Question map
Consider the following information : 1. Central Asia - Vosges - Fold mountain 2. Europe - Alps - Block mountain 3. North America - Appalachians - Fold mountain 4. South America - Andes - Fold mountain In how many of the above rows is the given information correctly matched ?
Explanation
The correct answer is option B – only two rows are correctly matched.
Let's analyze each row:
**Row 1 (Central Asia - Vosges - Fold mountain): INCORRECT**
The Vosges mountains are located in Europe, specifically along the Rhine Rift, not in Central Asia[2]. While they are associated with Hercynian mountain building, their location is wrongly stated.
**Row 2 (Europe - Alps - Block mountain): INCORRECT**
The Alps are located in Europe[3], but the Alps are young fold mountains formed due to the collision between African Plate and the Eurasian Plate[4], not block mountains.
**Row 3 (North America - Appalachians - Fold mountain): CORRECT**
The Appalachians are located in North America[5] and the Appalachians are very old fold mountains that were formed even before the breakup of Pangaea[6].
**Row 4 (South America - Andes - Fold mountain): CORRECT**
The Andes are in South America[7] and the Andes are examples of Alpine fold mountains[8].
Therefore, only rows 3 and 4 are correctly matched, making the answer **two**.
Sources- [2] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Hercynian Mountains > p. 132
- [3] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Alpine Mountain System > p. 132
- [4] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 8: Convergent Boundary > Formation of Alps, Urals, Appalachians and the Atlas Mountains > p. 123
- [5] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > 1) Very Old Fold Mountains > p. 135
- [6] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 8: Convergent Boundary > Formation of Alps, Urals, Appalachians and the Atlas Mountains > p. 123
- [7] Exploring Society:India and Beyond. Social Science-Class VI . NCERT(Revised ed 2025) > Chapter 3: Landforms and Life > THINK ABOUT IT > p. 45
- [8] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > 3) Alpine or Young Fold Mountains > p. 135
PROVENANCE & STUDY PATTERN
Guest previewThis is a textbook 'Sitter' from the static Physical Geography syllabus. It directly tests the standard examples found in NCERT Class XI and GC Leong (Chapter 2). The question relies on the classic 'Swap Trap'—switching the characteristics of well-known European ranges (Alps vs Vosges). No current affairs knowledge was required; pure static revision wins here.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Statement 1: Is the Vosges mountain range located in Central Asia?
- Statement 2: Are the Vosges mountain range classified as fold mountains?
- Statement 3: Is the Alps mountain range located in Europe?
- Statement 4: Are the Alps mountain range classified as block mountains?
- Statement 5: Is the Appalachian Mountains mountain range located in North America?
- Statement 6: Are the Appalachian Mountains mountain range classified as fold mountains?
- Statement 7: Is the Andes mountain range located in South America?
- Statement 8: Are the Andes mountain range classified as fold mountains?
- Directly names the Vosges and locates them as being 'along the Rhine Rift in Europe'.
- Placement in Europe contradicts the claim that the Vosges are in Central Asia.
Lists the Vosges explicitly among 'Inland Mountains' and associates it with 'Europe' alongside the Black Forest.
A student could use this example-listing rule to check continent membership of other named ranges (if Vosges is listed with European ranges, likely not in Central Asia).
Gives the Vosges as an example of Hercynian mountains that 'originated ... in Europe', linking Vosges to a European geologic group.
One could extend the geologic/tectonic grouping: if Vosges is categorized with European Hercynian mountains, it's unlikely to be a Central Asian range.
Provides a list of major mountains that define 'Central Asia' (Pamir, Tien Shan, Kun-Lun, Hindukush), showing which ranges are typically considered Central Asian.
Compare the named Central Asian ranges with the Vosges — absence of Vosges from this Central Asia list suggests it is not usually classified there.
Notes that most of the world's mountains are grouped by continent (e.g., Himalayas in Asia, Alps in Europe), implying continental classification is a common organizing principle.
Apply the continent-grouping principle: determine which continental group (Europe vs Asia) Vosges is normally grouped with to assess the statement.
Lists 'Block mountains (Vosges mountains in France, the Black Forest in Germany...)' showing an explicit classification of Vosges as block mountains in this typology.
A student could compare the block-mountain label here with other sources or maps showing Vosges structure to evaluate whether they fit block- vs fold-mountain criteria.
Groups 'Vosges and the Black Forest' under 'Hercynian Mountains', a named orogeny/time-period of mountain building.
Knowing Hercynian (Variscan) orogeny is often linked to folded mountain belts, a student could check whether Hercynian/Variscan ranges are typically fold mountains and whether Vosges formed in that style.
Defines 'old fold mountains' as those from Caledonian and Hercynian periods and gives the pattern that Hercynian-era ranges can be 'old fold mountains'.
Combine this with the fact that Vosges are listed as Hercynian (snippet 6) to infer Vosges might be considered old fold mountains — then verify with structural details or maps.
Lists general characteristics and environment of fold mountains (e.g., formed from folded sedimentary strata, often along continental margins, presence of fossils, seismicity).
A student could examine geological maps or rock types of the Vosges (sedimentary vs block-faulted basement) and their location relative to plate margins to see if they match fold-mountain traits.
Gives the formation mechanism of fold mountains (compressive folding of sedimentary strata in geosynclines), a rule to test against Vosges geology.
Use basic geologic facts or maps to check whether Vosges show folded sedimentary strata from a geosyncline or instead show block faulting, helping judge if Vosges are fold mountains.
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- Explicitly refers to the 'Alpine mountains of Europe' as examples of the alpine mountain system.
- Places the Alps among well-known continental mountain ranges, linking them to the European region.
- Identifies Mont Blanc as 'in Western Europe' and as the highest mountain of the Alps, directly tying the Alps to Europe.
- Uses a specific European landmark (Mont Blanc) to locate the range geographically.
- Describes the Alps as young fold mountains formed by collision involving the Eurasian Plate, linking their geology to the Eurasian (European) region.
- Connects the Alps' formation process to plate interactions that involve Europe's tectonic realm.
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Gives a clear definition of block (fault‑block) mountains formed by large‑scale faulting and lists typical examples (horsts and graben).
A student could compare the Alps' known origin or structure to this faulting pattern to see if they match.
Describes the specific block‑mountain mechanism (central block downfaults to form rift valley while surrounding blocks stand higher).
Use basic geologic maps or a plate‑tectonic summary of the Alps to check whether such rift/horst–graben geometry occurs there.
Explains horst/graben morphology and lists classic block‑mountain examples (Vosges, Black Forest) with characteristic flat/steep profiles.
Compare the Alps' topography and summit/scape profiles to these block‑mountain examples to judge similarity.
States that the Alps are young fold mountains formed by collision between the African and Eurasian plates (i.e., an orogenic/folding origin).
Combine this fold‑origin statement with the block‑mountain definitions to infer that the Alps are likely not block (fault‑block) mountains.
Lists the Alps explicitly among 'Alpine or Young Fold Mountains' and characterizes such ranges by rugged relief and high peaks (traits different from typical block mountains).
A student could use this contrast in morphology (rugged, high peaks vs. flat‑topped horsts) as an additional criterion to assess whether the Alps fit block‑mountain morphology.
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- Explicitly lists the Appalachians with the phrase 'Appalachians in North America'.
- Classifies Appalachians as a very old fold mountain with North American location as an example.
- Describes North America's major physiographic features and places the Appalachian Mountains to the east of the continent.
- Uses the Appalachians as a named geographic feature of the North American landscape.
- Refers to 'the Appalachians of the USA', directly locating the range within the United States (North America).
- Links the Appalachians to other continental mountain chains, reinforcing their North American position.
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- Explicitly identifies the Appalachians as very old fold mountains.
- Links Appalachian formation to continental collision (North America and Europe).
- Classifies 'very old fold mountains' and lists the Appalachians as an example.
- Describes typical features of very old fold mountains (age and rounded, low relief).
- Includes the Appalachians among mountain belts produced when two continents weld, i.e., fold mountain ranges.
- Places Appalachians alongside classic fold ranges (Himalayas, Alps, Urals) in the continent-continent convergence context.
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- Explicitly names the Andes and locates them in South America.
- Refers to Mount Aconcagua as being in South America and the highest peak of the Andes, linking the range to the continent.
- Uses the phrase 'southern Andes' in the context of Patagonia, a region of South America.
- Describes climatic effects of the Andes on Patagonia, tying the range to South American geography.
- Explains the Andes' formation via interaction of the Nazca Plate and the South American Plate, linking the range to the South American landmass.
- Describes features (Peru-Chile trench, continental arc volcanism) specific to the Andean margin of South America.
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- Explicitly lists the Andes among 'Fold mountains' examples.
- Direct categorical statement naming Andes with other fold mountain ranges.
- Identifies the Andes as an example of alpine/young fold mountains.
- Groups Andes with other well-known fold mountain systems (Rockies, Alps, Himalayas).
- Describes Andes formation by convergence and subduction with folding and ongoing uplift.
- Explains folding process and volcanism consistent with fold-mountain formation.
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- [THE VERDICT]: Sitter. Directly solvable from GC Leong (Ch. 2) or NCERT Class XI (Fundamentals of Physical Geography).
- [THE CONCEPTUAL TRIGGER]: Classification of Mountains (Fold, Block, Volcanic, Residual) and their global mapping.
- [THE HORIZONTAL EXPANSION]: Memorize the 'Canonical Examples': - Block (Horst): Vosges (France), Black Forest (Germany), Sierra Nevada (USA), Salt Range (Pakistan). - Rift (Graben): Rhine Valley, East African Rift, Narmada Valley. - Old Fold: Urals, Aravallis, Appalachians. - Young Fold: Alps, Andes, Rockies, Atlas, Himalayas.
- [THE STRATEGIC METACOGNITION]: The examiner's favorite trick is the 'Attribute Swap'. They took the Alps (Fold) and Vosges (Block) and swapped their types. When studying landforms, always create a matrix: Name | Continent | Type | Formation Era (Hercynian/Alpine).
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The Vosges is identified as an inland mountain range in Europe rather than in Central Asia.
High-yield for geography questions that require distinguishing mountain ranges by continent and region; helps eliminate incorrect location options in MCQs and map-based questions. Links to topics on regional physiography and comparative location of European vs Asian mountain systems.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Continental Mountains > p. 133
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Hercynian Mountains > p. 132
Pamir, Tien Shan, Kunlun, Hindukush and Altai are characteristic ranges of Central Asia and are separate from European ranges like the Vosges.
Essential for questions on Central Asian geography, biodiversity and climate influences; enables clear regional classification of mountain systems and supports answers about climatic barriers and biodiversity patterns in Asia.
- Environment and Ecology, Majid Hussain (Access publishing 3rd ed.) > Chapter 4: BIODIVERSITY > europe and central Asia > p. 7
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Continental Mountains > p. 133
Mountains are classified as coastal or inland and by orogenic origin (e.g., Hercynian), which determines their geography and geological history.
Useful for linking physical geography concepts—formation history, location, and morphology—to specific ranges; helps answer questions on mountain genesis, age, and their role in regional physiography.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Continental Mountains > p. 133
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Hercynian Mountains > p. 132
Hercynian and Caledonian mountain-building periods are categorised as old fold mountains, linking named ranges (e.g., Vosges) to fold-mountain classification.
High-yield for tectonics questions: knowing orogenic names lets you classify mountain ranges and their relative ages; connects to geological history and map-based identification tasks in UPSC. Enables elimination-style answers on origin and age of ranges.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > 2) Old Fold Mountains > p. 135
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Hercynian Mountains > p. 132
Mountain classification distinguishes fold, block and volcanic types, and the same range may appear under different type-lists in sources.
Essential for answer-writing on mountain origins and morphology; helps cross-check conflicting classifications and frame balanced answers discussing multiple formation hypotheses. Useful for questions asking to classify specific ranges.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Original or Tectonic Mountains > p. 133
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > 10.2. Fold Mountains > p. 134
Fold mountains form by compression of sedimentary strata in geosynclines and commonly occur at convergent plate margins.
Core concept for tectonics/physiography—links processes (compression, geosyncline) to landforms and global examples; appears frequently in mains/optional geography and helps explain seismicity and volcanic associations.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > 10.2. Fold Mountains > p. 134
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Characteristics of Fold Mountains > p. 136
The Alps are a principal example of the Alpine mountain system and are geographically situated in Europe.
High-yield for physical geography: knowing major mountain systems and regional placement helps answer location and comparison questions. Connects to world physiography, tourism, climate influences, and geopolitics of European highlands.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 10: Types of Mountains > Alpine Mountain System > p. 132
- Exploring Society:India and Beyond. Social Science-Class VI . NCERT(Revised ed 2025) > Chapter 3: Landforms and Life > THINK ABOUT IT > p. 45
Discover the small, exam-centric ideas hidden in this question and where they appear in your books and notes.
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The 'Rhine Rift Valley' separates the Vosges and the Black Forest. Since the valley is a Graben (depressed block), the mountains on either side MUST be Horsts (Block Mountains). This geological relationship is the shadow fact that cements the answer.
Etymology & Definition Hack: The term 'Alpine' literally refers to the Alps. Therefore, the Alps *must* be the archetype of 'Alpine Fold Mountains'. Row 2 says Alps are 'Block mountain'—this is a definitional contradiction. Eliminate Row 2 immediately.
Link to Economic Geography: Old Fold Mountains (Appalachians, Pennines) are globally famous for high-grade Coal/Iron deposits (Carboniferous period). Young Fold Mountains (Andes, Rockies) are associated with Copper/Tin porphyry deposits and active seismicity.
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