NCERT Class 11 Geography Fundamental of Physical Geography: Chapter 4 — C H A P T E R

NCERT CBSE Class 11 Geography Fundamental of Physical Geography Chapter 4 English PDF

This chapter from NCERT's Fundamental of Physical Geography, Class 11, delves into the distribution of oceans and continents. It introduces Alfred Wegener's Continental Drift Theory, proposed in 1912, which suggested that continents were once joined as a supercontinent called Pangaea, surrounded by the mega-ocean Panthalassa. The chapter explores the evidence supporting this theory, including the matching coastlines of continents (Jig-Saw-Fit), the presence of rocks of the same age across oceans, tillite deposits indicating ancient glaciation in different Southern Hemisphere landmasses, and the distribution of fossils like Lemurs and Mesosaurus. It also discusses the forces Wegener proposed for drifting (pole-fleeing and tidal forces) and later theories like Arthur Holmes' Convectional Current Theory. The chapter highlights how post-WWII ocean floor mapping provided new insights into this geological phenomenon, crucial for understanding Earth's dynamic surface.

Quick info

BoardCBSE / NCERT
ClassClass 11
SubjectGeography
BookFundamental of Physical Geography
ChapterChapter 4 — C H A P T E R
LanguageEnglish
PDF typeNCERT Textbook
SessionCBSE 2026
Reading time6 minutes
Word count1119

Learning outcomes

Vocabulary

WordMeaning
PangaeaThe supercontinent that existed during the late Paleozoic and early Mesozoic eras, comprising all the landmasses of the Earth.
PanthalassaThe vast global ocean that surrounded Pangaea.
Continental DriftThe theory that Earth's continents have moved over geologic time relative to each other, thus appearing to have 'drifted' across the ocean bed.
LaurasiaThe northern component of Pangaea, which later split into North America, Europe, and Asia.
GondwanalandThe southern component of Pangaea, which later split into South America, Africa, Antarctica, Australia, and India.
TilliteA sedimentary rock formed from glacial deposits.
Radiometric datingA method of determining the age of rocks and minerals by measuring the rate of decay of radioactive isotopes.
Placer depositsDeposits of valuable minerals, such as gold or platinum, found in stream beds or other alluvial deposits.
Convection currentsCirculation of material in the Earth's mantle caused by differences in temperature and density.
FossilsThe preserved remains or traces of ancient organisms.

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Practice questions

  1. Who proposed the Continental Drift Theory and in which year? Answer: Alfred Wegener proposed the Continental Drift Theory in 1912.
  2. What were the names of the supercontinent and the mega-ocean proposed by Wegener? Answer: The supercontinent was named Pangaea, and the mega-ocean was called Panthalassa.
  3. Name two pieces of evidence that support the Continental Drift Theory. Answer: Two pieces of evidence are the matching of continents (Jig-Saw-Fit) and rocks of the same age across oceans.
  4. What is tillite and what does it indicate? Answer: Tillite is a sedimentary rock formed from glacial deposits, indicating extensive and prolonged glaciation.
  5. What forces did Wegener suggest were responsible for continental drift? Answer: Wegener suggested the pole-fleeing force and tidal force.

Practice MCQs

Q1. According to Wegener, the supercontinent was named:

Q2. The mega-ocean surrounding Pangaea was called:

Q3. Which of the following is NOT considered evidence for continental drift?

Q4. Tillite deposits are evidence of:

Q5. The radiometric dating of rocks from Brazil's coast matched with those from:

Q6. Arthur Holmes proposed which theory to explain the forces behind continental movement?

Frequently asked questions

What is the main idea of the Continental Drift Theory?

The Continental Drift Theory, proposed by Alfred Wegener, suggests that Earth's continents were once joined together in a single supercontinent called Pangaea and have since drifted apart to their current positions.

What evidence did Wegener use to support his theory?

Wegener used evidence such as the matching shapes of continental coastlines (Jig-Saw-Fit), similar rock formations and ages across oceans, distribution of fossils, and tillite deposits indicating ancient glaciation.

What were the proposed forces for continental drift?

Wegener suggested that the rotation of the Earth (pole-fleeing force) and the gravitational pull of the moon and sun (tidal force) were responsible for continental drift.

What is Pangaea and Panthalassa?

Pangaea was the name given to the supercontinent, and Panthalassa was the name of the vast ocean that surrounded it.

How did post-World War II research contribute to understanding continental distribution?

Detailed mapping of the ocean floor after WWII revealed its complex relief and provided new data that supported and expanded upon the ideas of continental movement and plate tectonics.

What is tillite and why is it significant?

Tillite is a sedimentary rock formed from glacial deposits. Its presence in continents now in tropical or temperate zones (like India, Africa, South America) provides strong evidence for past glaciation and continental drift.

Related resources

Important topics

Continental Drift Theory by Alfred Wegener Evidence supporting Continental Drift (Jig-Saw-Fit, Rocks, Fossils, Tillite) Pangaea and Panthalassa Convectional Current Theory Post-drift studies and Ocean Floor Mapping

Topics covered

Continental Drift Theory Alfred Wegener Pangaea Panthalassa Laurasia Gondwanaland Evidence for Continental Drift Jig-Saw-Fit Rocks of Same Age Across Oceans Tillite Placer Deposits Distribution of Fossils Convectional Current Theory Ocean Floor Mapping

NCERT Class 11 Geography — Fundamental of Physical Geography — Chapter 4 — C H A P T E R. Verified by NCERT Help Editorial Team. Reviewed on 29 Jul 2026. Last updated 10 Aug 2026.