Rocks, Minerals and Volcanism

Rocks and Minerals

Rocks are aggregations of minerals. Approximately 98 percent of the earth's crust is composed of eight elements: oxygen, silicon, aluminium, iron, calcium, sodium, potassium, and magnesium. The most abundant element in the earth's crust is oxygen and the most abundant minerals are the feldspars, while the most abundant element in the entire earth is iron. Rocks are broadly classified as hard or soft depending on their resistance to erosion and weathering. Igneous and metamorphic rocks are generally harder and more resistant, while sedimentary rocks are generally softer and more susceptible to erosion.

Igneous Rocks

Igneous rocks are the parent or primary rocks of the earth, being the first to form through the cooling and solidification of magma and lava. They are crystalline in nature, with the size of crystals determined by the rate of cooling. Rapid cooling produces small or no crystals, as seen in extrusive basalt that cools quickly at the surface. Slow cooling deep within the earth allows large, well-formed crystals to develop, as seen in intrusive granite.

On the basis of depth of formation, igneous rocks are classified as extrusive, formed at the surface through volcanic eruptions, and intrusive, formed below the surface through the cooling of magma underground. Intrusive rocks are further divided into hypoabyssal rocks formed at relatively shallow depths and plutonic rocks formed at great depth. On the basis of chemical composition, igneous rocks are classified as acidic or basic. Acidic igneous rocks such as granite are rich in silica and aluminium, lighter in colour, more viscous, and associated with violent eruptions and elevated landforms. Basic igneous rocks such as basalt are rich in iron and magnesium, darker in colour, more fluid, and associated with fissure eruptions and extensive plateaus and plains. Igneous rocks do not contain fossils because the high temperatures involved in their formation destroy all organic material. They occur in compact, massive forms and are resistant to weathering.

Sedimentary Rocks

Sedimentary rocks form through the process of lithification, in which sediments derived from the breakdown of pre-existing rocks are transported, deposited, compacted, and cemented over time. They are stratified or layered, with each layer known as a bedding plane. Although sedimentary rocks cover the largest proportion of the earth's surface area, they account for only about 5 percent of the total mass of the earth's crust. They are economically significant because they contain fossil fuels, mineral ores, and serve as aquifers for groundwater storage. Because they are permeable, surface water percolates through them into underlying aquifers, making sedimentary rock regions among the richest in groundwater resources.

Physically formed or clastic sedimentary rocks result from mechanical disintegration of existing rocks, with examples including sandstone, clay, shale, and loess. Sandstone is both porous and permeable, while clay is porous but impermeable. Loess is a very fine sedimentary deposit rich in lime that is extremely susceptible to erosion. Wind deposits large amounts of loess in surrounding regions, and river systems in loess-dominated areas are known for shifting their courses and producing badland topography. The Yellow River of China, known as Hwangho, carries enormous quantities of loess eroded from the Gobi Desert, making it the muddiest major river in the world, notorious for flooding and course changes, and is called the Sorrow of China.

Chemically formed sedimentary rocks result from deposition of minerals carried in solution. Solution deposits include rock salt and halite. Carbonation produces limestone and gypsum when carbonic acid formed from atmospheric carbon dioxide and water reacts with calcium-rich rocks. Oxidation produces iron-rich reddish-brown weathering crusts, a common process in tropical and subtropical India. Organically formed sedimentary rocks derive from the decomposition of biological material. Coal forms from buried vegetation compressed over geological time. Limestone and chalk form from the accumulated skeletal material of marine organisms rich in calcium carbonate, including coral reefs.

Metamorphic Rocks

Metamorphic rocks form through the transformation of pre-existing rocks under conditions of intense heat and pressure without the rocks dissolving. The transformation alters their mineral composition and crystal structure without disintegration. A characteristic feature of metamorphic rocks is foliation, the parallel arrangement of crystals in bands. Common metamorphic rocks and their parent rocks include quartzite from sandstone, marble from limestone, slate and, at higher grades, schist from shale, and gneiss from granite. Metamorphic rocks are generally harder and more resistant than the rocks from which they were formed.

The Rock Cycle

The rock cycle describes the continuous transformation of rocks from one type to another over geological time. Magma from the earth's interior cools to form igneous rocks. Weathering and erosion break down igneous rocks into sediments that are transported and deposited, then lithified into sedimentary rocks. Both igneous and sedimentary rocks can be subjected to heat and pressure, transforming them into metamorphic rocks. Metamorphic rocks can be melted back into magma and the cycle begins again. The rock cycle is not linear or strictly sequential; rocks can transform between any types depending on the processes to which they are subjected.

Earthquakes

An earthquake is the sudden shaking of the ground caused by the release of energy accumulated along geological faults or at plate boundaries. The focus or hypocentre is the point within the earth where energy is released. The epicentre is the point on the earth's surface directly above the focus and is always the first surface point to experience the seismic waves. Earthquakes are measured by the Richter Scale, which measures the magnitude of energy released on a logarithmic scale, and the Mercalli Scale, which measures the intensity of shaking as felt at the surface.

Earthquakes are classified by depth into shallow-focus earthquakes occurring within 70 kilometres of the surface, intermediate-focus earthquakes between 70 and 300 kilometres, and deep-focus earthquakes between 300 and 700 kilometres. Shallow-focus earthquakes cause the greatest damage at the surface. Most earthquakes occur at plate boundaries where tectonic stresses are concentrated. The Circum-Pacific Belt or Pacific Ring of Fire accounts for the majority of global seismic activity. The Mid-Continental Belt, extending through the Mediterranean, Caucasus, Himalayas, and into Southeast Asia, is the second major seismic zone. Intraplate earthquakes also occur far from plate boundaries along ancient fault lines.

The distribution of earthquakes follows the distribution of plate boundaries. Convergent boundaries produce the most powerful and damaging earthquakes, especially at subduction zones. Transform boundaries such as the San Andreas fault system produce very powerful shallow earthquakes due to the lateral grinding of plates. Divergent boundaries produce relatively weaker earthquakes. Earthquakes associated with continent-continent collision zones such as the Himalayas are powerful but are not accompanied by tsunamis since the collision does not displace large volumes of ocean water.

Measuring Earthquakes and the Seismic Zonation of India

Earthquakes are measured in two ways. Magnitude measures the energy released at the source and has one value for each earthquake. Charles Richter's local magnitude scale (1935) is the logarithm of the largest wave amplitude recorded on a standard seismograph at a standard distance, so each whole number marks a tenfold increase in amplitude and about a thirty-twofold increase in energy. Because it saturates for great earthquakes, seismologists now use the moment magnitude scale of Thomas Hanks and Hiroo Kanamori (1979), based on the seismic moment: the rigidity of the rocks multiplied by the area of fault rupture and the amount of slip. Intensity measures the effects of shaking on people, buildings and the ground at a particular place, so one earthquake has many intensities. The Modified Mercalli scale (1931) and the Medvedev-Sponheuer-Karnik or MSK scale (1964), used in India, both run from I to XII, and reported intensities are mapped as isoseismal lines around the epicentre. In India the National Center for Seismology under the Ministry of Earth Sciences runs the national seismic network.

Seismic zones are demarcated by the Bureau of Indian Standards in the zoning map of IS 1893, its code for the earthquake-resistant design of structures, first issued in 1962 and revised several times since. Zones are drawn from the maximum intensity observed or expected, judged from the record of past earthquakes and their isoseismals, from the tectonic setting, including active faults, thrusts and lineaments, and from the geology. Each zone carries a zone factor, the peak ground acceleration, as a fraction of gravity, assumed in designing buildings. Until 2002 the map had five zones, I to V. The Latur earthquake of 1993, which killed about 10,000 people in Zone I, showed that no part of the peninsula is free of risk, and the 2002 edition merged Zone I into Zone II and upgraded parts of the peninsula, leaving four zones. Its map was retained in the 2016 edition.

Zone (IS 1893, 2002)	Risk	MSK intensity	Zone factor
V	Very high	IX and above	0.36
IV	High	VIII	0.24
III	Moderate	VII	0.16
II	Low	VI or less	0.10

By December 2025 the Bureau had issued a revised zonation map that adds a new highest category, Zone VI, and places the whole of Uttarakhand in it, where the 2002 map had divided the state between Zones IV and V. A national map is too coarse for planning within cities, where soft soils amplify shaking, so seismic microzonation maps local ground conditions for cities such as Delhi and Guwahati.

Tsunamis

A tsunami is a series of ocean waves generated by a sudden large-scale displacement of ocean water, most commonly caused by submarine earthquakes, but also by submarine landslides, volcanic eruptions, and meteor impacts. In the open ocean, tsunami waves have very long wavelengths and low heights and travel at speeds of up to 800 kilometres per hour, making them difficult to detect. As they enter shallow coastal waters, they slow down and increase dramatically in height, releasing enormous destructive energy onshore. Because submarine earthquakes at convergent plate boundaries produce the most violent vertical displacement of the ocean floor, these boundaries are the most tsunamigenic. The eastern coast of India is particularly vulnerable to tsunamis because it faces the Java or Sunda Trench where the Indo-Australian plate subducts beneath the Sunda (Eurasian) plate, as demonstrated by the 2004 Indian Ocean Tsunami caused by the interaction of the Indian and Burmese plates. Early warning systems using seismograph networks and ocean buoys are the primary means of tsunami hazard mitigation.

Volcanism

Volcanism encompasses all processes related to the movement of molten material within and through the earth's crust, including both the underground formation of intrusive landforms and the surface expression through volcanic eruptions and the creation of extrusive landforms. A volcano is specifically a vent or opening through which molten rock, gases, and fragmented material are expelled. The material erupted consists of water vapour and gases such as sulphur oxides, carbon dioxide, carbon monoxide, nitrogen oxides, and methane, which account for roughly 60 percent of volcanic output. Magma and lava constitute the second component, with acidic magma being silica-rich, viscous, lighter in colour, and associated with violent central eruptions, while basic magma is iron-rich, fluid, darker, and hotter, associated with quiet fissure eruptions that build extensive plateaus. Pyroclastic material or tephra, the third component, includes volcanic ash, dust, cinders, and larger rock fragments that can cause atmospheric pollution and short-term global cooling by reducing incoming solar radiation.

Intrusive Volcanic Landforms

When magma cools and solidifies underground without reaching the surface, it forms intrusive or plutonic landforms that are only exposed after overlying rocks have been removed by erosion. A batholith is the largest intrusive igneous body, generally composed of granite, found at the greatest depths and sometimes forming the core of mountain ranges. A lopolith is a saucer-shaped mass of igneous rock with a concave upper surface. A laccolith is an intrusive mound connected to the surface by a feeder pipe, creating a dome-like uplift of overlying rocks. A phacolith is a lens-shaped igneous body found in pairs at the crest of anticlines or the base of synclines, also connected by a pipe. A sill is a sheet of intrusive igneous rock injected parallel to the bedding planes of sedimentary rocks. A dyke is an intrusive igneous body that cuts vertically or at an angle across the bedding planes of surrounding rocks.

Extrusive Volcanic Landforms

Volcanic mountains form through the accumulation of erupted material. Ash and cinder cones are small, weak structures formed from loose pyroclastic material and rarely attain significant heights. Composite cones or stratovolcanoes are the tallest and most imposing volcanic mountains, built from alternating layers of lava and pyroclastic material. The solidified lava acts as cement between the ash layers, giving these cones great structural strength and resistance to erosion. Major composite cones include Cotopaxi in the Andes, Mount Rainier, Shasta, and Hood in the Cascades, Mount Mayon in the Philippines, Mount Fujiyama in Japan, and Mount Kilimanjaro, the highest peak in Africa. India's only confirmed active volcano, Barren Island, and Narcondam, generally regarded as dormant, both lie in the Andaman and Nicobar Islands. Shield cones or basic lava cones form from basaltic magma, which flows easily and spreads widely before solidifying, producing broad, low-profile structures such as Mauna Loa and Mauna Kea in the Hawaiian Islands. Parasitic cones form when secondary branches develop off the main feeder pipe of a volcano, producing numerous smaller subsidiary cones on the flanks of the main mountain.

A crater is the vent or opening at the top of a volcano through which eruption occurs. A caldera is a much larger depression formed either by the explosion of the volcanic cone or by its collapse into an emptied magma chamber. When water accumulates in a crater or caldera, it forms a crater lake. Volcanic plateaus and plains form from extensive outpourings of basaltic lava through fissure eruptions. After weathering, basaltic lava produces black soil that is highly fertile, moisture-retaining, and well suited to cash crops such as cotton. Major volcanic plateaus include the Columbia Snake Plateau of the United States, the Parana Plateau of South America, the Drakensberg Plateau of South Africa, the Siberian Plateau of Russia, the Deccan Lava Plateau of India, and the Kimberley Plateau of Australia.

Hot springs and geysers form when groundwater comes into contact with underlying magma or hot rocks, is heated, expands, and rises to the surface. In geysers, the heated water erupts periodically and with great force. The main geyser fields are in Iceland, New Zealand, Yellowstone National Park in the United States, Kamchatka in Russia, and El Tatio in Chile. When the heat is so intense that water evaporates entirely before reaching the surface, the resulting superheated steam is called a fumarole. Regions of hot springs and geysers are important for medical tourism, since sulphur-rich waters are used for treating skin conditions, and for geothermal energy generation. The United States leads the world in geothermal electricity generation, while Iceland leads in the share of its energy drawn from geothermal heat. In India, Manikaran in Himachal Pradesh is a notable geothermal site.

Pseudovolcanic Features

Pseudovolcanic features resemble volcanic craters, cones or eruptions but are not produced by magma rising from depth through a feeder conduit. The main kinds are these:

• Meteorite impact craters are circular depressions with raised rims formed by the explosive impact of a meteorite. Lonar crater in Buldhana district of Maharashtra, about 1.8 kilometres across, is a rare impact crater formed in basalt, and its saline, alkaline lake was declared a Ramsar site in 2020. Barringer or Meteor Crater in Arizona is the best known example elsewhere.
• Mud volcanoes are cones and pools built by mud, water and gas, chiefly methane, forced up from overpressured sediments along faults, mostly in compressional zones such as the accretionary wedges above subduction zones. The mud is usually cold. India's best known mud volcanoes are on Baratang Island in the Andamans, and the Caspian coast of Azerbaijan and the Makran coast of Pakistan have many. The Lusi mud flow, which began in 2006 in East Java, buried several villages.
• Pseudocraters or rootless cones form where lava flows over marsh or a shallow lake and the trapped water flashes to steam and blasts through the lava, building small craters with no conduit below. Those around Lake Mývatn in Iceland are the type example.
• Collapse craters form where the roof over a cavity in limestone, gypsum or salt falls in, giving crater-like sinkholes.
• Gas blowout craters form where gas under pressure in frozen ground bursts out, as in the craters found on the Yamal peninsula of Siberia from 2014.

They are told apart from true volcanic forms by the absence of fresh igneous material and of a feeder pipe, and in impact craters by shock-metamorphosed rock and impact glass.

World Distribution of Volcanoes

The global distribution of volcanoes is closely related to the distribution of plate boundaries. Four major volcanic zones are recognised. The Circum-Pacific Belt or Pacific Ring of Fire contains approximately 60 percent of the world's active volcanoes and represents primarily convergent plate boundaries where the Pacific plate subducts beneath surrounding plates including the Indo-Australian, Eurasian, North and South American, and Antarctic plates. It extends from Antarctica through New Zealand, the Philippines, Japan, and along the Pacific coasts of the Americas. The Mid-Continental Belt, also a convergent boundary zone, contains about 20 percent of the world's volcanoes and includes the volcanic centres of the Mediterranean region such as Mount Stromboli, Mount Etna, and Mount Vesuvius in Italy, while Mount Pelee in the Caribbean belongs to the separate Lesser Antilles island arc. The Himalayas are notably absent from this belt despite lying within the mid-continental zone, because continent-continent collision prevents the subduction necessary for volcanism. The Mid-Oceanic Belt contains about 15 percent of the world's volcanoes and represents divergent plate boundaries, producing fissure-type eruptions along mid-oceanic ridges such as those of Iceland. Hotspot volcanoes account for approximately 5 percent of global volcanic activity and occur within plate interiors far from boundaries, in regions of anomalously thin crust or high mantle temperatures. Examples include the Hawaiian Islands in the Pacific and the Reunion Islands in the Indian Ocean.

Mechanism of Volcanic Eruption and Climatic Impact

Volcanic eruptions are driven by heat generated primarily by radioactive mineral decay within the mantle, which produces convection currents that carry magma upward. At convergent boundaries, the subducting plate melts as it descends and the resulting magma is forced upward through the overlying plate under intense pressure, producing violent central eruptions. At divergent boundaries, the separation of plates creates fissures through which fluid basaltic magma rises quietly and spreads laterally, building mid-oceanic ridges and volcanic plateaus. The intensity of an eruption depends on the composition of the magma, with silica-rich acidic magma producing more explosive eruptions than fluid basic magma.

Volcanic eruptions have significant short-term and long-term climatic effects. In the short term, the injection of sulphur dioxide and ash into the stratosphere reflects incoming solar radiation, producing global cooling. The 1991 eruption of Mount Pinatubo in the Philippines caused measurable global temperature decrease in the following years. In the long term, the release of carbon dioxide contributes to greenhouse warming, making volcanoes contributors to both cooling and warming depending on the time scale of analysis. Over geological time scales, volcanic activity has been linked to episodes of mass extinction and subsequent evolutionary diversification of life forms. There is also evidence suggesting that the melting of glaciers and ice caps reduces the superincumbent pressure on the crust, potentially increasing the rate of volcanic eruptions in formerly glaciated regions, though this relationship remains an area of active research.

Phreatic Eruptions

A phreatic eruption is a steam-driven explosion that occurs when groundwater, a crater lake or the water of a hydrothermal system is suddenly heated by magma or hot rock beneath it. Water flashing to steam expands to well over a thousand times its volume, and when the pressure exceeds the strength of the overlying rock it blasts open a crater. The ejecta are shattered older rock, ash, steam and gases, with no fresh magma. This distinguishes it from a phreatomagmatic eruption, in which magma meets water directly and is itself fragmented, as in the Surtseyan eruptions off Iceland, and from a magmatic eruption driven by gases dissolved in magma. Phreatic eruptions are usually small and brief, but they can recur for weeks and may herald a magmatic eruption, as the steam explosions at Mount St Helens did from March 1980 before its great eruption that May.

Their consequences follow from this character:

• They give little warning, since no magma rises to produce clear seismic or ground-deformation signals, so they are hard to forecast.
• Near the vent, ballistic blocks, ash fall and hot, fast-moving base surges kill or injure people within a kilometre or two.
• They release carbon dioxide, hydrogen sulphide and sulphur dioxide, and ejected acid crater-lake water and ash can set off lahars on wet slopes.
• Because volcanic summits and hydrothermal fields attract visitors, the toll falls on tourists and hikers. The eruption of Mount Ontake in Japan in September 2014 left 63 people dead or missing, and that of Whakaari or White Island in New Zealand in December 2019 killed 22.

Hazard management therefore relies on monitoring gas output, crater-lake temperature and shallow seismicity, and on exclusion zones around active vents.