III CLIMATE AND VEGETATION
III CLIMATE AND VEGETATION — Study Notes
NCERT-aligned · 10 notes · 3 shown free
Introduction
ExplanationIntroduction
Climate is the average weather conditions of a place over a long period, typically 30 years or more. It includes temperature, humidity, atmospheric pressure, wind, rainfall, and other meteorological elements. Vegetation refers to the plant life or plant communities in a particular region. The climate of a region greatly influences the type of vegetation found there. This chapter explores the various climatic regions of India and the corresponding vegetation types, highlighting the interdependence between climate and vegetation. India’s vast geographical expanse and diverse topography result in varied climatic conditions, which in turn support a wide range of vegetation types. Understanding the relationship between climate and vegetation is crucial for comprehending ecological patterns, agricultural practices, and environmental conservation in India.
- Climate is the long-term average of weather conditions.
- Vegetation refers to the plant life in a region.
- Climate influences the type and distribution of vegetation.
- India’s diverse climate leads to varied vegetation types.
- Studying climate and vegetation helps understand ecological and agricultural patterns.
- 📌 Climate: The average weather conditions of a place over a long period.
- 📌 Vegetation: The plant life or plant communities in a region.
Factors Influencing Climate
ExplanationFactors Influencing Climate
India’s climate is influenced by several factors that determine temperature, precipitation, and seasonal variations. These factors include latitude, altitude, pressure and wind system, distance from the sea, and relief features. Latitude affects the amount of solar radiation received; India lies mostly in the tropical zone, resulting in generally high temperatures. Altitude influences temperature as it decreases with increasing height; the Himalayan region experiences cold climate due to high altitude. Pressure and wind systems, such as the monsoon winds, bring seasonal rainfall and affect temperature. The distance from the sea moderates temperature; coastal areas have moderate temperatures while interior regions experience extremes. Relief features like mountains act as barriers to wind and rainfall, influencing local climate. For example, the Himalayas block cold Central Asian winds, protecting the Indian subcontinent from severe winters. These factors collectively shape the diverse climatic conditions across India.
- Latitude determines solar radiation and temperature.
- Altitude causes temperature to decrease with height.
- Pressure and wind systems influence rainfall and temperature.
- Distance from the sea affects temperature moderation.
- Relief features like mountains influence wind and rainfall patterns.
- 📌 Latitude: The angular distance north or south of the equator.
- 📌 Altitude: Height above sea level.
- 📌 Monsoon: Seasonal reversing wind accompanied by corresponding changes in precipitation.
Climatic Regions of India
ExplanationClimatic Regions of India
India’s climate can be broadly divided into six major climatic regions based on temperature and rainfall patterns: (1) Tropical Wet Climate, (2) Tropical Dry Climate, (3) Subtropical Humid Climate, (4) Mountain Climate, (5) Desert Climate, and (6) Th
Practice Questions — III CLIMATE AND VEGETATION
Includes NCERT exercise questions with answers
Q1.1. Multiple choice questions. (i) Who amongst the following was the first to consider the possibility of Europe, Africa and America having been located side by side. (a) Alfred Wegener (c) Abraham Ortelius (b) Antonio Pellegrini (d) Edmond Hess (ii) Polar fleeing force relates to: (a) Revolution of the Earth (c) Rotation of the earth (b) Gravitation (d) Tides (iii) Which one of the following is not a minor plate? (a) Nazca (c) Philippines (b) Arabia (d) Antarctica (iv) Which one of the following facts was not considered by those while discussing the concept of sea floor spreading? (a) Volcanic activity along the mid-oceanic ridges. (b) Stripes of normal and reverse magnetic field observed in rocks of ocean floor. (c) Distribution of fossils in different continents. (d) Age of rocks from the ocean floor. (v) Which one of the following is the type of plate boundary of the Indian plate along the Himalayan mountains? (a) Ocean-continent convergence (b) Divergent boundary (c) Transform boundary (d) Continent-continent convergence
Answer:
1.(i) (c) Abraham Ortelius was the first to consider the possibility of Europe, Africa and America having been located side by side. (ii) (a) Polar fleeing force relates to the Revolution of the Earth. (iii) (d) Antarctica is not a minor plate; it is a major tectonic plate. (iv) (c) Distribution of fossils in different continents was not considered while discussing the concept of sea floor spreading. (v) (d) The type of plate boundary of the Indian plate along the Himalayan mountains is Continent-continent convergence.
Explanation:
1.(i) Abraham Ortelius in the 16th century first suggested that continents might have been joined together. Alfred Wegener later developed the continental drift theory. (ii) Polar fleeing force is related to the centrifugal force due to Earth's revolution around the Sun. (iii) Antarctica is a major plate, unlike Nazca, Arabia, and Philippines which are minor plates. (iv) Sea floor spreading discussions focused on volcanic activity, magnetic stripes, and age of ocean floor rocks, but not on fossil distribution. (v) The Indian plate collides with the Eurasian plate forming the Himalayas, a continent-continent convergent boundary.
Q2.2. Answer the following questions in about 30 words. (i) What were the forces suggested by Wegener for the movement of the continents? (ii) How are the convectional currents in the mantle initiated and maintained? (iii) What is the major difference between the transform boundary and the convergent or divergent boundaries of plates? (iv) What was the location of the Indian landmass during the formation of the Deccan Traps?
Answer:
(i) Wegener suggested that the continents moved due to forces like the polar fleeing force and tidal force. (ii) Convectional currents in the mantle are initiated by heat from the Earth's core causing mantle material to rise and fall, maintaining the currents. (iii) Transform boundaries involve plates sliding past each other horizontally, unlike convergent or divergent boundaries where plates collide or move apart. (iv) During the formation of the Deccan Traps, the Indian landmass was located in the southern hemisphere near the equator, moving northwards.
Explanation:
(i) Wegener proposed forces such as polar fleeing force (centrifugal force due to Earth's rotation) and tidal force from the Moon and Sun to explain continental movement. (ii) Heat from the Earth's core causes mantle material to heat up, become less dense and rise; upon cooling, it sinks, creating convection currents. (iii) Transform boundaries are characterized by lateral sliding of plates, causing earthquakes but no creation or destruction of crust, unlike convergent (collision) or divergent (separation) boundaries. (iv) Geological evidence shows the Indian plate was in the southern hemisphere during the Deccan Traps volcanic activity about 65 million years ago.
Q3.3. Answer the following questions in about 150 words. (i) What are the evidences in support of the continental drift theory? (ii) Bring about the basic difference between the drift theory and Plate tectonics. (iii) What were the major post-drift discoveries that rejuvenated the interest of scientists in the study of distribution of oceans and continents?
Answer:
(i) Evidences supporting continental drift theory include the fit of the continents like South America and Africa, similarity of fossils across continents, matching geological formations, and paleoclimatic evidence such as glacial deposits in now tropical regions. (ii) The drift theory proposed by Wegener suggested continents moved but lacked a mechanism. Plate tectonics explains the movement of lithospheric plates driven by mantle convection, providing a mechanism for continental drift and sea-floor spreading. (iii) Major post-drift discoveries include the mapping of mid-ocean ridges, discovery of sea-floor spreading, paleomagnetic studies showing magnetic striping on ocean floors, and understanding of plate boundaries, which revived interest in continental and oceanic distribution.
Explanation:
(i) The matching coastlines, fossil records (like Mesosaurus), geological similarities, and evidence of past climates support the idea that continents were once joined. (ii) Drift theory lacked explanation for forces causing movement; plate tectonics introduced mantle convection and plate boundaries as mechanisms. (iii) Discoveries such as mid-ocean ridges, magnetic anomalies, and sea-floor spreading provided concrete evidence for plate movements and ocean basin evolution.
Q4.Project Work Prepare a collage related to damages caused by an earthquake.
Answer:
This is a creative project work requiring students to collect images, news clippings, and information about earthquake damages and prepare a collage showcasing the impact of earthquakes on life and property.
Explanation:
The project helps students understand the destructive nature of earthquakes and raises awareness about earthquake preparedness and safety measures.
Q5.What percentage of the Earth's surface is covered by continents, and what percentage is covered by oceanic waters?
Answer:
29% continents and 71% oceanic waters
Explanation:
Continents cover approximately 29% of the Earth's surface, while the remaining 71% is covered by oceanic waters. This distribution is a fundamental fact in physical geography and helps understand the Earth's surface composition.
Q6.Who first proposed the idea that the continents were once joined together, and in which year?
Answer:
Abraham Ortelius, 1596
Explanation:
Abraham Ortelius, a Dutch map maker, first proposed the possibility that continents were once joined together in 1596. Although Alfred Wegener later developed the comprehensive continental drift theory in 1912, Ortelius was the earliest to suggest this idea.
Q7.According to Alfred Wegener's continental drift theory, what was the name of the super continent and the surrounding mega ocean?
Answer:
Pangaea and Panthalassa
Explanation:
Wegener proposed that all continents were once joined as a single super continent called Pangaea, surrounded by a mega ocean named Panthalassa. This concept is central to the continental drift theory.
Q8.Which two large continental masses did Pangaea split into according to Wegener's theory?
Answer:
Laurasia and Gondwanaland
Explanation:
Pangaea first broke into two large continental masses: Laurasia in the north and Gondwanaland in the south. These subsequently fragmented into the continents we know today.
All 6 Chapters in India - Physical Environment
Geography · Class 11