Scientists urge to protect glacial-period coastal red sand dunes

GS Paper: 1- Indian Heritage sites

Important for

Prelims exam: Erra Matti Dibbalu

Mains exam: Significance of Erra Matti Dibbalu

Why in News?

The city of Visakhapatnam is blessed with a number of sites that have geological importance. One among them is the coastal red sand dunes, popularly known as ‘Erra Matti Dibbalu’.

About ‘Erra Matti Dibbalu’

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Importance of Erra Matti Dibbalu

Geological Survey of India (GSI)

  • The Geological Survey of India (GSI) was established in 1851 with the primary goal of finding coal deposits for the Railways.
  • The GSI’s primary functions are to create and update national geoscientific information, as well as to assess mineral resources.
  • It is headquartered in Kolkata and has regional offices in Lucknow, Jaipur, Nagpur, Hyderabad, Shillong, and Kolkata, as well as State Unit offices in almost every state of the country.
  • GSI is now an attached office to the Ministry of Mines.

Indonesia’s Mount Semeru volcano erupts

GS PAPER 1: Volcanoes

Important for

Prelims Exam: About Volcanoes

Mains Exam: Implications of Volcanoes

Why in News?

Indonesia’s Mount Semeru erupted on December 4 spewing hot ash clouds a mile into the sky and sending rivers of lava down its side, sparking the evacuation of nearly 2,000 people exactly one year after its last major eruption killed dozens.

Key Points

Implication of Eruption

Mount Semeru

Volcano

A volcano is an opening in the earth’s crust through which gases, molten rocks materials (lava), ash, steam etc. are emitted outward in the course of an eruption. Such vents or openings occur in those parts of the earth’s crust where the rock strata are relatively weak. Volcanic activity is an example of endogenic process. Depending upon the explosive nature of the volcano, different land forms can be formed such as a plateau (if the volcano is not explosive) or a mountain (if the volcano is explosive in nature).

Types of Volcano

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Conical Vent and Fissure Vent : A conical vent is a narrow cylindrical vent through which magma flows out violently. Conical vents are common in andesitic (composite or strato volcano) volcanism.A fissure vent, also known as a volcanic fissure or eruption fissure, is a narrow, linear volcanic vent through which lava erupts, usually without any explosive activity. The vent is often a few meters wide and may be many kilometres long. Fissure vents are common in basaltic volcanism.

Composite Cones or Strato volcanoes:They are conical or central type volcanic landforms.Along with andesitic lava, large quantities of pyroclastic material and ashes find their way to the ground.They are accumulated in the vicinity of the vent openings leading to formation of layers, and this makes the mounts appear as composite volcanoes.The highest and most common volcanoes have composite cones.Example: Vesuvius, Mt. Fuji, Stromboli (Lighthouse of the Mediterranean) etc.

Shield Volcanoes or Lava domes:These volcanoes are mostly made up of basalt, a type of lava that is very fluid when erupted. They are not steep.They become explosive if somehow water gets into the vent; otherwise, they are less explosive.Example: Mauna Loa (Hawaii).

Lava Plains and Basalt Plateaus:Sometimes, a very thin magma escapes through cracks and fissures in the earth’s surface and flows after intervals for a long time, spreading over a vast area, finally producing a layered, undulating (wave like), flat surface.Example: Deccan traps (peninsular India), Snake Basin, U.S.A, Icelandic Shield, Canadian Shield etc.

Cinder cone (Tephra cones):Cinder cones are small volume cones consisting predominantly of tephra that result from strombolian eruptions.They usually consist of basaltic to andesitic material.

Calderas:After the eruption of magma has ceased from the cones, the crater frequently turns into a lake at a later time.Water may collect in the crater. This lake is called a ‘caldera’.Example: Lake Toba in Sumatra, Crater Lake in Oregon, USA.

Mid-Ocean Ridges:These volcanoes occur in the oceanic areas. There is a system of mid-ocean ridges more than 70,000 km long that stretches through all the ocean basins. The central portion of this ridge experiences frequent eruptions.The lava is basaltic in nature.Cools slowly and flows through longer distances.The lava here is responsible for sea floor spreading.Example: Mid-Atlantic ocean ridge; extension is seen in the Iceland.

Intrusive Volcanic Landforms: Intrusive landforms are formed when magma cools within the crust. The intrusive activity of volcanoes gives rise to various forms.

Batholiths:These are huge mass of igneous rocks, usually of granite.These rock masses formed due to cooling down and solidification of hot magma inside the earth.They appear on the surface only after the denudation processes remove the overlying materials and may be exposed on surface after erosion.Example: Wicklow mountains of Ireland; the uplands of Brittany, France.

Laccoliths:These are large dome-shaped intrusive bodies connected by a pipe-like conduit from below.These are basically intrusive counterparts of an exposed domelike batholith.Example: The laccoliths of Henry mountains in the Utah, USA.As and when the lava moves upwards, a portion of the same may tend to move in a horizontal direction wherever it finds a weak plane.In case it develops into a saucer shape, concave to the sky body, it is called Lopolith.Example: The Bushveld lopolith of Transvaal, South Africa.

Phacolith:A wavy mass of intrusive rocks, at times, is found at the base of synclines or at the top of anticline in folded igneous country.Such wavy materials have a definite conduit to source beneath in the form of magma chambers (subsequently developed as batholiths). These are called the Phacoliths.Example: Corndon hill in Shropshire, England.

Sills:These are solidified horizontal lava layers inside the earth.The near horizontal bodies of the intrusive igneous rocks are called sill or sheet, depending on the thickness of the material.The thinner ones are called sheets while the thick horizontal deposits are called sills.Example: Great whin sill of NE England

Dykes:When the lava makes its way through cracks and the fissures developed in the land, it solidifies almost perpendicular to the ground.It gets cooled in the same position to develop a wall-like structure. Such structures are called dykes.These are the most commonly found intrusive forms in the western Maharashtra area. These are considered the feeders for the eruptions that led to the development of the Deccan traps. Cleveland Dyke of Yorkshire, England.

India tops index on social hostilities relating to religion

GS Paper: 2- Social Issues

Important for

Prelims exam: Social Hostilities Index (SHI)

Mains exam: Social Hostilities Index (SHI), Religious intolerance

Why in News?

India ranked relatively low in the Government Restrictions Index (GRI) measures government laws, policies and actions that restrict beliefs and practices.

About Social Hostilities Index (SHI) 

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How terribly has India fared?

Government Restrictions Index (GRI)

Official Data

RUSSIAN OIL PRICE CAP

GS PAPER 2: Global groupings

Important for

Prelims Exam: About Russian oil cap

Mains Exam: Significance of Russian oil cap

Why in News?

The European Union, G7, and Australia have decided to cap the price of Russia’s oil exports at $60 per barrel in an attempt to limit the fossil fuel earnings that support Moscow’s budget, its military and the war in Ukraine.

What is the price cap and how would it work?

How would oil keep flowing to the global economy?

What effect would different cap levels have?

What is Russia and other countries won’t go along?

What about the EU embargo?

India’s aviation safety ranking

GS Paper: 3- Economy

Important for

Prelims exam: India’s aviation safety ranking

Mains exam: India’s aviation safety ranking and International Civil Aviation Organization (ICAO)

Why in News?

With the country getting its highest-ever rank in the ICAO aviation safety rankings, DGCA chief Arun Kumar said the challenge now is to maintain and further improve the air safety ecosystem.

Key highlights

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About International Civil Aviation Organization (ICAO)