magma is very viscous and its temperature is low, then it is slowly squeezed out to the surface. Such an eruption is called extrusive.

Volcano types

Most common central type volcanoes is a hill, mountain or hill with a depression at the top – crater , from which magma comes to the surface. thrown out during a volcanic eruption

fragments of rock from it,

ash, pouring lava

remain on its slopes.

The height of the mountain increases

Xia, and with it the crater

moving higher and

Another type of volcanoes - linear, or fissure . Their occurrence is associated with the rise of liquid basalt magma along a crack in the earth's crust. Liquid lava spreads over vast areas, forming lava sheets. Such a volcano looks like a crack on the surface of the Earth.

active volcanoes

Krakatoa

Fujiyama

Klyuchevskaya Sopka

Extinct volcanoes

kilimanjaro

TEST

1. A geological formation that occurs above channels and cracks in the earth's crust, through which ash, lava, hot gases, water vapor, rock fragments erupt onto the earth's surface

a) an earthquake

b) sea quake

c) a volcano

2. The word "volcano" comes from the name of the ancient Roman god:

a) the underworld

3. Find two causes of a volcanic eruption

a) a flood

b) earthquake

c) pressure drop in the magma chamber

d) tsunami

4. Find three signs of a volcanic eruption

a) increased output of gases and mineral waters;

b) temperature increase;

c) underground noise.

d) lowering the temperature

5. Choose the wrong classification of volcanoes a) by shape b) by the amount of erupted lava c) by activity

d) by location

Answers to the test

3 - b, c

4 - a, b, c

Homework

Chapter 2, clause 5, tasks from the technological map Task of a creative nature:

(optional and optional)

make a model of a volcano;

make a selection of facts about a volcanic eruption

Volcanologists and geomorphologists study the features of volcanoes and the phenomena of volcanism.

Structure: hearth, vent, crater. A focus is a place in the earth's crust or mantle. A vent is a channel through which magma rises. A crater is a hole, a funnel, a bowl on the top of a mountain-volcano.

Volcanoes are classified by location, shape and activity.

By activity: extinct, dormant, active. Such a classification is rather conditional. The extinct ones have not erupted for more than 1000 years: they retain their general shape, the crater and slopes undergo changes. Sometimes they are active. Example: Mont Pele on Martinique, the Valley of Volcanoes in Buryatia, Kalara volcanoes.

Sleeping volcanoes are volcanoes in which the probability of an eruption is higher than that of extinct ones. Some of them are called supervolcanoes - Toba in Sumatra, Taulo in New Zealand, volcanoes of Kamchatka.

Active ones are the main object of interest for volcanologists; they erupt frequently. They are located in the belts of young mountains, where mountain building continues. There is no consensus among scientists on how to accurately classify these geological formations. The most active volcanism: South and Central America, Hawaii, Japan, Sunda Islands.

Classified by location: subglacial, terrestrial, underwater. According to the shape, types are distinguished: domed, cinder cone, thyroid, stratovolcano, complex view.

On the basis of the general design, formations of the central and linear types are distinguished. The former have a central channel through which lava comes to the surface. The second type is fissure, the channels through which the lava rises have an elongated shape. Scientists distinguish an areal type, but such types have not been recorded on Earth, at least in our time. It is believed that they existed when the planet was forming.

The eruption is considered an emergency, a catastrophe. It can happen an hour, a month, a year, several years. The consequences of the eruption: the formation of depressions-calderas, geysers, fumaroles. There may be low mountains, islands. Lakes form in craters.

Types of eruption: Hawaiian (basalt lava comes to the surface, accompanied by smoky clouds, fire avalanches), hydroexplosive (a lot of steam is released, confined to water bodies).

A mud-type volcano is a formation, as a result of which mud, gases, and not magma, come to the surface. They are found on the territory of Russia, Central Asia.

The largest formations: San Pedro, Cotopaxi, Ojos del Salado in the Andes, Elbrus in the Caucasus, Fujiyama in Japan, Etna and Vesuvius in Italy, Klyuchevskaya Sopka in Kamchatka.

Fixed not only on Earth. If on other planets of the solar system and their satellites.