Earth Features in Two Dimensions Flashcards

(30 cards)

1
Q

It is a type of map used by geologists, engineers and geographers

A

Topographic map

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2
Q

A topographic map represents the Earth’s surface in …

A

horizontal and vertical distance

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3
Q
  • or vertical distance is depicted as *
A

elevation

contour lines

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4
Q

These are continuous lines that connect points of equal elevation above or below a reference plane on the Earth’s surface

A

contour lines

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5
Q

It is called the reference plane

A

datum

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6
Q

Elevations are measured for topographic maps through reference plane. What is the reference plane/datum?

A

mean (average) sea level

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7
Q

The datum and contour interval are usually declared in the lower central margin of the map
(Datum = mean sea level)

A

pass

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8
Q

It defines the vertical difference in the elevation or depth between nearby contour lines and is constant for a given topographic map.

A

contour interval (CI)

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9
Q

Contour interval defines the * between nearby contour lines

A

vertical difference in the elevation or depth

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10
Q

Lines printed thicker than the normal contour line

A

Index

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11
Q

Reference points called * represent * points of elevation

A
bench marks (BM)
known
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12
Q

The difference in elevation between two points on a topographic map

A

relief

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13
Q

Difference between the highest and lowest points on a map

A

total relief

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14
Q

Distance in elevation between two specific points

A

local relief

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15
Q

The relief divided by the distance between two particular points gives the * between those points

A

slope or gradient

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16
Q

It is the rise over run between the given points

A

slope or gradient

17
Q

How is a topographic map constructed?

A

A topographic map is constructed by measuring elevations in the field and plotting these using their corresponding coordinates.

18
Q

Between points of known measurements, elevations are * and contour lines are drawn to separate elevations greater or less than the represented value

A

*interpolated (estimated)

19
Q

It is the easiest method of interpolation wherein it assumed that the gradient between two points is uniform; that is the distance between two points is measured and the units between them are equally distributed

A

linear interpolation

20
Q

Steep slopes are shown by * contours, while gentle slopes are relatively *. * contour lines represent uniform slope.

A

closely spaced,
wider-spaced,
Evenly spaced

21
Q
  • slopes are shown by closely spaced contours, while * slopes are relatively wider-spaced. Evenly spaced contour lines represent * slope.
A

Steep, gentle, uniform

22
Q

Contour lines never cross, except to show an * where the * contours are dashed. Contour lines can also * to form a single line along a *.

A

overhanging cliff, hidden

merge, vertical cliff face

23
Q

Contour lines never *, except to shown an where the hidden contours are * . Contour lines can also merge to form a * along a vertical cliff face.

A

cross, dashed, single line

24
Q

Hills, mountains and volcanoes are generally represented by a * of *. A concentric series of closed contours with * on the downhill side represents a closed depression

A

concentric series, closed contour lines

hachure marks

25
* are generally represented by a concentric series of closed contour lines. A concentric series of closed contours with hachure marks on the downhill side represents a *
Hills, mountains and volcanoes | closed depression
26
When contour lines cross * channels, they form a 'V' that points *. Contours that occur on * side of ridges and valleys are always *.
streams or dry stream upstream opposite, paired
27
When contour lines * streams or dry stream channels, they form a '*' that points upstream. Contours that occur on opposite side of * are always paired.
cross, V | ridges and valleys
28
A difference in horizontal and vertical scales causes a *. This is almost always necessary in the construction of a readable profile, because without vertical exaggeration, the profile may be so * that only the highest peaks are *
``` vertical exaggeration (VE) shallow, visible ```
29
A * causes a vertical exaggeration (VE). This is almost always necessary in the construction of a readable profile, because without vertical exaggeration, the profile may be so shallow that only the * are visible
difference in horizontal and vertical scales | highest peaks
30
Vertical exaggeration formula If you have a vertical exaggeration of 3, it indicates the relief shown on the profile is 3 times * than the true relief.. This makes the slopes on the profile 3 times * than the corresponding slopes in "real life"
fractional vertical scale/fractional horizontal scale | greater, steeper