Volcanoes

Endogenic forces

Reason — Endogenic forces originate from the interior of the Earth and are responsible for landform-building processes such as earthquakes, volcanic eruptions, mountain building, and plate movements.

Volcano

Reason — A volcano is a vent in the earth's crust from which fiery hot magma erupts from the earth's interior.

Heat from the sun

Reason — Volcanic eruptions are caused by internal heat, pressure, plate tectonics, and magma movement, not by the Sun's heat, which is an external force.

Vent

Reason — A volcano erupts steam, gases, lava, ash, dust, and other solid and liquid materials. A vent is not an eruptive product but the opening through which lava reaches the surface.

Caldera

Reason — During repeated eruptions the summit of a volcano may be blown up and in its place a large depression called caldera is formed.

Both A and R are true and R is the correct explanation of A.

Explanation — The earth's crust is made up of a series of movable plates. When these plates slide past each other or collide against each other due to intense heat inside the earth's core, their edges produce faults along the lines of weakness. It is along these plate boundaries that the crust is weakened and through which the hot magma gushes out leading to volcanic eruption.

Geysers

Reason — A geyser is a fountain of hot water and steam that escapes when underground water comes into contact with hot volcanic rocks.

Extinct Volcano : Mt. Etna

Reason — Mt. Etna in Italy is an example of an active volcano, which is presently in an active state and has erupted in the recent past.

Both A and R are true but R does not explain A.

Explanation — Steam is the most abundant gas released during a volcanic eruption. During violent eruptions, volcanic materials of varying sizes are ejected. Both statements are true, but the reason does not explain why steam is the most abundant gas.

Tsunami

Reason — Volcanoes create landforms, provide geothermal energy, and promote tourism. Tsunamis caused by volcanic eruptions are destructive, not constructive.

Pacific Ring of fire

Reason — The Circum-Pacific Belt, also known as the Pacific Ring of Fire, contains over 80% of the world's active volcanoes and lies along major earthquake zones.

Mid-world Mountain Belt

Reason — Mt. Vesuvius, Mt. Etna and Mt. Stromboli, the famous active volcanoes, are located in the Mid-world Mountain Belt.

Hot springs

Reason — Hot springs, which contain many dissolved minerals, are also known as Thermal Springs.

A is true but R is false.

Explanation — Lava and volcanic ash weather over time to form mineral-rich, fertile soil, making volcanic regions highly productive for agriculture. Although fresh volcanic ash may temporarily damage crops, it does not permanently make land unsuitable for cultivation.

The Pacific Ring of Fire is near the earthquake belt around the young fold mountains. It is called so because over 80% of the total number of active volcanoes are concentrated in this region. Among these are included 40 active volcanoes in Andes, over 100 in the Philippines, 70 in Indonesia and 40 in Japan.

A volcano is a vent in the earth's crust from which fiery hot magma erupts from the earth's interior. For example, Mt. Stromboli in Italy.

Active volcano - Mt. Etna in Italy
Dormant volcano - Mt. Kilimanjaro in Africa

The molten material while still under the earth's surface, melts weak rocks and creates a huge chamber for itself. Fresh magma continues to pour inside the chamber. This is known as magma chamber.

A volcano erupts a number of products like steam, gases, molten rock, dust, ashes and other liquid and solid matter.

Two types of landforms made by volcanoes are-

1. Volcanic Plateaus — For example, Plateau of Peninsular India
2. Volcanic mountains — For example, Mauna Loa in Hawaii

The two causes of volcanic eruptions are-

1. Heat and Pressure inside the Earth — Temperature and pressure increase towards the Earth's interior. The intense heat melts rocks into magma, and the built-up pressure forces the magma to escape through cracks and fissures in the Earth's crust.

2. Plate Tectonics — Most volcanoes occur along plate boundaries. When tectonic plates collide, separate, or slide past one another, weaknesses develop in the crust, allowing magma to rise to the surface and erupt.

The two types of volcanoes are-

1. Active volcanoes — These are the volcanoes which are presently in active state and which have erupted in the recent past. For example, Mt. Etna in Italy.

2. Dormant volcanoes — These volcanoes have not erupted in recent historical period. They may become active at any time. For example, Mt. Kilimanjaro in Africa.

(i) Many volcanoes are found along plate boundaries because when tectonic plates slide past each other or collide against each other due to intense heat inside the earth's core, their edges produce faults along the lines of weakness. It is along these plate boundaries that the crust is weakened and through which the hot magma gushes out leading to volcanic eruptions.

(ii) Volcanic mountains are the most diverse mountains in the world because there are great differences in volcanic eruptions as well as materials they throw up.

(iii) Hot springs have medicinal properties to cure skin diseases since they are a rich source of sulphur.

The landforms created by volcanoes on the surface of the earth are-

1. Volcanic Plateaus — These are derived from lava which flows from volcanic eruptions. For example, Columbian Plateau.

2. Volcanic Mountains — These mountains are built from material ejected from the fissures of the earth's crust. For example, Mauna Loa in Hawaii.

3. Volcanic Plains — These plains are formed by extensive volcanic flooding from volcanic centres. For example, Victorian Plains in Victoria.

4. Caldera Lake — A large depression at the summit of a volcano is called a caldera. When this depression gets filled with water, it forms a lake known as caldera lake. For example, Crater Lake in USA.

5. Hot springs — The movement of magma in the interior of the earth heats up underground water particularly around magma chambers. When water turns into steam, it gushes up to the surface. Hot springs are a rich source of sulphur. For example, hot springs at Manikaran in Kullu Valley, Himachal Predesh.

6. Geysers — It is a fountain of hot water and steam that escapes when underground water comes into contact with hot volcanic rocks. For example, the Old Faithful geyser in Wyoming, USA.

Three destructive effects of volcanoes are-

1. When the volcanoes erupt they destroy life and property. The hot lava together with ash and dust destroy not only human beings but also animals as well as plant life.
2. Agricultural fields are covered with layers of volcanic ash and dust making them unsuitable for cultivation.
3. Huge clouds are formed after the eruption of volcanoes causing heavy rains which result in floods and landslides.

(i) Volcanic Cone — The erupted fluid material being hot collects around the vent and begins to cool gradually and solidifies. The accumulation of material around the vent gives to the volcano its typical cone-like shape known as a volcanic cone.

(ii) Caldera — A large depression at the summit of a volcano is called a caldera.

(iii) Geyser — It is a fountain of hot water and steam that escapes when underground water comes into contact with hot volcanic rocks. For example, the Old Faithful geyser in Wyoming, USA.

Volcanoes are found along the weak zones of the earth’s crust where due to continuous tussle by tectonic forces maximum active volcanoes have created. The important volcanic zones of the world are-

1. Circum-Pacific Belt — The volcanoes occur near the earthquake belts around the young fold mountains. It is also known as 'Pacific Ring of Fire' because over 80% of the total number of active volcanoes are concentrated in this region. Among these are included 40 active volcanoes in Andes, over 100 in the Philippines, 70 in Indonesia and 40 in Japan.

2. Mid-World Mountain Belt — Mt. Stromboli, Mt. Vesuvius and Mt. Etna are located in the Midworld Mountain Belt. The only active volcano in India, in Andaman and Nicobar Islands is also located in this belt. The Hawaiian Islands, Canary Islands, Mt. Kenya are all in the Midworld Mountain belt.

If an extinct volcano erupted during a holiday, it could have significant consequences. Here are some of the potential outcomes:

1. Lava flows — The eruption could produce fast-moving lava flows, which could endanger the lives of the people and cause damage to properties.
2. Ash clouds — The volcanic ash cloud could disrupt flights, causing travel chaos for tourists. It could also cause respiratory problems for people with pre-existing health conditions.
3. Landslides and mudflows — The eruption could trigger landslides and mudflows in the surrounding areas.
4. Environmental damage — The eruption could have long-term environmental effects, such as damage to vegetation, wildlife habitats, and ecosystems. Climate changes could also result from the eruption.
5. Economic impact — The eruption could cause significant economic losses for the tourism industry in the region.
6. Emergency response — The eruption would require an emergency response to evacuate people from the area and provide them with basic necessities such as food, water, and medical supplies.

One day, when I was sitting in my balcony, I suddenly noticed a volcano erupting at a distance. It was a horrifying sight.

1. I saw a plume of ash rising from the volcano. It was a thick, dark cloud that blocked out the sun.
2. Bright orange lava sprouted out of the volcano and started flowing down the side of the volcano.
3. There were also explosions of ash and rock from the volcano, which created a loud booming sound and sent debris flying through the air.