Pashmina shawls

GS Paper: 1- Art and Culture

Important for

Prelims exam: Pashmina shawls, Chiru (Tibetan Antelope)

Why in News

Traders of universally prized Pashmina shawls are complaining that “obsolete testing methods” have resulted in many of their export consignments being flagged by Customs authorities for presence of Shahtoosh guard hair, which is obtained from endangered Tibetan antelopes.

About Pashmina

Features

Economic benefits: Pashmina is a largely unorganised cottage and handicraft industry which provides employment and livelihood to approximately six lakh people, most notably to local skilled villagers and artisans in Kashmir.

About Pashmina Shawls

Chiru (Tibetan Antelope)

Status

Shahtoosh Shawls

G20 Presidency

GS Paper: 2- Agreements involving India,International Institutions

Important for:

Prelims exam: G20 Presidency

Mains exam: Aims and Objective of G20

Why in News

The G20 presidency of India officially began on December 1 after the unveiling of the country’s logo, website, and theme by the Indian government. One Earth, One Family, One Future was Modi’s rallying cry, which was aptly emphasised by the phrase “Vasudhaiva Kutumbakam.”

C:\Users\Chanakya\Documents\PTI11_08_2022_000232B.jpg

About G20

Aims and Objectives

Global Scenario

India’s Priority

New guidelines for TV channels

GS Paper: 2 (Governance)

Important for

Prelims Exam: Authorities related to this

Mains Exam: Significance of New TV channels Guidelines

Why in News?

The Union Cabinet has approved new guidelines for uplinking and downlinking of TV channels, under which all stations holding permission except for foreign channels and where it may not be feasible will have to broadcast content on issues of national importance and social relevance for at least 30 minutes every day.

Key Points

  • Limited Liability Parterneship (LLP)
  • LLP is an alternative corporate business form that gives the benefits of limited liability of a company and the flexibility of a partnership.
  • The LLP can continue its existence irrespective of changes in partners. It is capable of entering into contracts and holding property in its own name.
  • The LLP is a separate legal entity, is liable to the full extent of its assets but liability of the partners is limited to their agreed contribution in the LLP.
  • Further, no partner is liable on account of the independent or un-authorized actions of other partners, thus individual partners are shielded from joint liability created by another partner’s wrongful business decisions or misconduct.
  • Mutual rights and duties of the partners within a LLP are governed by an agreement between the partners or between the partners and the LLP as the case may be. The LLP, however, is not relieved of the liability for its other obligations as a separate entity.
  • Since LLP contains elements of both ‘a corporate structure’ as well as ‘a partnership firm structure’ LLP is called a hybrid between a company and a partnership.

Telecom Regulatory Authority of India

New Information Technology (Intermediary Guidelines and Digital Media Ethics Code) Rules 2021 Rules 2021

New IT Rules 2021

Groundwater extraction

GS PAPER 3: Environment

Important for

Prelims Exam: Authorities and Data Related to this

Mains Exam: Conservation of Water

Why in News?

Groundwater extraction in India saw an 18-year decline, according to an assessment by the Central Ground Water Board (CGWB) made public.

Key Highlights

Central Ground Water Board (CGWB)

Central Ground Water Board (CGWB), a subordinate office of the Ministry of Water Resources, Government of India, is the National Apex Agency entrusted with the responsibilities of providing scientific inputs for management, exploration, monitoring, assessment, augmentation and regulation of ground water resources of the country. Central Ground Water Board was established in 1970 by renaming the Exploratory Tube wells Organization under the Ministry of Agriculture, Government of India. It was merged with the Ground Water Wing of the Geological Survey of India during 1972.

Availibility of water

https://d18x2uyjeekruj.cloudfront.net/wp-content/uploads/2022/04/Annual_per_capita_availability_of_water_1947-2050_estimated.jpg

Current Situation

https://d18x2uyjeekruj.cloudfront.net/wp-content/uploads/2022/04/editorial-10.jpg

Government Initiatives

Water being a state subject the projects on water conservation are planned, funded, executed and maintained by  the State Governments. Government of India supplements the efforts of the States through technical and financial assistance to them through various schemes and programmes.

Water conservation initiatives are taken up by the Central Government on continuous basis and are covered under various schemes and programmes such as Mahatma Gandhi National Rural Employment Guarantee Scheme (MGNREGS),  Atal BhujalYojana,  Pradhan MantriSinchayeeYojana (PMKSY), Atal Mission for Rejuvenation and Urban Transformation (AMRUT),  Unified Building Bye Laws (UBBL) of Delhi, 2016, Model Building Bye Laws (MBBL), 2016, Urban and Regional Development Plan Formulation and Implementation (URDPFI) Guidelines, 2014 etc.

Water management in India- Challenges and Policy initiatives Issues and  Analysis @ abhipedia Powered by ABHIMANU IAS

Earthquake

GS PAPER 1: Geography

Important for

Prelims Exam: Tectonic plates location, Faults

Mains Exam: Suggest some measure to curb the impact of earthquake on people

Why in News?

AT LEAST six people were killed when a powerful 6.6-magnitude earthquake jolted the remote mountainous region of western Nepal.

What is Earthquake?

An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth‘s lithosphere that creates seismic waves. Earthquakes can range in intensity, from those that are so weak that they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities.

Type of Faults

https://upload.wikimedia.org/wikipedia/commons/thumb/7/77/Fault_types.svg/220px-Fault_types.svg.png

A- Strike-slip faults

Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other; transform boundaries are a particular type of strike-slip fault. Strike-slip faults, particularly continental transforms, can produce major earthquakes up to about magnitude 8. Strike-slip faults tend to be oriented near vertically, resulting in an approximate width of 10 km (6.2 mi) within the brittle crust.[9] Thus, earthquakes with magnitudes much larger than 8 are not possible.

B- Normal faults

Normal faults occur mainly in areas where the crust is being extended such as a divergent boundary. Earthquakes associated with normal faults are generally less than magnitude 7. Maximum magnitudes along many normal faults are even more limited because many of them are located along spreading centers, as in Iceland, where the thickness of the brittle layer is only about six kilometres (3.7 mi)

C- Reverse faults

Reverse faults occur in areas where the crust is being shortened such as at a convergent boundary. Reverse faults, particularly those along convergent plate boundaries, are associated with the most powerful earthquakes, megathrust earthquakes, including almost all of those of magnitude 8 or more. Megathrust earthquakes are responsible for about 90% of the total seismic moment released worldwide

Tectonic Plates

New Understanding of Earth's Architecture: Updated Maps of Tectonic Plates

What causes earthquakes and where do they happen?

cartoon of cutout wedge of earth

The earth has four major layers: the inner core, outer core, mantle and crust. The crust and the top of the mantle make up a thin skin on the surface of our planet.

But this skin is not all in one piece ,t is made up of many pieces like a puzzle covering the surface of the earth. Not only that, but these puzzle pieces keep slowly moving around, sliding past one another and bumping into each other. We call these puzzle pieces tectonic plates, and the edges of the plates are called the plate boundaries. The plate boundaries are made up of many faults, and most of the earthquakes around the world occur on these faults. Since the edges of the plates are rough, they get stuck while the rest of the plate keeps moving. Finally, when the plate has moved far enough, the edges unstick on one of the faults and there is an earthquake.

Seismic Waves

Surface Waves (L-waves):

  • Complex motion (i.e. shearing)
  • Causes the greatest destruction
  • Exhibits the greatest amplitude and slowest velocity.

Body Waves – Travel through Earth’s interior.

Two types:

Primary (P-waves): Push-pull (compress and expand) motion.

Travels through solids, liquids, and gases. 2)

Secondary (S-waves): “Shake” motion at right angles to their direction of travel (i.e. shearing).

Travels only through solids (This is how we know that the outer core is a liquid).

India’s seismic zones

https://www.drishtiias.com/images/uploads/1596107581_image4.png