Question 1

Physical Geography — Southern Temperate Zone In world regional climatology, the Southern Temperate Zone is the belt of latitudes lying between which two standard parallels/circles of latitude? Choose the most accurate pair.

Accepted Answer

Introduction / Context: Geographers divide Earth's surface into heat zones using well-defined latitude lines: the equator, the two tropics, and the two polar circles. The temperate zones fall between the tropics and the respective polar circles. This question checks whether you can correctly locate the Southern Temperate Zone using these reference parallels. Given Data / Assumptions: Tropic of Capricorn is at about 23.5° S. Antarctic Circle is at about 66.5° S. Temperate zones are between a tropic and a polar circle, not between a polar circle and the pole. Concept / Approach: The Earth's axial tilt (~23.5°) defines the tropics and polar circles. The temperate zone lies between each tropic and its corresponding polar circle: in the south that is from the Tropic of Capricorn to the Antarctic Circle. Regions poleward of the Antarctic Circle belong to the frigid (polar) zone; regions equatorward of the Tropic of Capricorn belong to the tropical zone. Step-by-Step Solution: Identify southern markers: Tropic of Capricorn (23.5° S) and Antarctic Circle (66.5° S).Recall definition: Temperate = between a tropic and a polar circle.Match to options: the correct bracket is Tropic of Capricorn ↔ Antarctic Circle.Select option that states exactly this pair. Verification / Alternative check: Any school atlas diagram of heat zones shows the temperate bands between 23.5° and 66.5° in each hemisphere, confirming the boundaries above. Why Other Options Are Wrong: Antarctic Circle and South Pole: That is the frigid/polar zone. Tropic of Cancer and Tropic of Capricorn: That is the tropical zone. Tropic of Capricorn and the equator: Also tropical, not temperate. Common Pitfalls: Mixing up the southern markers or assuming symmetry but pairing the wrong lines. Remember: temperate sits between the near tropic and the near polar circle. Final Answer: the Tropic of Capricorn and the Antarctic circle

Question 2

Seismology — Where Do Earthquake Waves Originate? In an earthquake, transverse (S), longitudinal (P), and surface waves ultimately trace back to which point of origin in the Earth system?

Accepted Answer

Introduction / Context: Basic seismology distinguishes the hypocentre (focus) and the epicentre. P and S body waves originate at depth and travel through the Earth, while surface waves are generated as body waves interact with near-surface layers. Correctly naming the point of origin is foundational for reading seismograms and locating earthquakes. Given Data / Assumptions: P waves (longitudinal) and S waves (transverse) propagate from a subsurface source. Surface waves are produced near the surface but are ultimately triggered by the deep source rupture. “Focus” (hypocentre) is within the Earth; “epicentre” is the surface projection. Concept / Approach: The earthquake starts at the focus (also called the hypocentre) within the Earth's crust or upper mantle. The epicentre is the point directly above it on the surface. Thus, all seismic wavefronts trace back to the focus as the initiation point of elastic energy release, even though surface waves propagate along the surface after conversion. Step-by-Step Solution: Define terms: focus = subsurface origin; epicentre = surface projection.Identify where rupture and energy release begin → the focus.Therefore, select the choice that states “focus within the body of the earth.” Verification / Alternative check: Seismic location solutions always report a latitude–longitude (epicentre) and a depth (focus). This dual report demonstrates the real subsurface origin. Why Other Options Are Wrong: Epicentre within/on the body: Epicentre is not within the body; it is on the surface. Focus on the surface: By definition the focus is not on the surface. Common Pitfalls: Using “epicentre” and “focus” interchangeably. They are linked but distinct; the focus is the true origin point. Final Answer: the focus within the body of the earth

Question 3

Astronomy — Equinox Months The two annual equinoxes (when day and night are approximately equal worldwide) occur in which pair of months?

Accepted Answer

Introduction / Context: Equinoxes mark the moments when the Sun crosses the celestial equator and the Earth experiences roughly equal day and night lengths. This is a staple concept for calendars, seasons, and celestial navigation. Knowing the typical months helps in correlating seasonal changes across hemispheres. Given Data / Assumptions: Equinoxes occur twice each year. Vernal (March) equinox begins northern spring; autumnal (September) equinox begins northern autumn. Dates shift slightly year to year (around 20–23 of the month) but the months are consistent. Concept / Approach: Because of Earth's orbit and axial tilt, the Sun's apparent path intersects the celestial equator around March and September annually. These are the only months that fit the global pattern of day–night equality, with solstices occurring in June and December instead. Step-by-Step Solution: Recall seasonal markers: March & September → equinoxes; June & December → solstices.Match to options: choose March and September.Confirm global effect: equal day and night lengths around these dates. Verification / Alternative check: Any astronomical almanac or school atlas calendar highlights equinoxes in March and September. Why Other Options Are Wrong: January/June and July/December include a solstice month rather than equinox pairs. September/December pairs an equinox with a solstice. Common Pitfalls: Confusing equinoxes with solstices, which mark maximum/minimum solar declination. Final Answer: March and September

Question 4

Climate Patterns — Where Is the Smallest Annual Temperature Range? Considering global climate zones, which zone typically exhibits the smallest annual (seasonal) temperature range?

Accepted Answer

Introduction / Context: Annual temperature range refers to the difference between average temperatures of the warmest and coldest months. This is governed by latitude, ocean–land distribution, and atmospheric circulation. Identifying the zone with the tightest range helps explain biodiversity patterns, agriculture, and energy demand. Given Data / Assumptions: The equator receives nearly constant solar input year-round. Oceanic influence is strong in many equatorial regions. Higher latitudes experience larger seasonal contrasts due to changing solar angles and day length. Concept / Approach: Near the equator, the Sun's altitude and day length vary little through the year, so monthly means are similar. Subtropical, temperate, and polar zones see progressively greater seasonality because of axial tilt effects and, in continental interiors, reduced oceanic moderation. Therefore, the equatorial tropical zone has the smallest annual range. Step-by-Step Solution: Compare insolation variability by latitude: minimal at equator, large at poles.Consider oceanic moderation; many equatorial regions are maritime.Conclude smallest seasonal swing occurs in the equatorial tropical zone.Select the option naming this zone. Verification / Alternative check: Climatology maps show equatorial isotherms nearly horizontal and closely spaced by month, indicating small seasonal variation. Why Other Options Are Wrong: Subtropical and temperate zones show distinct seasons; ranges are larger. Polar zones have extreme seasonality tied to 24-hour daylight/darkness cycles. Common Pitfalls: Assuming “hot” means “big range.” Heat level is different from variability; equatorial climates are hot but stable. Final Answer: equatorial tropical climate zone

Question 5

Astronomical Time — Interval Between Vernal Equinoxes The time from one March (vernal) equinox to the next aligns most closely with which of the following durations?

Accepted Answer

Introduction / Context: The cycle from one vernal equinox to the next defines the tropical year, which underpins our civil calendar. Understanding this duration explains why leap years are required and why seasons recur at approximately the same calendar dates each year. Given Data / Assumptions: Tropical year ≈ 365.2422 days. Options are coarse (whole-number) approximations. We seek the nearest whole-day figure. Concept / Approach: The interval between successive vernal equinoxes is slightly more than 365 days. Calendars approximate this with 365 days most years and add a leap day roughly every four years to keep seasons aligned. Among the choices, 365 days is far closer to 365.2422 than the other options. Step-by-Step Solution: Recall tropical year ≈ 365.24 days.Compare options: 365 is closest to 365.24.Select 365 days as the nearest whole-day approximation.Note: fractional remainder handled via leap-year rules. Verification / Alternative check: The Gregorian calendar uses 97 leap days every 400 years to average 365.2425 days per year, closely tracking the tropical year. Why Other Options Are Wrong: 359, 361, 363 days are far from the accepted tropical year length. Common Pitfalls: Confusing the sidereal year (≈ 365.2564 days) with the tropical year; both are near 365 but the tropical year governs equinox-to-equinox timing. Final Answer: 365 days

Question 6

Materials & Soils — Clay for Brick-Making In traditional construction, which soil type commonly provides the plastic, fine-grained clay used to make bricks for house construction?

Accepted Answer

Introduction / Context: Bricks are typically made from fine-grained, plastic clays that can be molded, dried, and fired. The suitability of soil for brick-making depends on texture, mineralogy, and the presence of salts or organic matter. This question asks you to identify the soil source that commonly supplies workable brick clays in many regions. Given Data / Assumptions: Good brick earth needs fine particles (clay/silt) with manageable plasticity. Excess salts (saline/alkaline) cause efflorescence and weakness. The query is at school level and seeks the most common, practical source. Concept / Approach: Alluvial deposits along rivers often contain layered silts and clays that, after proper mixing and tempering, make good bricks. Laterite soils can be cut into blocks (laterite stone) but are not the standard plastic clays for molded bricks. Black soils (vertisols) shrink–swell strongly and need careful processing; saline–alkali soils are unsuitable due to soluble salts and poor structure. Step-by-Step Solution: Identify required properties: fine texture, plasticity, low harmful salts.Match common field sources: floodplains and alluvial terraces supply suitable clays.Eliminate soils with problematic chemistry (saline/alkali) or structure (extreme shrink–swell).Choose “alluvial soil.” Verification / Alternative check: Handbooks on brick-making emphasize riverine/alluvial clays and silts as common raw materials, subject to testing and blending for optimal performance. Why Other Options Are Wrong: Black soil: High shrink–swell; not a preferred universal choice without modification. Laterite soil: Used as stone blocks; not typical plastic brick clay. Saline and alkaline soils: Detrimental salts lead to efflorescence and weakness. Common Pitfalls: Assuming any clayey soil is fine; soluble salts and organics must be controlled to avoid firing defects. Final Answer: alluvial soil

Question 7

Plate Tectonics — Types of Convergent Boundaries Convergent plate margins can occur in which combinations of lithosphere types? Identify the correct set(s).

Accepted Answer

Introduction / Context: Convergent boundaries form where plates move toward each other. The nature of convergence depends on whether the colliding plates are oceanic or continental. Recognizing all possible pairings is essential for understanding trenches, volcanic arcs, and mountain belts. Given Data / Assumptions: I = oceanic–oceanic convergence. II = oceanic–continental convergence. III = continental–continental convergence. Concept / Approach: All three pairings occur in nature. Oceanic–oceanic convergence typically creates island arcs and deep-ocean trenches. Oceanic–continental convergence produces volcanic mountain chains on the continent and a trench offshore. Continental–continental convergence, after consuming intervening oceanic lithosphere, produces high plateaus and mountain ranges through crustal shortening and thickening. Step-by-Step Solution: List pairings: I, II, III are the classic three convergent types.Confirm geologic expressions: island arcs, Andean arcs, Himalayan-type orogens.Since all are real, choose “All of the above.” Verification / Alternative check: Examples: I (Mariana), II (Andes), III (Himalaya). These verify all three types exist. Why Other Options Are Wrong: Any subset (I, II), (II, III), (I, III) omits a valid convergent style. Common Pitfalls: Thinking continental–continental convergence requires active subduction; it follows after subduction closure and manifests mainly as collision and thickening. Final Answer: All of the above

Question 8

Atmospheric Sciences — Weather vs. Climate The discipline that focuses on day-to-day variations in weather (as distinct from long-term averages) is called:

Accepted Answer

Introduction / Context: “Weather” describes atmospheric conditions over short periods (hours to days), while “climate” describes long-term statistics (decades). Different scientific branches emphasize these time scales. Recognizing the correct term is essential for interpreting forecasts versus climate normals. Given Data / Assumptions: Focus is daily to weekly variability. Not concerned with 30-year normals or long-term trends in this question. Terminology is standard in earth sciences curricula. Concept / Approach: Meteorology examines atmospheric processes that drive immediate weather: fronts, convection, cyclones, jet streams, and precipitation systems. Climatology compiles and analyzes statistical properties over long periods. Cyclogenesis is a specific process (formation/intensification of cyclones), not the entire discipline of daily weather study. Step-by-Step Solution: Identify the time scale: day-to-day → weather.Map to the field: weather science → meteorology.Exclude climatology (long-term) and cyclogenesis (a process within meteorology).Select “meteorology.” Verification / Alternative check: National weather services and forecast centers are staffed by meteorologists; climate research institutes focus on climatology and long-term change. Why Other Options Are Wrong: Climatology: Averages and trends over decades or more. Cyclogenesis: One phenomenon, not the entire study of day-to-day weather. None: Incorrect because the correct term exists. Common Pitfalls: Using the words interchangeably. Always tie “meteorology” to short-term forecasting and analysis. Final Answer: meteorology

Question 9

World Geography — Identifying the Southernmost Location Listed Among the following prominent locations, which lies farthest to the south on the globe?

Accepted Answer

Introduction / Context: Being able to rank places by latitude is a fundamental map skill. This question contrasts a few well-known southern-hemisphere locations with one near the equator to see if you can identify which is the farthest south. Given Data / Assumptions: Southern hemisphere latitudes increase in value as you move away from the equator. Cape Horn (often written “Cape of Horn” in older texts) is at the southern tip of South America. Wellington (NZ) and Cape of Good Hope are further north than Cape Horn; Colombo is in the northern hemisphere. Concept / Approach: Check approximate latitudes: Cape Horn is near 56° S; Wellington around 41° S; Cape of Good Hope around 34° S; Colombo is ~7° N. The farther from the equator toward the pole in the southern hemisphere, the larger the S latitude number; hence Cape Horn is the farthest south among the choices. Step-by-Step Solution: List candidate latitudes qualitatively: Horn (mid-50s S) > Wellington (~41 S) > Good Hope (~34 S) > Colombo (~7 N).Compare: 56 S is farthest south among the set.Select “Cape of Horn, S. America.” Verification / Alternative check: Any atlas confirms Cape Horn lies well below 50° S, beyond the other listed sites. Why Other Options Are Wrong: Cape of Good Hope: Considerably farther north than Cape Horn. Colombo: Northern hemisphere, not south at all. Wellington: Southern, but not as far south as Cape Horn. Common Pitfalls: Confusing “Cape of Good Hope” with “Cape Agulhas” (Africa’s true southern tip at ~35° S); even Cape Agulhas is far north of Cape Horn. Final Answer: Cape of Horn, S. America

Question 10

Human Geography — Scope of Study What does contemporary human geography include within its scope at an introductory level?

Accepted Answer

Introduction / Context: Human geography examines how human activities, institutions, and cultural practices are distributed across space and how they shape—and are shaped by—places and regions. The field spans multiple subdisciplines that connect social science and spatial analysis. Given Data / Assumptions: Introductory scope typically includes cultural, economic, political, and urban geography, and elements of behavioral geography. Focus is on spatial patterns, processes, and the human–environment relationship. The question asks whether these themes are part of human geography. Concept / Approach: Cultural geography studies language, religion, identity, and landscapes; economic geography maps production, trade, and development; political geography examines states, borders, and geopolitics; urban geography interprets cities, transport, and settlement systems; behavioral geography explores decision-making and spatial perception. Together these form the core of human geography's curriculum and research concerns. Step-by-Step Solution: Check each option against human geography's subfields.Society and culture → cultural geography (included).Behaviour and urban systems → behavioral and urban geography (included).Economics and politics → economic and political geography (included).All listed areas are within scope → choose “All of the above.” Verification / Alternative check: Standard human geography textbooks structure chapters around culture, economy, politics, urbanization, population, and development—matching the options provided. Why Other Options Are Wrong: Picking any single theme understates the breadth of human geography. Common Pitfalls: Confusing human geography with physical geography; the latter covers landforms, climate, biomes, and hydrology, though both intersect in human–environment studies. Final Answer: All of the above

Question 11

Igneous Petrology — What Controls the Rock Type That Forms from Magma? In igneous geology, the specific type of igneous rock that crystallises from a magma depends on multiple factors. Which factors collectively govern the rock that ultimately forms?

Accepted Answer

Introduction / Context: Igneous rocks form when molten material (magma or lava) cools and solidifies. Petrologists classify these rocks based on mineral content, texture, and genesis. The final rock type is not determined by a single variable; instead, multiple controls act together during crystallisation to produce the observed mineral assemblages and textures. Given Data / Assumptions: Magma has a definable bulk chemistry (silica, alkalis, iron, magnesium, calcium, etc.). Cooling occurs over a temperature range and may be slow (plutonic) or fast (volcanic). Textures (grain size, porphyritic character, glassiness) reflect cooling history and nucleation/growth kinetics. Concept / Approach: Mineralogy follows compositional rules (e.g., basaltic vs granitic chemistries) and phase equilibria. Temperature determines which minerals are stable at a given moment, while the rate of cooling controls crystal size and the extent to which equilibrium is achieved. The interaction among composition, temperature, and cooling rate produces the spectrum of igneous rocks from fine-grained basalts to coarse-grained granites, including porphyritic and glassy varieties. Step-by-Step Solution: Composition sets potential minerals: silica-rich magmas tend to quartz, K-feldspar, muscovite; silica-poor to olivine, pyroxene, Ca-plagioclase.Temperature path dictates crystallisation sequence and stability fields for minerals as the melt cools.Cooling rate governs texture: slow cooling → coarse grains; rapid cooling → fine grains or glass; mixed cooling → porphyritic textures.Combine factors: the same chemistry can yield different textures under different cooling histories, and different chemistries yield different mineral suites at similar temperatures. Verification / Alternative check: Phase diagrams and experimental petrology demonstrate mineral appearance/disappearance with changing temperature and composition; natural examples (e.g., shallow dikes vs deep plutons) show texture shifts due to cooling rate. Why Other Options Are Wrong: Single-factor choices ignore the coupled influence of chemistry, temperature path, and kinetics, leading to incomplete predictions. Common Pitfalls: Assuming texture alone defines rock type; both mineralogy (from composition) and texture (from cooling rate) must be considered, along with the temperature history. Final Answer: All of the above

Question 12

Seasonal Astronomy — When Does Spring Begin in the North Temperate Zone? Identify the celestial condition that marks the start of spring (the vernal equinox) in the Northern Hemisphere.

Accepted Answer

Introduction / Context: Seasons are governed by Earth’s axial tilt and its orbit around the Sun. In calendar and celestial terms, the Northern Hemisphere’s spring begins at the vernal equinox, one of two times each year when day and night are nearly equal worldwide. Given Data / Assumptions: The question concerns the specific solar declination at spring onset. Vernal equinox occurs around March 20–21. Overhead Sun position refers to solar declination matching surface latitude at local noon. Concept / Approach: At each equinox, the Sun’s declination is 0°, meaning it is directly overhead at the geographic equator. Solstices differ: at the June solstice the Sun is overhead at the Tropic of Cancer (approximately 23.5° N), marking the start of Northern summer; at the December solstice it is overhead at the Tropic of Capricorn (approximately 23.5° S), marking Northern winter. Therefore, the start of spring corresponds to the Sun being directly overhead the equator. Step-by-Step Solution: Recall equinox condition: solar declination = 0°.Match overhead position: equator at local noon.Identify seasonal label: vernal equinox → Northern spring.Select the option that states the Sun is directly overhead the equator. Verification / Alternative check: Analemma/equation of time charts and astronomy references show declination crossing 0° at equinoxes, confirming the overhead equator condition. Why Other Options Are Wrong: Tropic of Cancer: June solstice → start of Northern summer, not spring.“Sun returns to equator”: Vague phrasing; while true conceptually, the precise and accepted statement is overhead at equator.“Sun is at the Tropic of Cancer”: Repeats solstice condition, not equinox. Common Pitfalls: Confusing equinox with equal temperature; it actually refers to equal day and night lengths due to Earth’s geometry, not weather conditions. Final Answer: the sun is directly overhead the equator

Question 13

Great-Circle Measurement — Tool for Shortest Earth Distance Which representation is most useful for measuring the shortest distance and route between two places on Earth’s surface?

Accepted Answer

Introduction / Context: On a sphere, the shortest path between two points lies along a great circle. Flat maps distort distances and directions to varying degrees. Selecting the correct tool to visualise true shortest routes is fundamental to navigation and geography. Given Data / Assumptions: Earth is approximately an oblate spheroid; for route planning it is treated as a sphere. Different map projections preserve different properties (area, shape, distance, direction), but not all simultaneously. We need the most faithful depiction for great-circle distance. Concept / Approach: A globe preserves Earth’s geometry without projection distortion, so great circles can be traced directly to yield shortest routes. Atlas, thematic, and wall maps are flat projections; while some projections can represent great circles as straight lines (e.g., gnomonic) or preserve distances from a point, they still require interpretation and conversion. For straightforward accuracy, the globe is superior. Step-by-Step Solution: Define shortest path: great-circle arc on a sphere.Identify medium without distortion: three-dimensional globe.Evaluate alternatives: flat maps introduce projection error.Choose “Globe.” Verification / Alternative check: Airline routes drawn on globes follow great-circle arcs; on Mercator maps they appear curved because of projection effects, confirming the globe’s fidelity for distance. Why Other Options Are Wrong: Atlas/Thematic/Wall maps: Useful, but projection choice limits direct shortest-distance measurement without corrections. Common Pitfalls: Assuming a straight line on any map is always the shortest path; this depends on the projection and is generally untrue outside special cases. Final Answer: Globe

Question 14

Soils and Climate — Which Soil Forms Under Heavy Rainfall, High Humidity, and Dense Vegetation? Identify the soil type typically found where rainfall is heavy, humidity is high, and vegetation growth is luxuriant and waterlogged conditions commonly …

Accepted Answer

Introduction / Context: Climate and drainage strongly influence soil formation. In regions with persistent moisture and abundant vegetation, organic matter can accumulate faster than it decomposes, creating distinctive hydromorphic soils important to ecology and land use planning. Given Data / Assumptions: Environment: heavy rainfall, high humidity, vigorous plant growth. Waterlogging or poor drainage is common under such conditions. We match soils to formative environment. Concept / Approach: Under saturated, anaerobic conditions, plant remains only partially decompose, accumulating as peat within marshes, bogs, and swamps. These peat and marshy soils are rich in organic matter but often acidic, low in mineral nutrients, and compressible. By contrast, saline and alkaline soils form in arid to semi-arid settings with high evaporation and poor leaching. Black soils (vertisols) develop from basaltic parent materials in seasonal climates with swelling clays. Alluvial soils form from river deposits and span many climates but are not specifically tied to constant high humidity and waterlogging. Step-by-Step Solution: Relate climate (wet, humid) → low oxygen in saturated profiles.Low oxygen slows decomposition → organic matter builds up to form peat.Name the resulting soil: peat and marshy soil.Exclude arid or basalt-specific soils that do not match the stated environment. Verification / Alternative check: Wetland classifications and soil surveys consistently map peat/muck soils in high-rainfall, poorly drained landscapes such as coastal marshes and montane bogs. Why Other Options Are Wrong: Saline/alkaline: Typically in dry climates with evaporation > precipitation.Black soil: Associated with basaltic parent material and pronounced dry-wet cycles.Alluvial: Riverine deposition, not necessarily persistently waterlogged and humic. Common Pitfalls: Equating dense vegetation with high fertility; peat soils may be nutrient-poor and acidic despite lush growth. Final Answer: peat and marshy soil

Question 15

Rock Strength and Bonding — Where Are the Strongest Interparticle Bonds Typically Found? Considering the bonding and textures among rock classes, which rocks commonly exhibit the strongest internal particle-to-particle bonds?

Accepted Answer

Introduction / Context: Rock strength depends on mineral bonding, fabric, porosity, and cementation. Different rock classes form under different processes which influence how grains are held together, affecting engineering behaviour and erosion resistance. Given Data / Assumptions: Igneous rocks crystallise from melt, often forming interlocking crystals. Metamorphic rocks recrystallise under heat and pressure, developing foliation or granular textures. Sedimentary rocks are typically clastic or chemical, with grains bound by cement. Concept / Approach: Many igneous rocks (e.g., granite, diorite, gabbro) feature an interlocking crystalline texture that yields strong, cohesive bonding with low primary porosity. While some metamorphic rocks are extremely strong (e.g., quartzite, gneiss), foliation planes may introduce anisotropy and potential weakness. Clastic sedimentary rocks (e.g., sandstone, shale) rely on secondary cement (silica, calcite, iron oxides) and can be weak where cement is poor or clay content is high. Thus, as a generalised statement for introductory exams, igneous rocks are credited with the strongest bonds overall. Step-by-Step Solution: Compare formation: melt crystallisation vs recrystallisation vs cementation.Evaluate textures: interlocking igneous crystals provide high cohesion.Account for variability but choose the broadly correct class.Select igneous rocks as the common case with strongest bonding. Verification / Alternative check: Engineering handbooks and rock mechanics texts report high unconfined compressive strengths for massive igneous rocks relative to many sedimentary units and foliated metamorphic rocks. Why Other Options Are Wrong: Metamorphic: Can be strong but may be anisotropic along foliation.Sedimentary: Strength depends on cement; often weaker than crystalline igneous.All similar: False; strength varies widely by class and texture. Common Pitfalls: Overgeneralising without considering anisotropy; even strong rocks can have weak planes that control failure. Final Answer: igneous rocks

Question 16

The place of origin of an earthquake is called

Accepted Answer

Focus

Question 17

Which city is known as 'Gold capital of the world' ?

Accepted Answer

Johannesburg

Question 18

Eclipses occur due to which optical phenomena

Accepted Answer

Rectilinear propagation

Question 19

Name the Continents that form a mirror image of each other___

Accepted Answer

Africa and South America

Question 20

The difference in the duration of day and night increases as one moves from

Accepted Answer

Equator to poles

World Geography Questions