UPSC Static Quiz – Geography : 18 June 2026 We will post 5 questions daily on static topics mentioned in the UPSC civil services preliminary examination syllabus. Each week will focus on a specific topic from the syllabus, such as History of India and Indian National Movement, Indian and World Geography, and more. We are excited to bring you our daily UPSC Static Quiz, designed to help you prepare for the UPSC Civil Services Preliminary Examination. Each day, we will post 5 questions on static topics mentioned in the UPSC syllabus. This week, we are focusing on Indian and World Geography.
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Question 1 of 5
1. Question
Consider the following statements:
Statement I: The Earth’s primordial atmosphere, composed mainly of hydrogen and helium, was lost during the early stages of its evolution.
Statement II: Intense solar winds emanating from the young Sun stripped away the lighter, early atmospheres of the terrestrial planets.
Which one of the following is correct in respect of the above statements?
Correct
Solution: A
- During the early developmental phase of the Solar System, the planets formed through the accretion of gas and dust around the young proto-Sun. The primordial atmospheres of the terrestrial planets, including Earth, were dominated by lighter gases like hydrogen and helium.
- However, the young Sun was highly active and emitted intense solar winds—streams of charged particles flowing outward into space. These high-energy solar winds stripped the light gases from the relatively weak gravitational grasp of the inner terrestrial planets. This process left them temporarily bare until volcanic degassing and later volatile accretion from comets created a denser, carbon-dioxide and water-vapour rich secondary atmosphere.
- Thus, Statement-I describes a correct geomorphological and astronomical fact, and Statement-II provides the correct physical mechanism for this loss.
Incorrect
Solution: A
- During the early developmental phase of the Solar System, the planets formed through the accretion of gas and dust around the young proto-Sun. The primordial atmospheres of the terrestrial planets, including Earth, were dominated by lighter gases like hydrogen and helium.
- However, the young Sun was highly active and emitted intense solar winds—streams of charged particles flowing outward into space. These high-energy solar winds stripped the light gases from the relatively weak gravitational grasp of the inner terrestrial planets. This process left them temporarily bare until volcanic degassing and later volatile accretion from comets created a denser, carbon-dioxide and water-vapour rich secondary atmosphere.
- Thus, Statement-I describes a correct geomorphological and astronomical fact, and Statement-II provides the correct physical mechanism for this loss.
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Question 2 of 5
2. Question
Consider the following statements:
- The Phanerozoic Eon is divided into the Paleozoic, Mesozoic, and Cenozoic Eras, representing the era of visible life.
- The Great Oxidation Event occurred during the Archean Eon, leading directly to the formation of the ozone layer.
- The Holocene Epoch represents the current warm interglacial period of the Quaternary.
Which one of the following conclusions based on the above statements is correct?
Correct
Solution: C
- Statement 1 is correct: The Phanerozoic Eon is the current geological eon characterized by abundant, complex animal and plant life. It is divided into three major eras: the Paleozoic, the Mesozoic (the age of reptiles), and the Cenozoic (the age of mammals).
- Statement 2 is incorrect: The Great Oxidation Event did not occur during the Archean Eon. It occurred during the Paleoproterozoic Era of the Proterozoic Eon (around 2.4 to 2.0 billion years ago) when cyanobacterial photosynthesis produced enough oxygen to accumulate in the atmosphere and form the protective ozone layer.
- Statement 3 is correct: The Holocene Epoch is the latest subdivision of the Quaternary Period. It represents the warm interglacial stage that followed the retreat of the Pleistocene ice sheets, accommodating the rise of human civilization.
Thus, statements 1 and 3 are correct, which includes statement 3.
Incorrect
Solution: C
- Statement 1 is correct: The Phanerozoic Eon is the current geological eon characterized by abundant, complex animal and plant life. It is divided into three major eras: the Paleozoic, the Mesozoic (the age of reptiles), and the Cenozoic (the age of mammals).
- Statement 2 is incorrect: The Great Oxidation Event did not occur during the Archean Eon. It occurred during the Paleoproterozoic Era of the Proterozoic Eon (around 2.4 to 2.0 billion years ago) when cyanobacterial photosynthesis produced enough oxygen to accumulate in the atmosphere and form the protective ozone layer.
- Statement 3 is correct: The Holocene Epoch is the latest subdivision of the Quaternary Period. It represents the warm interglacial stage that followed the retreat of the Pleistocene ice sheets, accommodating the rise of human civilization.
Thus, statements 1 and 3 are correct, which includes statement 3.
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Question 3 of 5
3. Question
Through which of the following combinations of water bodies does the equator pass?
Correct
Solution: B
The equator is the primary parallel of latitude dividing the Earth into the Northern and Southern Hemispheres. It crosses several key water bodies across South America, Africa, and Asia. Among these, it passes directly through the Gulf of Guinea (Atlantic Ocean), Lake Victoria in East Africa, and the Pacific Ocean. However, the equator does not pass through Lake Tanganyika (which lies further south in the East African Rift), Lake Tonlé Sap in Cambodia, or Patos Lagoon in southern Brazil.
Incorrect
Solution: B
The equator is the primary parallel of latitude dividing the Earth into the Northern and Southern Hemispheres. It crosses several key water bodies across South America, Africa, and Asia. Among these, it passes directly through the Gulf of Guinea (Atlantic Ocean), Lake Victoria in East Africa, and the Pacific Ocean. However, the equator does not pass through Lake Tanganyika (which lies further south in the East African Rift), Lake Tonlé Sap in Cambodia, or Patos Lagoon in southern Brazil.
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Question 4 of 5
4. Question
Consider the following crops:
- Soya bean
- Sorghum
- Sugarcane
- Wheat
In the context of intensive subsistence agriculture in monsoon Asia, which of the above crops are predominantly grown in regions where paddy cultivation is not feasible due to differences in relief, soil, or rainfall?
Correct
Solution: D
- Wet paddy (rice) cultivation requires hot, humid conditions, significant rainfall (over 100 cm), and flat, low-lying fields that can be flooded. In many parts of monsoon Asia, such as the interior parts of the Indo-Gangetic plain, Deccan Plateau, and northern China, either the rainfall is lower, the soil is different, or the terrain is not suitable for flooding.
- In these areas, farmers still practice intensive subsistence agriculture (high labour input on small plots) but cultivate other crops.
- Wheat (4) is the dominant crop in the drier parts of the Indo-Gangetic plains (e.g., Punjab, Haryana, Western UP) and North China Plain.
- Soya bean (1) and Sorghum (2) (Jowar) are important crops in the drier parts of China and India (e.g., Deccan plateau). They are more drought-resistant than rice.
- Sugarcane (3) is also grown intensively in these regions, for example, in Uttar Pradesh in India, where it is a major cash crop within the subsistence framework.
All four crops are characteristic of the “other than paddy” variant of intensive subsistence agriculture, grown where conditions are not ideal for rice.
Incorrect
Solution: D
- Wet paddy (rice) cultivation requires hot, humid conditions, significant rainfall (over 100 cm), and flat, low-lying fields that can be flooded. In many parts of monsoon Asia, such as the interior parts of the Indo-Gangetic plain, Deccan Plateau, and northern China, either the rainfall is lower, the soil is different, or the terrain is not suitable for flooding.
- In these areas, farmers still practice intensive subsistence agriculture (high labour input on small plots) but cultivate other crops.
- Wheat (4) is the dominant crop in the drier parts of the Indo-Gangetic plains (e.g., Punjab, Haryana, Western UP) and North China Plain.
- Soya bean (1) and Sorghum (2) (Jowar) are important crops in the drier parts of China and India (e.g., Deccan plateau). They are more drought-resistant than rice.
- Sugarcane (3) is also grown intensively in these regions, for example, in Uttar Pradesh in India, where it is a major cash crop within the subsistence framework.
All four crops are characteristic of the “other than paddy” variant of intensive subsistence agriculture, grown where conditions are not ideal for rice.
-
Question 5 of 5
5. Question
With reference to the salinity of enclosed or semi-enclosed seas, consider the following statements:
- The Red Sea exhibits one of the highest salinities in the world due to high evaporation and negligible freshwater input from rivers.
- The Baltic Sea has extremely low salinity because it receives significant freshwater runoff from numerous rivers and has limited connection to the open ocean.
- The salinity of the Black Sea is significantly lower at the surface than in its deep waters due to a strong influx of river water, creating a permanent halocline.
How many of the above statements are correct?
Correct
Solution: C
- Statement 1 is correct. The Red Sea is a long, narrow body of water situated in a hot, arid region. It experiences extremely high rates of evaporation. Furthermore, it receives almost no significant freshwater input from precipitation or rivers. Its only connection to the open ocean is through the narrow Strait of Bab-el-Mandeb. This combination of factors leads to exceptionally high surface salinity, often reaching 41 ppt.
- Statement 2 is correct. The Baltic Sea, located in Northern Europe, is a classic example of a brackish water body. It is semi-enclosed with only a narrow and shallow connection to the North Sea (and thus the Atlantic). It is surrounded by a large land area from which numerous rivers (e.g., Oder, Vistula) discharge vast amounts of freshwater. Evaporation rates are low due to the high latitude. This massive freshwater input and limited mixing with saltier ocean water result in very low surface salinity, typically ranging from 3 to 8 ppt.
- Statement 3 is correct. The Black Sea is another semi-enclosed sea with a large drainage basin, receiving freshwater from major rivers like the Danube, Dnieper, and Don. This creates a low-salinity surface layer (around 18 ppt). However, it has a restricted connection to the much saltier Mediterranean Sea through the Bosporus Strait. The dense, saline Mediterranean water flows into the Black Sea and sinks to the bottom. This creates a strong, stable stratification with a permanent halocline (a layer of rapid salinity increase) that prevents vertical mixing. As a result, the deep waters of the Black Sea are anoxic (lacking oxygen).
Incorrect
Solution: C
- Statement 1 is correct. The Red Sea is a long, narrow body of water situated in a hot, arid region. It experiences extremely high rates of evaporation. Furthermore, it receives almost no significant freshwater input from precipitation or rivers. Its only connection to the open ocean is through the narrow Strait of Bab-el-Mandeb. This combination of factors leads to exceptionally high surface salinity, often reaching 41 ppt.
- Statement 2 is correct. The Baltic Sea, located in Northern Europe, is a classic example of a brackish water body. It is semi-enclosed with only a narrow and shallow connection to the North Sea (and thus the Atlantic). It is surrounded by a large land area from which numerous rivers (e.g., Oder, Vistula) discharge vast amounts of freshwater. Evaporation rates are low due to the high latitude. This massive freshwater input and limited mixing with saltier ocean water result in very low surface salinity, typically ranging from 3 to 8 ppt.
- Statement 3 is correct. The Black Sea is another semi-enclosed sea with a large drainage basin, receiving freshwater from major rivers like the Danube, Dnieper, and Don. This creates a low-salinity surface layer (around 18 ppt). However, it has a restricted connection to the much saltier Mediterranean Sea through the Bosporus Strait. The dense, saline Mediterranean water flows into the Black Sea and sinks to the bottom. This creates a strong, stable stratification with a permanent halocline (a layer of rapid salinity increase) that prevents vertical mixing. As a result, the deep waters of the Black Sea are anoxic (lacking oxygen).
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