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Subject: Geography

  • The lapses in the Disaster Management Bill

    Why in the News?

    The Disaster Management (Amendment) Bill, 2024, raises serious concerns. Instead of addressing the shortcomings of the Disaster Management Act (DMA), 2005, the Bill reduces opportunities for participation, accountability, and efficient governance.

    What are the lapses in the recent bill?

    • Top-Down Terminology: The Bill employs terms like “monitor” and “guidelines,” which suggest a top-down approach, rather than fostering community engagement through terms like “supervision” and “direction.”
      • This undermines trust between authorities and local communities, which are crucial in disaster response.
    • Neglect of Local Roles: While the Bill defines critical concepts such as ‘hazard’, ‘resilience’, and ‘vulnerability’, it fails to recognise the essential roles of local communities, panchayats, and NGOs in disaster management.
    • Lack of Intersectional Consideration: The Bill does not address intersectional discrimination affecting vulnerable groups like women, disabled individuals, lower castes, and LGBTQIA communities. Ignoring these factors limits the Bill’s inclusivity and effectiveness.
    • Absence of Accountability Mechanisms: The omission of performance evaluations for district authorities raises concerns about accountability. Without mechanisms to assess preparedness and response effectiveness, there is a risk of shifting blame onto individual philanthropic efforts during disasters.
    • Exclusion of Law and Order Issues: By stating that ‘man-made causes’ do not include law and order matters, the Bill complicates the role of police in disaster management while still involving them in executive committees.
    • Removal of Relief Standards: Key provisions regarding minimum standards of relief for disaster victims have been omitted from the Bill. This includes special provisions for vulnerable populations such as widows and orphans, which diminishes the support system for those affected by disasters.
    • Centralisation of Power: The Bill centralises decision-making by transferring responsibilities from local executive committees to national authorities, potentially leading to inefficiencies and delays in disaster response.
    • Neglect of Animal Welfare: The Bill does not address the impact of disasters on animals or include provisions for their welfare, which is a significant oversight given the scale of animal casualties during disasters.
    • Urban Disaster Management Authority (UDMA): The rationale behind establishing a separate UDMA is unclear, raising questions about its effectiveness given existing municipal structures that may not adequately address urban flooding issues caused by poor planning.

    What are the lessons learnt from a spectrum of areas?

    • Community Engagement: Successful disaster responses have historically relied on local knowledge and community action.
      • For example, in Cyclone Aila (2009, Sundarbans): Local villagers and fisherfolk initiated rescue operations well before official disaster response teams could arrive, saving countless lives.
    • Intersectionality Matters: Acknowledging diverse vulnerabilities ensures that disaster management strategies are comprehensive and equitable.
      • For example, Kerala Floods (2018): Specific interventions for women and children in relief camps improved health and hygiene outcomes, showcasing the value of targeted measures.
    • Accountability is Crucial: Clear accountability mechanisms are necessary to ensure that authorities fulfil their responsibilities effectively.
      • For example, in Uttarakhand Flash Floods (2013): Lack of timely action by district authorities and poor preparedness exacerbated the disaster’s impact, underscoring the need for performance evaluations.

    Can Regional collaboration work out?

    Regional collaboration could significantly enhance disaster management efforts, particularly in South Asia where cross-border challenges are prevalent:

    • Shared Resources and Knowledge: Collaborative frameworks among countries like SAARC, BIMSTEC, and BRICS could facilitate resource sharing and knowledge exchange during disasters.
    • Joint Preparedness Plans: Developing regional action plans based on shared vulnerabilities can strengthen collective responses to disasters.
    • Addressing Zoonotic Diseases: Given the increasing threat of zoonotic diseases, a coordinated regional approach could improve public health responses during disasters.

    What is the Sendai Framework for Disaster Risk Reduction?

    • The Sendai Framework for Disaster Risk Reduction (2015-2030) is a comprehensive international agreement aimed at reducing disaster risks and enhancing resilience globally.
    • It was adopted by UN member states during the Third UN World Conference on Disaster Risk Reduction held in Sendai, Japan, from March 14 to 18, 2015.
    • India is a signatory to the Sendai Framework for Disaster Risk Reduction (2015-2030).

    Way forward: 

    • Strengthen Community Participation and Inclusivity: Amend the Bill to explicitly involve local communities, panchayats, and NGOs in disaster management.
    • Promote Accountability and Regional Cooperation: Introduce performance evaluations for district authorities to ensure preparedness and effective disaster responses.

    Mains PYQ:

    Q Describe various measures taken in India for Disaster Risk Reduction (DRR) before and after signing ‘Sendai Framework for DRR (2015-2030)’. How is this framework different from ‘Hyogo Framework for Action, 2005’? (UPSC IAS/2018)

  • Ken-Betwa Link Project (KBLP) launched

    Ken-Betwa Link Project (KBLP) launched

    Why in the News?

    PM Modi laid the foundation stone of the Ken-Betwa River Linking National Project, the first project under the National Perspective Plan (NPP) for interlinking rivers, conceptualized in 1980. The project would submerge over 10 per cent of the core area of the Panna Tiger Reserve.

    About the Ken-Betwa Link Project (KBLP):

    About
    • Objective: Transfer water from the Ken River to the Betwa River, both tributaries of the Yamuna.
      • Ken-Betwa Canal: Envisages a 221 km canal (including a 2-km tunnel) for water diversion.
      • Submergence area: Jhansi, Banda, Lalitpur and Mahoba districts of UP and Tikamgarh, Panna and Chhatarpur districts of MP.
    • It’s the first interlinking project under the National Perspective Plan (1980).
    • Targeted completion within 8 years, as per the Ministry of Jal Shakti.
    Key Components
    • It will irrigate 10.62 lakh ha (8.11 lakh ha in MP and 2.51 lakh ha in UP) and provide drinking water to ~62 lakh people.
    • Power Generation: Aims for 103 MW of hydropower and 27 MW of solar power.

    Phases:

    1. Phase-I: Construction of Daudhan Dam, related tunnels, canal, and powerhouses.
    2. Phase-II: Building of Lower Orr Dam, Bina Complex Project, and Kotha Barrage.

    Daudhan Dam:

      • Foundation stone laid in December 2024 by PM Narendra Modi.
      • 2,031 m in length and 77 m in height, submerging ~9,000 ha across 10 villages.
    • Construction contract awarded to NCC Ltd.
    Geographical Features of Ken and Betwa River Ken River: Rises near Ahirgawan in Madhya Pradesh, flows through Bundelkhand, joins the Yamuna near Chilla village in UP.

    Betwa River: Originates in the Vindhya Range (near Hoshangabad, MP), also flows through Bundelkhand, and meets the Yamuna at Hamirpur (UP).

    • Both rivers traverse hilly and plateau regions of Bundelkhand, often facing drought-like conditions.
    • Both are highly seasonal; flows depend largely on monsoon rainfall.
    Significance
    • Water Scarcity Mitigation: Aims to alleviate drought-like conditions in Bundelkhand by ensuring year-round irrigation.
    • Enhanced Agriculture: 10.62 lakh ha of farmland to benefit, improving crop yields and farm income.
    • Drinking Water Supply: Targets ~62 lakh people in MP and UP, improving public health.
    • Energy Generation: A total of 130 MW (103 MW hydropower + 27 MW solar), boosting renewable energy capacity in rural areas.
    • Bundelkhand Development: Expected to spur socio-economic growth, reduce rural distress and migration, and aid industrial expansion.
    • Template for Future Projects: As the first interlinking project under the National Perspective Plan, its success could pave the way for additional river-linking schemes nationwide.

     

    PYQ:

    [2020] The interlinking of rivers can provide viable solutions to the multi-dimensional inter-related problems of droughts, floods, and interrupted navigation. Critically examine.

  • Assessment of Water Resources of India, 2024 by CWC

    Why in the News?

    • The Central Water Commission (CWC) recently released its study titled ‘Assessment of Water Resources of India, 2024.
      • It estimated India’s average annual water availability from 1985 to 2023 at 2,115.95 billion cubic meters (BCM).

    Key Highlights of CWC’s ‘Assessment of Water Resources of India 2024’ Report:

    • Total Water Availability: India’s average annual water availability between 1985 and 2023 is estimated at 2,115.95 billion cubic meters (BCM).
    • Top 3 Basins in (annual water availability):
      • Brahmaputra Basin: 592.32 BCM
      • Ganga Basin: 581.75 BCM
      • Godavari Basin: 129.17 BCM
    • Bottom 3 Basins in (annual water availability):
      • Sabarmati Basin: 9.87 BCM
      • Pennar Basin: 10.42 BCM
      • Mahi Basin: 13.03 BCM
    • Comparison to Previous Assessment (2019):
      • The current figure of 2,115.95 BCM is higher than the 1,999.2 BCM estimated in 2019.
      • The increase is due to the inclusion of Bhutan’s contribution to the Brahmaputra basin and Nepal’s contribution to the Ganga basin.
    • Per Capita Water Availability:
      • Based on the 2019 study: 1,486 cubic meters for the year 2021.
      • For 2024, with the new data, the per capita availability is projected to be 1,513 cubic meters (based on a population of 1.398 billion).
      • Despite the increase, India remains under water stress (less than 1,700 cubic meters per capita).
    • Utilizable Water Resources:
      • The CWC estimates utilizable surface water at 690 BCM out of the total 1,999.2 BCM.
      • Smaller basins have a higher proportion of utilisable water compared to larger ones like the Brahmaputra sub-basin.

    About the Central Water Commission (CWC):

    • CWC was established in 1945 as the Central Waterways, Irrigation and Navigation Commission (CWINC) on the advice of Dr. B. R. Ambedkar.
    • Operates under the Ministry of Jal Shakti, Department of Water Resources, River Development, and Ganga Rejuvenation.
    • A statutory advisory body for water resource development and management.
    • Headquarters: New Delhi.
    • Chairman serves as the Ex-Officio Secretary to the Government of India.
    • Responsibilities include:
      • Control, conservation, and utilization of water resources.
      • Maintaining the National Register of Large Dams (NRLD).
      • Conducting hydrological surveys.
      • Handles surface water, while the Central Groundwater Board (CGWB) manages groundwater resources.
    • Wings:
      • Designs and Research (D&R) Wing.
      • River Management (RM) Wing.
      • Water Planning and Projects (WP&P) Wing.

     

    PYQ:

    [2020] Consider the following statements:

    1. 36% of India’s districts are classified as “overexploited” or “critical” by the Central Ground Water Authority (CGWA).

    2. CGWA was formed under the Environment (Protection) Act.

    3. India has the largest area under groundwater irrigation in the world.

    Which of the statements given above is/are correct?

    (a) 1 only

    (b) 2 and 3 only

    (c) 2 only

    (d) 1 and 3 only

  • Cyclone Fengal

    Why in the News?

    • A depression over the Southwest Bay of Bengal has intensified into a deep depression and is likely to further intensify into Cyclone Fengal.
      • The system is currently close to an area with higher sea surface temperatures (SST), contributing to its potential intensification into a cyclonic storm.

    Origin of the Name ‘Fengal’

    • The name ‘Fengal’ was proposed by Saudi Arabia and is rooted in Arabic.
    • It reflects a combination of linguistic tradition and cultural identity.

    Cyclone Naming Process:

    • Cyclones in the North Indian Ocean are named by the World Meteorological Organization (WMO) and the United Nations Economic and Social Commission for Asia and the Pacific (UNESCAP) panel.
    • This panel includes 13 member countries, such as India, Bangladesh, Sri Lanka, and Pakistan, among others.
      • Each member country submits a list of potential cyclone names, and these names are used sequentially as cyclones form in the region.
      • This system, in place since 2004, ensures easy identification and effective communication of storms to the public.

     

    PYQ:

    [2015] In the South Atlantic and South Eastern Pacific regions in tropical latitudes, cyclone does not originate. What is the main reason behind this?

    (a) Sea Surface temperature are low

    (b) Inter Tropical Convergence Zone seldom occurs

    (c) Coriolis force is too weak

    (d) Absence of land in those regions

  • Salt Chimneys discovered in the Dead Sea

    Salt Chimneys discovered in the Dead Sea

    Why in the News?

    Researchers have identified unique salt chimneys on the Dead Sea floor.

    Key facts about the Dead Sea:

    Details
    Location • Located between Jordan and Israel, with the eastern shore in Jordan and the western shore in Israel.
    • The southern half of the western shore belongs to Israel, and the northern half is in the West Bank.• Divided by Al-Lisan peninsula into two basins: the northern basin is deep (400 m), and the southern basin is shallow (< 3 m).
    Geographical Features • 430.5 meters below sea level, the Earth’s lowest land-based feature.
    • Length: 50 km, Width: 15 km at its widest point.
    • Surrounded by the Judaea hills (west) and Transjordanian plateaus (east).
    Salinity and Density • Salinity: 34.2%, almost ten times saltier than ordinary seawater, making it the fourth saltiest water body in the world.
    • Density: 1.240 kg/L, which allows people to float easily.
    Inlets and Outlets • Main inlet: Jordan River.
    • No outlet, water loss occurs primarily through evaporation.
    • High salinity and harsh climate result in no life except for algae and microorganisms.

     

    About the Salt Chimneys 

    • Salt chimneys are tall, chimney-like structures made of crystallized salt, recently discovered on the Dead Sea floor.
    • They are found by researchers from the Helmholtz Centre for Environmental Research (UFZ) during an underwater survey.
    • These chimneys range from 1 to over 7m in height.
    • Formation Process:
      • Groundwater from surrounding aquifers flows through old salt deposits around the Dead Sea basin, dissolving halite (salt) and carrying it as brine.
      • Despite being saline, the brine is less dense than the Dead Sea water due to its high salinity, causing it to rise as a plume from the lake bed.
      • When this brine contacts the colder Dead Sea water, it rapidly crystallizes, forming chimney structures that can grow several centimeters in height each day.

    Potential Role in Sinkhole Forecasting

    • Thousands of sinkholes have appeared near the Dead Sea in recent decades; understanding chimney formation may aid in preventing future collapses in vulnerable areas.
    • Researchers have linked the formation of salt chimneys to underground cavities, which are often the precursors to sinkholes.
    • The location of these chimneys may help predict areas at high risk for sinkhole formation, offering a way to monitor and mitigate potential hazards.

  • Barak River

    Why in the News?

    Police found dead bodies floating in the Barak River (inflicted due to Manipur Violence).

    About the Barak River:

    Details
    Geographical Location • Originates from Japvo mountain in Manipur hills at 3,015 m altitude.
    • Flows south, forming the border between Assam and Manipur up to Jirimat.
    • Flows for 524 km in India, and then enters Bangladesh as Surma and Kushiyara, later becoming Meghna River.• The river is navigable in parts, with National Waterway 6 (121 km).
    Physical Features • Length: 564 km in total, with 524 km in India.
    • Drainage area in India: 41,157 sq. km (1.38% of India’s total area).
    • Tributaries: Jiri, Dhaleswari, Singla, Longai, Sonai, and Katakhal.
    Flora and Fauna/Important Sites • Fauna: Home to over 2,000 species of fish and rare creatures like the Siamese crocodile, susu dolphin, smooth-coated otter, and black mugger crocodile.
    • Flora: Includes Varzea forest, Los llamjao, tidal forests (mangroves), Pats (flat-topped table mountains), and large tropical swamps.
    • Wetlands support farming and biodiversity.
    • Hydropower projects: Tipaimukh Dam, Tista Champamati, Dhansiri Barrages.
    • Affected by flooding and soil erosion, especially during monsoon.

     

    PYQ:

    [2014] Consider the following rivers:

    1. Barak

    2. Lohit

    3. Subansiri

    Which of the above flows/flow through Arunachal Pradesh?

    (a) 1 only

    (b) 2 and 3 only

    (c) 1 and 3 only

    (d) 1, 2 and 3

  • What is DANA?

    Why in the News?

    The extreme conditions in eastern Spain which saw Valencia get a year’s worth of rain in just 8 hours can be blamed on an event locally known as Depresion Aislada en Niveles Altos (DANA).

    What is DANA?

    • Depresion Aislada en Niveles Altos (DANA), is commonly referred to as the “cold drop” in English.
    • It is a meteorological phenomenon in the western Mediterranean region that brings intense rainfall and flooding.
    • The term “DANA” was coined by Spanish meteorologists to specifically describe this weather phenomenon.

    Features and Location:

    • DANA occurs when cold air from the Polar Regions separates from the polar jet stream and descends over the warmer Mediterranean Sea.
    • The contrast between cold air aloft and warm, moist air near the surface causes atmospheric instability, leading to the rapid formation of cumulonimbus clouds and intense thunderstorms.
    • It primarily affects Spain and Portugal but can also impact Italy, France, and other areas around the Mediterranean Sea.
    • This occurs in autumn and spring, as temperature variations are more pronounced during these seasons.

    PYQ:

    [2014] The seasonal reversal of winds is the typical characteristic of:

    (a) Equatorial climate

    (b) Mediterranean climate

    (c) Monsoon climate

    (d) All of the above climates

  • TN declares Heatwaves a State-specific Disaster

    Why in the News?

    • The Tamil Nadu government has officially declared heatwaves a State-specific disaster.
      • It announced an ex-gratia payment of ₹4 lakh for families of individuals who die from heat-related causes, including those involved in relief operations.

    Key Details of the Declaration

    • Purpose: This declaration allows the government to provide immediate relief to those affected by extreme heat, especially during the severe temperatures of April and May 2024.
    • Funding: Relief efforts will be supported by the State Disaster Response Fund.
    • Other State-specific disasters in TN: Sea erosion, lightning, thunder, whirlwinds, and gale winds as State-specific disasters to ensure relief assistance for those impacted by these events.

    Note: 

    • Kerala in March this year, declared man-animal conflict as a state-specific disaster, becoming the first state in the country to do so.
    • Once an issue is declared a state-specific disaster, the onus to deal with it shifts to the state disaster management authority, which, powered by the Disaster Management Act, can take quicker and more decisive action.
    • Also, district collectors can directly intervene in their capacity as the chairman of the district disaster body.

     

    heatwave

    About Heatwaves:

    Details
    Definition A heatwave is a prolonged period of excessively hot weather, relative to the usual climate of a region.
    Occurrence Typically occurs in India between March and June.
    Declaration by IMD
    • Plains: The maximum temperature is at least 45°C
    • Hills: The maximum temperature is at least 30°C
    • Coastal regions: The maximum temperature is at least 37°C and the departure from normal is at least 4.5°C
    Formation • High-Pressure Systems: Develop when high pressure settles over a region for days or weeks.
    • Air Sinking: Forces air to sink, warming and drying it.
    • Increased Radiation: Fewer clouds lead to higher surface temperatures.
    • Surface Winds: Warm air from lower latitudes or continental winds intensify heat.
    Criteria for Declaring a Heatwave At least two stations in a meteorological subdivision must meet one of the following criteria for two consecutive days (declared on the second day):
    Based on Departure from Normal:
    – Heat Wave: Temperature departure of 4.5°C to 6.4°C above normal.
    – Severe Heat Wave: Temperature departure of >6.4°C above normal.
    Based on Actual Maximum Temperature (plains only):
    – Heat Wave: Maximum temperature reaches 45°C or higher.
    – Severe Heat Wave: Maximum temperature reaches 47°C or higher.
    Duration Typically lasts a minimum of four days but can extend to seven or ten days.
    Longest Recorded Spell: May 2015, lasting from 18 to 31 May.
    Impact of Heatwaves • Heat Strokes: Increased risk, especially for the elderly and those with chronic illnesses.
    • Increased Healthcare Costs: Higher hospital visits and death rates from related illnesses.
    • Reduced Productivity: Extreme heat affects the output of over 1 billion workers.
    • Risk of Wildfires: Heat domes can lead to wildfires.
    • Effect on Vegetation: Prolonged heat damages crops and leads to droughts.
    • Increased Energy Demands: Higher electricity usage for cooling, driving up rates.

     

    PYQ:

    [2013] Bring out the causes for the formation of heat islands in the urban habitat of the world.

    [2013] The annual range of temperature in the interior of the continents is high as compared to coastal areas. What is / are the reason / reasons?

    1. Thermal difference between land and water

    2. Variation in altitude between continents and oceans

    3. Presence of strong winds in the interior

    4. Heavy rains in the interior as compared to coasts

    Select the correct answer using the codes given below.

    (a) 1 only

    (b) 1 and 2 only

    (c) 2 and 3 only

    (d) 1, 2, 3 and 4

  • Cyclone Dana

    Why in the News?

    West Bengal and Odisha experienced heavy rainfall as Tropical Cyclone Dana is anticipated to make landfall later tonight.

    What are Cyclones?

    • Cyclones are wind systems rotating inwardly towards an area of low atmospheric pressure. They are categorised into Tropical (Temperature-induced) and Temperate (extra-tropical) cyclones (airmass-induced).
    • Formation Conditions: Tropical cyclones originate in warm regions, requiring conditions such as
    1. Warm sea surface (> 27°C),
    2. Coriolis Force,
    3. Pre-existing low-pressure systems,
    4. Small vertical wind speed differences, and
    5. Upper air divergence.

    Characteristics of Tropical Cyclones:

    • They form over warm water bodies due to energy derived from the condensation of warm water within cumulonimbus clouds.
    • Wind rotation is influenced by the Coriolis force, resulting in anti-clockwise rotation in the northern hemisphere and clockwise in the southern hemisphere.
    • By 30° latitude, the diminished warmth halts cyclone activity.

    What is the “Landfall” of a Cyclone?

    • Landfall occurs when a tropical cyclone moves from the sea onto the land.
    • As per the IMD, a cyclone makes landfall when the centre of the storm, or its eye, crosses the coast.
    • Landfall should not be confused with a “direct hit”, where the eyewall (area of high winds) hits land but the eye of the cyclone remains offshore.
    • According to the National Oceanic and Atmospheric Administration (NOAA), a cyclone’s strongest winds may still impact land even if the centre of the storm does not reach the coast.

    How long does a Cyclone Landfall last?

    • The duration of landfall typically lasts a few hours, depending on the wind speed and size of the storm.
    • For cyclone Dana, the landfall process is expected to last five to six hours with wind speeds around 125 km/h, impacting a wide region.
    • Cyclones usually weaken after landfall as they lose their moisture supply and experience increased surface friction.
    • While landfall is often the most destructive phase of a cyclone, it also signals the beginning of the cyclone’s dissipation.

    PYQ:

    [2015] In the South Atlantic and South Eastern Pacific regions in tropical latitudes, cyclone does not originate. What is the main reason behind this?

    (a) Sea Surface temperature are low

    (b) Inter Tropical Convergence Zone seldom occurs

    (c) Coriolis force is too weak

    (d) Absence of land in those regions

  • Baku and South Caucasus Region

    South Caucasus Region (Transcaucasia)

    Why in the News?

    • The 29th COP to the United Nations Framework Convention on Climate Change (UNFCCC) will begin on November 11, 2024, in Baku, the capital of Azerbaijan.
      • As global leaders gather near the Caspian Sea, the surrounding region of the South Caucasus faces significant climate challenges.

    Key Areas at Risk:

    (1) Regional/transboundary areas:

    • Northern Armenia and southern Georgia
    • North-west Azerbaijan and north-east Georgia (Alazani/Ganykh river basin)

    (2) Within countries:

    • Yerevan and Ararat Valley (Armenia)
    • Lake Sevan (Armenia)
    • Kura-Ara(k)s lowlands (Azerbaijan)
    • Baku and Absheron peninsula (Azerbaijan)
    • Adjara and the Black Sea coast (Georgia)
    • Tbilisi, Mtskheta-Mtianeti, and Kakheti regions (Georgia)

     

    About South Caucasus Region (Transcaucasia):

    Details
    Location South of the Greater Caucasus Mountains, bordered by Russia (north), Turkey and Iran (south), between the Black Sea (west) and Caspian Sea (east).
    Countries Armenia, Azerbaijan, and Georgia; includes disputed territories like Nagorno-Karabakh (Artsakh), Abkhazia, and South Ossetia.
    Mountains Lesser Caucasus Mountains (up to 3,000m); includes the Zangezur Range, Meskheti Range, and Armenian Highlands.
    Seas Between the Black Sea and Caspian Sea; Absheron Peninsula (Azerbaijan) extends into Caspian Sea, rich in oil.
    Rivers and Lakes Major rivers: Kura River (Georgia & Azerbaijan) and Aras River (Armenia & Azerbaijan). Key lake: Lake Sevan (Armenia).
    Climate
    • Continental climate: hot summers and cold winters;
    • Subtropical climate along Georgia’s Black Sea coast;
    • Semi-arid to desert climate near Caspian Sea, especially Azerbaijan.
    Natural Resources Rich in oil and natural gas, particularly in Azerbaijan; critical hub for energy pipelines like the Baku-Tbilisi-Ceyhan pipeline.
    Geopolitical Importance Strategic transit route for energy resources to Europe; region of geopolitical tensions due to conflicts (Nagorno-Karabakh, South Ossetia, Abkhazia).

     

    PYQ:

    [2014] Turkey is located between:

    (a) Black Sea and Caspian Sea

    (b) Black Sea and Mediterranean Sea

    (c) Gulf of Suez and Mediterranean Sea

    (d) Gulf of Aqaba and Dead Sea