{GS1 – Geo – PG – Geomorphology} Puga Hot Spring
- Context (PIB): A study identifies Puga Hot Spring, Ladakh, as a potential site to understand the origin of life and aid Mars life-detection, owing to its extreme geothermal and organic-preserving conditions.
About Puga Hot Spring
- Location: Puga Valley is located in the Changthang Plateau, in the southeastern part of Ladakh, within the Union Territory of Ladakh, India.
- Geothermal Significance: Part of the Himalayan geothermal belt, known for intense hydrothermal activity.
- Key Features: Hot springs, mud pools, sulphur deposits, and surface temperatures reaching up to 84°C, indicating intense geothermal activity.
- Rich in borax, sulphur, and lithium; forms travertine deposits through continuous CaCO₃ precipitation, which helps preserve organic molecules.
Puga’s Role in Origin of Life Studies
- Travertine deposits at Puga preserve amino acids, formamide, and fatty acids, confirming CaCO₃’s role in stabilising prebiotic organic molecules.
- Acts as a natural prebiotic reactor, offering insights into the origin of life on Earth.
- Serves as a Mars analogue, aiding ISRO’s life-detection tools for future planetary missions.
- Prebiotics are a type of non-digestible fibre that acts as food for the beneficial bacteria in your gut.
- Travertine is a form of terrestrial limestone deposited around mineral springs.
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{GS2 – Governance – Issues} Governance Lapses in Ladki Bahin Welfare Scheme
- Context (IE): Over 26 lakh ineligible beneficiaries, including 14,000 men, received funds under Mukhyamantri Majhi Ladki Bahin Yojana, exposing ethical breaches, poor targeting, and administrative lapses.
Ethical and Administrative Concerns
- Breach of Public Trust: Misuse of funds meant for underprivileged women violates the scheme’s intent, highlighting ethical lapses by both beneficiaries and administrators.
- Leakage in welfare schemes: It reflects weak digital governance, marked by poor Aadhaar-seeding & inadequate inter-departmental data sharing.
- Administrative Vigilance: The absence of strong cross-verification mechanisms before disbursal shows a failure in due diligence & accountability.
- Politicisation of Welfare: Announced close to elections, the scheme served as a vote-pulling tool, raising concerns about populist policymaking & fiscal irresponsibility.
- Targeting Failures: Inclusion of lakhs of ineligible recipients indicates flawed targeting, potentially excluding genuine beneficiaries.
Way Forward
- Digital Beneficiary Mapping: Integration of Aadhaar, income tax, & welfare databases while using AI/ML-based eligibility validation models.
- Gender-Specific Digital Filters: Use gender authentication tools at onboarding to detect & prevent male inclusion in women-centric schemes.
- Citizen Oversight: Establish quarterly audit bodies involving officials, civil society, and data experts to ensure local transparency.
- Rationalisation of Scheme Overlaps: Undertake a policy audit to reduce welfare duplication and improve progressive targeting.
{GS3 – IE – Banking} Minimum Average Balance Penalties
- Context (IE): The Department of Financial Services (DFS) advised Public Sector Banks (PSBs) to review penalties for not maintaining the minimum average balance (MAB).
About Minimum Average Balance Penalties
- MAB penalties are fees charged by banks when an account holder does not maintain the required monthly average balance in their savings account.
- Monthly Average Balance is the average of daily closing account balances over a month.
- Purpose: It incentivises account holders to maintain stable balances, improving banks’ CASA ratio.
- Penalty Revenue: PSBs earned approximately ₹9,000 crore from MAB penalties over five years.
- Penalty Basis: MAB thresholds and penalties are set individually by banks within RBI guidelines.
- Penalty Calculation: It varies by bank and account type; penalties can be fixed or calculated as a percentage of the shortfall from the required MAB.
- Customer Implication: Heavy penalties disproportionately impact low-income users, prompting a shift away from formal banking towards fixed deposits or informal cash
- Current Account Savings Account (CASA) ratio is the proportion of a bank’s total deposits held in low-interest current and savings accounts. A higher CASA ratio reduces banks’ cost of funds, improving profit margins on lending.
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{GS3 – IE – Banking} Banking Laws (Amendment) Act, 2025
- Context (PIB): The Banking Laws (Amendment) Act, 2025, comes into effect from August 1, 2025, aiming to modernise & strengthen governance and regulatory frameworks across India’s banking sector.
- The Act introduces 19 amendments across five key laws—the RBI Act (1934), Banking Regulation Act (1949), SBI Act (1955), and the Banking Companies Acts (1970 & 1980).
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Key Provisions of the Act
- The provisions of the Act address legacy gaps through a comprehensive legal overhaul aimed at enhancing governance, audit quality, and depositor protection in Public Sector Banks (PSBs).
- Governance Safeguard: Raises ‘substantial interest’ threshold from ₹5 lakh to ₹2 crore, updating the 1968 limit to reduce insider control risks in banks.
- Tenure Reform: Extends the tenure of cooperative bank directors (excluding the chairperson and whole-time director) from 8 to 10 years, aligning with the 97th Constitutional Amendment.
- Investor Safeguard: Enables PSBs to transfer unclaimed shares and proceeds to the Investor Education and Protection Fund (IEPF), enhancing fund transparency.
- The ‘substantial interest’ threshold is the minimum financial stake a person must hold in a bank to be considered as having significant influence over its affairs.
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- The IEPF, established under the Companies Act, 2013, is a government-managed fund that safeguards unclaimed assets, promotes investor education, and enables rightful claims.
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- Audit Reform: Permits PSBs to determine auditor remuneration, improving audit quality and oversight.
{GS3 – DM – Issues} Kamchatka Earthquake & Tsunami
- Context (BBC): A magnitude 8.8 earthquake struck near Russia’s Kamchatka peninsula, triggering trans-Pacific tsunami warnings with limited damage.
About the Earthquake
- The 2025 Kamchatka earthquake was a high-magnitude rupture along a plate subduction boundary.
- Earthquake Type: It was a megathrust earthquake caused by one plate slipping beneath another.
- Subduction: Occurred off Kamchatka, where the Pacific Plate subducts beneath Okhotsk microplate.
- Epicentre: Epicentre lies ~130 km southeast of Petropavlovsk-Kamchatsky, in the North Pacific.
- Rupture: Fault rupture stretched ~450 km along the Kuril-Kamchatka trench segments.
- Fault Mechanism: The earthquake showed reverse faulting with vertical seafloor displacement.
- Slip Magnitude: The Pacific Plate moved ~10 metres during fault rupture off the Kamchatka coast.
- Hypocentre: Focus at ~21 km depth intensified vertical seabed displacement and tsunami risk.
- Slab Rigidity: Cold subducting slab enabled extreme elastic strain accumulation before rupture.
- Tsunami Alerts: Warnings were issued for Japan, Hawaii, the Philippines, and the Pacific Americas.
Tsunami After the Earthquake
- Megathrust earthquakes generate tsunamis by vertically displacing the overlying water column.
- Primary Trigger: Sudden vertical fault slip forces seawater upward, initiating tsunami formation.
- Prevalence: Over 80% of global tsunamis originate from megathrust subduction earthquakes.
- Rapid Onset: Vertical energy transfer during rupture causes tsunami waves within seconds.
- Rupture Magnitude: Longer fault ruptures displace larger volumes, increasing tsunami wave height.
Conditions for Tsunami Formation
- Tsunamis require specific earthquake properties related to magnitude, depth, and fault motion.
- Magnitude Threshold: Earthquake must exceed magnitude 6.5 to displace sufficient ocean water.
- Shallow Focus: Rupture depth must lie within ~70 km to disturb the seafloor.
- Vertical Uplift: Rapid upward movement of the seabed is essential to generate wave energy.
- Rupture Extent: Fault must rupture over a wide area to displace sufficient water.
- Plate Rigidity: The subducting slab must be rigid enough to store and release vertical strain.
Why the Kamchatka Tsunami Was Not Severe?
- Several geophysical factors limited the tsunami’s height and trans-oceanic impact.
- Shelf Gradient: A broad, shallow continental slope reduced tsunami wave amplification nearshore.
- Trench Geometry: The narrow subduction trench limited vertical uplift and tsunami spread.
- Segmented Rupture: Multi-segment rupture scattered energy, limiting vertical water displacement.
- Offshore Slip: Maximum displacement occurred far offshore, reducing wave buildup near land.
- No Submarine Landslide: Absence of underwater landslide averted tsunami wave amplification.
About Kamchatka
- Location: Kamchatka is situated in the Russian Far East, between Okhotsk Sea and Pacific Ocean.
- Tectonic Setting: It lies on a convergent plate margin within the Pacific Ring of Fire.
- Volcanism: Kamchatka hosts ~150 volcanoes, including Klyuchevskoy, Eurasia’s tallest active volcano.
- Mountains: It is flanked by the Sredinny and Vostochny Mountain ranges along its length.
- Geothermal Activity: Kamchatka contains one of the world’s most active geothermal zones.
- Climate & Flora: Sub-Arctic tundra supports mosses, lichens, and Kamchatka alder.
- Tribes: It is home to the Koryak, Chukchi, and Kamchadal tribal populations.
- UNESCO WHS: The Volcanoes of Kamchatka are listed as a UNESCO World Heritage Site.
- Geopolitical: The Kuril Archipelago forms a disputed boundary between Russia and Japan.

Credit: PBS
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{GS3 – S&T – BioTech} CRIB Rare Blood Group Found in India
- Context (TH): A new human blood group antigen named CRIB was discovered in Bengaluru and officially recognised by the International Blood Group Reference Laboratory (IBGRL), UK.
- A blood group antigen is a protein or sugar on red blood cells that triggers immune responses and helps determine blood type compatibility during transfusions.
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About CRIB Discovery
- CRIB is a recently identified human blood group antigen within the Cromer (CR) blood group system.
- Name Significance: ‘CRIB’ combines Cromer (CR) and India–Bengaluru (IB) to indicate its origin.
- Diagnostic Trigger: The antigen was identified following panreactivity, indicating the presence of an unknown antigen.
- Nomenclature Authority: It was officially designated by the International Society of Blood Transfusion (ISBT), the global authority for naming and classifying rare blood group antigens.
- The Cromer system is a rare blood group classification with antigens located on the Decay-Accelerating Factor (DAF) protein.
- DAF is a glycoprotein on various cell surfaces, including RBCs, that protects them from immune attacks.
- Panreactivity occurs when a blood sample reacts with all tested donor samples, indicating the presence of possible unidentified antibodies or rare antigens.
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Significance of CRIB Discovery
- It improves the Cromer group database and supports the advancement of global research.
- The discovery highlights India’s increasing expertise in molecular blood grouping research.
- It emphasises the need for rare donor registries and international coordination in blood typing.
{Prelims – In News} Piprahwa Relics
- Context (PIB): Piprahwa relics, associated with Lord Buddha’s mortal remains, returned to India.
Historical Background
- In 1898, British engineer William Claxton Peppé excavated a stupa at Piprahwa, Uttar Pradesh, believed to be one of the original eight built to enshrine Lord Buddha’s mortal remains.
- The excavation yielded a stone coffer containing ashes, bone fragments, and offerings such as gold ornaments, pearls, and gemstones.
- A Brahmi inscription on a casket confirmed the relics belonged to Lord Buddha, deposited by members of his Shakya clan.
Distribution and Dispersal of Relics
- Over 1,800 items were recovered during the excavation. In 1899, the Indian Museum in Kolkata received the largest share.
- Viceroy Lord Elgin gifted a portion of the bone relics to King Rama V of Siam (Thailand), and William Peppé kept a part, which was later listed for auction in 2025.
{Prelims – In News} SIMBEX-25
- Context (PIB): Recently, INS Satpura reached Singapore to participate in the 32nd edition of the Singapore-India Maritime Bilateral Exercise (SIMBEX-25).
About SIMBEX-25
- SIMBEX is a bilateral naval exercise between India and Singapore, held annually since 1994 (originally launched as Exercise Lion King).
- Longest uninterrupted naval exercise India has with any country.
- Aims to enhance interoperability and maritime security in the Indo-Pacific.
- Aligns with India’s ‘MAHASAGAR’ vision and Singapore’s strategic role in ASEAN.
- INS Satpura is a Shivalik-class stealth guided-missile frigate, indigenously designed and built by Mazagon Dock Shipbuilders Ltd.
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{Prelims – In News} Launch of NISAR Satellite
- Polar Orbit: GSLV conducted its first satellite launch into sun-synchronous polar orbit (SSPO).
- Cryogenic Precision: The mission showcased the CE20 cryogenic stage’s accuracy for orbital injection.
- NASA Launch: ISRO commercially launched a fully NASA-owned satellite for the first time.
Significance of the Launch
- Revenue Gain: The commercial contract generated significant revenue for ISRO.
- Strategic Partnership: The joint mission deepens India-U.S. trust in complex space collaboration.
- Tech Sovereignty: Launch proved indigenous cryogenic strength for independent satellite launches.
- Global Reputation: The mission elevated India’s profile in precision foreign satellite launches.
Read More > NISAR Satellite.