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World Geography

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medium importance~1 Q in Tier 12 formulas⚡ 12 shortcuts6 subtopics
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Earth's interior, earthquakes, rocks and volcanoes

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⏱ 7 min read🧩 5 question types🎯 20 practice Q
The idea in one minute

Interior of the Earth

LayerNatureOld name
CrustThinnest; continental crust mostly silica + aluminiumSiAl
MantleSilica + magnesium; upper part includes the asthenosphere (magma source)SiMa
CoreNickel + iron; outer core liquid, inner core solidNiFe

Discontinuities: Conrad (within crust), Mohorovičić / Moho (crust–mantle), Gutenberg (mantle–core), Lehmann (outer–inner core).

Earthquakes

  • Point of origin inside the Earth = focus (hypocentre); point on the surface directly above = epicentre.
  • P-waves (primary) are fastest and travel through solids, liquids and gases. S-waves (secondary) cannot pass through liquids — their shadow zone proved the outer core is liquid. Surface (L) waves are slowest and most destructive.
  • Recorded by a seismograph; Richter scale measures magnitude (energy, logarithmic), Mercalli scale measures intensity (damage).

Rocks

TypeFormed byExamples
Igneous ('primary rocks')Cooling of magma/lavaGranite (intrusive), basalt (extrusive)
SedimentaryLayers of deposits; contain fossilsSandstone, shale, limestone, coal
MetamorphicHeat and pressure change existing rocksLimestone → marble, sandstone → quartzite, shale → slate, granite → gneiss

Volcanoes and plates

  • About two-thirds of active volcanoes lie on the Pacific 'Ring of Fire'.
  • Stromboli (Italy) is the 'Lighthouse of the Mediterranean'; Vesuvius buried Pompeii in AD 79; Krakatoa (Indonesia) erupted catastrophically in 1883; Mauna Loa (Hawaii) is the largest active volcano.
  • Fold mountains (Himalayas, Alps, Andes, Rockies) form at convergent plate boundaries; mid-ocean ridges form at divergent boundaries; the San Andreas Fault is a transform boundary.
  • Continental drift was proposed by Alfred Wegener (1912); the supercontinent was Pangaea, surrounded by the ocean Panthalassa.
01

Inside the Earth - three layers

Our knowledge of the interior comes from seismic waves and mining, not direct observation. The three layers:

LayerDepth (about)Key facts
Crust5-10 km (ocean floors) to 30-70 km (continents)Thinnest layer; continental crust = SiAl (silica + aluminium), lighter; oceanic = SiMa (silica + magnesium), denser
Mantleup to about 2,900 kmMostly solid rock; the partly-molten asthenosphere in its upper part is the source of magma
Core2,900 km to centre (6,371 km)NiFe - nickel and iron; outer core liquid, inner core solid

Discontinuities (surfaces where wave speeds jump) - remember the order top to bottom: Conrad (within the crust), Mohorovicic (Moho) - crust and mantle (1909), Repetti (within the mantle), Gutenberg - mantle and outer core (about 2,900 km), Lehmann - outer and inner core.

02

Earthquakes

An earthquake is a sudden shake caused by the release of stored energy along faults. The point inside the Earth where it starts is the focus (hypocentre); the point on the surface directly above is the epicentre (shock strongest there). Waves are recorded by a seismograph.

  • P-waves (primary) - fastest, longitudinal, pass through solids and liquids.
  • S-waves (secondary) - slower, transverse, cannot pass through liquids - this proves the outer core is liquid.
  • L-waves (surface) - slowest, arrive last, do the most damage. Magnitude is measured on the Richter scale; damage (intensity) on the Mercalli scale. About 80% of the world's earthquakes occur in the Circum-Pacific belt - the 'Ring of Fire'. Giant sea waves set off by undersea earthquakes are tsunamis (a Japanese word meaning 'harbour wave'), as in the Indian Ocean tsunami of 2004.
03

Volcanoes

A volcano is an opening where magma (molten rock), ash and gases escape.

  • By activity: active (Barren Island - India's only active volcano; Stromboli, the 'Lighthouse of the Mediterranean'; Etna; Vesuvius, which buried Pompeii in 79 AD), dormant (sleeping, e.g. Fuji) and extinct (no record of eruption).
  • By shape: shield volcanoes (broad, runny lava - Mauna Loa, Hawaii), composite (strato) volcanoes (steep, alternating lava and ash - Fuji, Vesuvius), and calderas (collapsed craters).
  • Hot springs and geysers (e.g. Old Faithful of Yellowstone, USA) are related features. Volcanoes also cluster in the Ring of Fire and along mid-ocean ridges.
04

Rocks - three families

FamilyFormed byExamples
IgneousCooling of magma/lava ('fire rocks'; the oldest, primary rocks)Granite (intrusive/plutonic, big crystals), basalt (extrusive/volcanic; ocean floors)
SedimentaryLayers (strata) of sediments pressed together; the only rocks with fossils; cover most of the land surfaceSandstone, shale, limestone, coal
MetamorphicHeat + pressure change an existing rockLimestone to marble, sandstone to quartzite, shale to slate, granite to gneiss

The endless conversion of one rock type into another is the rock cycle. Igneous and metamorphic rocks hold most minerals (gold, copper); coal, oil and limestone - the economic favourites - sit in sedimentary rocks.

05

Mountains, plateaus and plains - the big division

  • Fold mountains - crust squeezed into folds by plate collision; the young fold mountains (Himalayas, Alps, Andes, Rockies) are the highest; older folds (Aravallis, Urals) are worn down.
  • Block mountains - land raised between two faults (Vosges, Black Forest, Sierra Nevada); rift valleys (Rhine, East Africa) are the sunken blocks between faults.
  • Volcanic mountains - built by eruptions (Fuji, Kilimanjaro).
  • Plateaus - raised flatlands (Tibet, the highest and largest; Deccan); plains - low, flat, fertile, the most densely populated landforms.
06

Question types you will see

Each type: how to recognise it, the method step by step, and one question to try.

Type 1very common3 practice Q

Layers of the Earth and discontinuities

How to spot it:

'The boundary between crust and mantle is', 'which layer is made of nickel and iron', 'SiAl/SiMa/NiFe', ordering of Conrad-Moho-Repetti-Gutenberg-Lehmann.

Method
  1. Layers: crust (SiAl/SiMa) - mantle - core (NiFe); outer core liquid, inner core solid.

  2. Discontinuities top to bottom: Conrad (in crust), Moho (crust-mantle), Repetti (in mantle), Gutenberg (mantle-outer core), Lehmann (outer-inner core) - 'Come Make Good Lunch'.

  3. Continental crust is lighter and thicker; oceanic crust is denser basalt.

Try this

The Gutenberg discontinuity separates which two layers of the Earth?

Show solution

The mantle from the outer core (about 2,900 km deep). Moho separates crust from mantle; Lehmann divides the two cores.

Type 2very common4 practice Q

Seismic waves and earthquake vocabulary

How to spot it:

'Which wave cannot pass through liquid', focus vs epicentre, Richter vs Mercalli, seismograph, 'Ring of Fire'.

Method
  1. Waves: P fastest (passes all matter), S stops in liquids (proves the outer core is molten), L surface waves - slowest, most destructive.

  2. Focus = origin inside; epicentre = surface point above it; waves recorded on a seismograph.

  3. Magnitude = Richter scale; damage intensity = Mercalli scale. About 80% of earthquakes strike the Circum-Pacific 'Ring of Fire'.

Try this

The point inside the Earth where an earthquake originates is called the:

Show solution

Focus (hypocentre). The point on the surface directly above it - where the shock is felt first and strongest - is the epicentre.

Type 3very common4 practice Q

Rock families and metamorphic pairs

How to spot it:

'Marble is formed from', 'fossils are found in which rock', 'which is an igneous rock', classify a list of rocks.

Method
  1. Three families: igneous (cooled magma - granite, basalt), sedimentary (strata, the only rocks with fossils - limestone, sandstone, shale, coal), metamorphic (changed by heat-pressure).

  2. Metamorphic pairs: limestone-marble, sandstone-quartzite, shale-slate, granite-gneiss.

  3. Igneous rocks are the oldest 'primary' rocks; sedimentary rocks cover most of the land surface and hold coal and oil.

Try this

Slate, used for roofing, is a metamorphic rock formed from which parent rock?

Show solution

Shale. The other classic pairs: limestone-marble, sandstone-quartzite, granite-gneiss.

Type 4common3 practice Q

Volcanoes: activity, shape and famous names

How to spot it:

'India's only active volcano', 'Lighthouse of the Mediterranean', shield vs composite volcano, Krakatoa/Vesuvius events.

Method
  1. Activity: active (Barren Island - India's only one; Stromboli; Etna; Vesuvius), dormant (Fuji), extinct.

  2. Shape: shield (broad, fluid lava - Mauna Loa, Hawaii), composite/strato (steep, alternating layers - Fuji, Vesuvius), caldera (collapsed crater).

  3. Volcanoes cluster in the Ring of Fire and along mid-ocean ridges; Krakatoa (Indonesia, 1883) is the classic explosive eruption.

Try this

Stromboli, often called the 'Lighthouse of the Mediterranean', is a/an:

Show solution

Active volcano (in the Aeolian islands, Italy) - its regular night glow guided sailors for centuries.

Type 5common3 practice Q

Mountain and landform types

How to spot it:

'Young fold mountains are', 'rift valley is formed by', block mountains with faults, highest/largest plateaus.

Method
  1. Fold mountains - squeezed crust; young folds (Himalaya, Alps, Andes, Rockies) are the highest, old folds (Aravallis, Urals) are worn down.

  2. Block mountains - raised fault blocks (Vosges, Black Forest); rift valleys - sunken blocks between faults (Rhine valley, East African rift).

  3. Plateau = raised flatland (Tibet highest and largest); plain = low, flat, fertile, most populated.

Try this

The Rhine valley and the East African rifts are examples of:

Show solution

Rift valleys - long, narrow sunken blocks (graben) formed where land has dropped between parallel faults.

07

Shortcuts that save time

⚡ Discontinuity order: 'Come Make Good Lunch'

Conrad (inside crust) → Moho (crust|mantle) → Gutenberg (mantle|core) → Lehmann (outer|inner core).

Example

Which discontinuity separates the crust from the mantle?

Show solution

The Mohorovičić (Moho) discontinuity.

⚡ Metamorphic pairs: 'Lime-Marble, Sand-Quartz, Shale-Slate, Granite-Gneiss'

The first letters of the new rock are easy: Marble from Limestone is the most asked (Taj Mahal marble).

08

Mistakes to avoid

Where most students lose marks on this subtopic.

Mistake 01

Saying S-waves travel through the outer core — they cannot pass through liquids.

Mistake 02

Mixing Richter (magnitude) with Mercalli (intensity).

Mistake 03

Calling granite a sedimentary rock — it is an intrusive igneous rock.

09

Quick revision

Read this the night before the exam.

  • Layers: crust (SiAl/SiMa) - mantle - core (NiFe); outer core liquid, inner solid.

  • Discontinuity order 'Come Make Good Lunch': Conrad, Moho, Repetti, Gutenberg, Lehmann.

  • S-waves stop at liquid - proof the outer core is molten; Richter = magnitude, Mercalli = intensity.

  • 80% of earthquakes and volcanoes: Pacific Ring of Fire; Barren Island = India's only active volcano.

  • Igneous (granite, basalt), sedimentary (fossils: limestone, coal), metamorphic (marble, slate, quartzite, gneiss).

  • Young fold mountains: Himalaya, Alps, Andes, Rockies; Tibet = highest plateau.

10

Practice: 20 questions

Sets of 10, mixed across the question types above. Every answer has a step-by-step explanation.

Topic test · 10 questions

Suggested time 4 min · wrong answers go to your mistake notebook automatically.