Geographical Terms and Isolines: Isobar to Isohyet
Notes on important geographical terms and isolines for exams: isobar, isotherm, isohyet, isobath, isogonic lines and the vocabulary of landforms and oceans.
By GK24 Editorial Team· Published · 5 min read

Geography has a vocabulary of its own, and a large part of the general knowledge paper is simply a test of that vocabulary. One line of a question gives a definition and the four options give four look-alike words: isohyet and isohel, isobar and isobath, isthmus and strait. The words are of two kinds. The first are the isolines, the lines drawn on a map through places having the same value of something, and the second are the names of landforms, of parts of the atmosphere and the ocean, and of features of the earth's interior. Learn the first by the quantity each line measures and the second by a one-line definition, and this chapter becomes two or three certain marks.
What an isoline is
An isoline, also called an isopleth, is a line on a map joining all points at which a quantity has the same value. The Greek prefix iso means equal, and the second half of the word names the quantity: therme for heat, baros for weight or pressure, hyetos for rain, helios for the sun, bathos for depth. A contour on a survey map is an isoline of height; the closely spaced contours of a steep slope and the widely spaced contours of a gentle slope are the first thing a map-reading question tests. On a weather map, isobars drawn at intervals of a few millibars show the pressure pattern, and their spacing gives the pressure gradient, which decides the strength of the wind.
The isolines asked in examinations
| Isoline | Joins places of equal | Where it is used |
|---|---|---|
| Isotherm | Temperature | Climatic maps; drawn after reducing temperature to sea level |
| Isobar | Atmospheric pressure | Weather maps; spacing shows the pressure gradient |
| Isohyet | Rainfall | Rainfall distribution maps |
| Isohel | Duration of sunshine | Maps of sunshine hours |
| Isoneph | Cloudiness or cloud cover | Cloud cover maps |
| Isohume | Relative humidity | Humidity maps |
| Isotach | Wind speed | Upper-air charts, jet stream maps |
| Isohaline | Salinity | Ocean salinity maps |
| Isobath | Depth of water | Ocean and lake bathymetric charts |
| Isohypse or contour | Height above sea level | Topographical sheets |
| Isopach | Thickness of a rock layer | Geological maps |
| Isogonic line | Magnetic declination | Magnetic maps; the agonic line is the line of zero declination |
| Isoclinic line | Magnetic dip or inclination | Magnetic maps; the aclinic line of zero dip is the magnetic equator |
| Isoseismal line | Earthquake intensity | Seismic maps, drawn around the epicentre |
| Isochrone | Travel time from a point | Transport and settlement geography |
| Isodapane | Total transport cost | Weber's theory of industrial location |
| Isotim | Transport cost of one raw material | Weber's theory of industrial location |
Terms of land and water bodies
- Isthmus: a narrow neck of land joining two larger landmasses, such as the Isthmus of Panama; a strait is the water counterpart, a narrow channel joining two seas, such as the Palk Strait.
- Peninsula: land surrounded by water on three sides; a cape is a pointed piece of land projecting into the sea, and an archipelago is a group or chain of islands.
- Atoll: a ring-shaped coral reef enclosing a lagoon; a fjord is a deep, steep-sided inlet of the sea in a glaciated valley.
- Delta: the depositional plain at a river's mouth; an estuary is a funnel-shaped mouth where no delta forms, as with the Narmada and the Tapi.
- Doab: the land between two rivers; the confluence is where two rivers meet, and a watershed or divide is the high ground separating two drainage basins.
- Canyon and gorge are deep, narrow valleys with steep walls; a mesa is a flat-topped highland with steep sides and a butte is the small remnant left when a mesa is eroded further.
Glacial, desert and karst vocabulary
- Glacial: a cirque is the armchair hollow at a glacier's head, an arête the knife-edged ridge between two cirques, a tarn the lake in a cirque, a moraine the ridge of glacial debris, a drumlin an inverted-boat-shaped mound of till and an esker a winding ridge of sand and gravel left by a sub-glacial stream.
- Desert: a barchan is a crescent-shaped sand dune, a yardang a wind-sculpted ridge, a playa the shallow salty lake of an inland basin, a wadi a dry desert valley and loess the fine wind-blown silt deposited far from the desert.
- Karst: stalactites hang from the roof of a limestone cave and stalagmites rise from its floor; a sinkhole or doline is a surface depression, lapies the grooved limestone surface and a polje a large flat-floored karst basin.
Terms of the atmosphere, the oceans and the interior
The earth is nearest the sun at perihelion, about 3 January, and farthest at aphelion, about 4 July. The equinoxes fall about 21 March and 23 September, when day and night are equal everywhere, and the solstices about 21 June and 22 December. A great circle is any circle whose plane passes through the centre of the earth, so the equator is a great circle and the shortest air route between two places lies along one. In the troposphere the normal lapse rate is about 6.5 degrees Celsius for every 1,000 metres of ascent; when the order is reversed and the air above is warmer, it is called a temperature inversion. Albedo is the proportion of insolation reflected back by a surface, and the Coriolis force is the deflecting force of the earth's rotation, right of the direction of motion in the northern hemisphere. In the ocean, the continental shelf is the shallow margin where the richest fishing grounds lie, a trench is the deepest ocean floor feature, a guyot a flat-topped submerged volcanic peak and upwelling the rise of cold nutrient-rich water along a coast. Inside the earth, the focus is where an earthquake originates and the epicentre the point on the surface above it; the Mohorovicic discontinuity separates crust from mantle and the Gutenberg discontinuity mantle from core, while isostasy is the balance between the standing blocks of the crust.
The look-alikes that decide the mark
- Isohyet is rainfall, isohel is sunshine; both begin with the same two letters.
- Isobar is pressure in the air, isobath is depth in the water.
- The agonic line has zero declination; the aclinic line has zero dip and is the magnetic equator.
- An isthmus is land between two seas; a strait is water between two lands.
Exam Point of View
The question is almost always a definition matched to a term, or a term matched to the quantity it measures. Expect one isoline question and one landform or atmosphere term in every general studies paper, and matching sets of four isolines with four quantities in SSC and Railway papers. The traps are fixed: isohyet against isohel, isobar against isobath, isogonic against isoclinic, agonic against aclinic, and isthmus against strait. Map-reading questions use contours, so remember that closely spaced contours mean a steep slope and that the spacing of isobars gives the pressure gradient and hence the wind speed.
Important Facts
| Isotherm | Line joining places of equal temperature, reduced to sea level |
|---|---|
| Isobar | Line joining places of equal atmospheric pressure |
| Isohyet | Line joining places of equal rainfall |
| Isohel | Line joining places of equal duration of sunshine |
| Isoneph | Line joining places of equal cloudiness |
| Isohume | Line joining places of equal relative humidity |
| Isotach | Line joining places of equal wind speed |
| Isohaline | Line joining places of equal salinity |
| Isobath | Line joining points of equal depth of water |
| Isohypse / contour | Line joining points of equal height above sea level |
| Isogonic and agonic | Equal magnetic declination; agonic line has zero declination |
| Isoclinic and aclinic | Equal magnetic dip; aclinic line of zero dip is the magnetic equator |
| Isoseismal | Line of equal earthquake intensity, drawn around the epicentre |
| Isodapane and isotim | Weber's lines of equal total transport cost and of equal cost for one raw material |
| Isthmus and strait | Narrow neck of land between two seas; narrow water channel between two lands |
| Perihelion and aphelion | Earth nearest the sun about 3 January; farthest about 4 July |
| Normal lapse rate | About 6.5 degrees Celsius fall per 1,000 metres of ascent in the troposphere |
| Focus and epicentre | Point of origin of an earthquake inside the earth; the point on the surface vertically above it |
Practice MCQs on this topic
Lines drawn on a map joining places that receive equal amounts of rainfall are called:
- A.Isobars
- B.Isohyets
- C.Isohels
- D.Isotherms
Show answer
The word comes from the Greek hyetos, meaning rain, so an isohyet joins all places on a map that receive the same amount of rainfall in a given period; rainfall distribution maps of India, which show the 200 centimetre and 50 centimetre lines, are drawn with isohyets.
Read the full explanation →An isohel is a line on a map joining places having equal:
- A.Cloudiness
- B.Duration of sunshine
- C.Humidity
- D.Salinity
Show answer
An isohel, from the Greek helios for the sun, joins places that receive sunshine for an equal number of hours, and such maps are used in studies of solar energy potential and of crop seasons.
Read the full explanation →Lines joining points of equal depth of water in an ocean or a lake are known as:
- A.Isobars
- B.Isobaths
- C.Isopachs
- D.Isohypses
Show answer
The Greek bathos means depth, so isobaths are the depth contours of a bathymetric chart; the 200 metre isobath is conventionally taken as the outer edge of the continental shelf.
Read the full explanation →Isoseismal lines on a map are drawn to show equal:
- A.Intensity of an earthquake
- B.Thickness of rock strata
- C.Travel time from a place
- D.Wind speed
Show answer
Isoseismal lines join points at which the shaking of an earthquake was felt with the same intensity, and because intensity falls away from the source, they are drawn as roughly concentric closed curves around the epicentre, the point of the surface vertically above the focus.
Read the full explanation →The line joining places where the magnetic declination is zero is called the:
- A.Isogonic line
- B.Agonic line
- C.Isoclinic line
- D.Aclinic line
Show answer
Magnetic declination is the angle between true north and magnetic north, and along the agonic line that angle is zero, so a compass needle there points to true north.
Read the full explanation →A narrow strip of land that joins two larger landmasses and separates two seas is called:
- A.A strait
- B.An isthmus
- C.An archipelago
- D.A peninsula
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The Isthmus of Panama joins North and South America and separates the Caribbean Sea from the Pacific, and the Isthmus of Suez joins Africa to Asia; both have been cut by canals precisely because they are narrow.
Read the full explanation →In Weber's theory of industrial location, a line joining points of equal total transport cost is called:
- A.An isotim
- B.An isodapane
- C.An isochrone
- D.An isopleth
Show answer
In Alfred Weber's least-cost theory of industrial location, isodapanes are drawn through all points at which the total transport cost, for assembling the raw materials and for distributing the finished product, is the same; the innermost isodapane marks the area of least total cost, where the plant should be sited.
Read the full explanation →Contour lines on a topographical map join points of equal:
- A.Height above sea level
- B.Depth of water
- C.Rainfall
- D.Temperature
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A contour, whose technical name is isohypse, joins all points standing at the same height above sea level and is the chief means of showing relief on a topographical sheet; contours drawn close together mean a steep slope, contours far apart a gentle slope, and contours that merge indicate a…
Read the full explanation →The position of the earth when it is nearest to the sun, about 3 January every year, is called:
- A.Aphelion
- B.Perihelion
- C.Equinox
- D.Solstice
Show answer
The earth's orbit is an ellipse, so its distance from the sun changes through the year; at perihelion, about 3 January, the earth is nearest the sun, which is why the northern winter half of the year is slightly shorter than the summer half.
Read the full explanation →Lines joining places in an ocean having equal salinity are called:
- A.Isohalines
- B.Isobaths
- C.Isotherms
- D.Isopycnals
Show answer
Salinity is the quantity of dissolved salts in a kilogram of sea water, expressed in parts per thousand, and isohalines map its distribution; the open ocean averages about 35 parts per thousand, while enclosed seas with high evaporation such as the Red Sea are far saltier and seas fed by…
Read the full explanation →Frequently Asked Questions
What are isolines in geography?
Isolines, also called isopleths, are lines drawn on a map through all points having the same value of a quantity, such as temperature, pressure, rainfall or height. The prefix iso means equal, and the rest of the word names the quantity measured.
What is the difference between an isohyet and an isohel?
An isohyet joins places receiving equal rainfall, from the Greek hyetos for rain, while an isohel joins places receiving an equal duration of sunshine, from helios, the sun. The pair is a standing favourite with examiners.
What do isobars show on a weather map?
Isobars join places of equal atmospheric pressure reduced to sea level. Their pattern shows cyclones and anticyclones, and their spacing gives the pressure gradient: closely spaced isobars mean a steep gradient and strong winds.
What is the difference between an isthmus and a strait?
An isthmus is a narrow strip of land joining two larger landmasses and separating two seas, as at Panama or Suez. A strait is the opposite: a narrow stretch of water joining two seas and separating two landmasses, as the Palk Strait between India and Sri Lanka.
Which line is called the magnetic equator?
The aclinic line, the line joining places where the magnetic dip or inclination is zero, so a freely suspended magnetic needle rests horizontal. It should not be confused with the agonic line, along which the magnetic declination is zero.
What is a contour line and what does its spacing show?
A contour, or isohypse, joins points of equal height above sea level. Contours close together show a steep slope, contours far apart a gentle slope, and contours that merge indicate a cliff or a waterfall.





