BACKGROUND INFORMATION
Topographic maps are used extensively by a variety of people
including geologists, field biologists, and hikers. A
topographic map is the representation, on a flat surface,
of part of the Earth's surface drawn to scale.
Relief.-- The features shown on topographic maps may be divided into three groups: (1) relief, which includes hills, valleys, mountains, etc.; (2) water features, including lakes, ponds, and streams; and (3) cultural features, man-made features like bridges, canal, buildings, and roads.
Relief is the difference in elevation between any two points. Where relief is low, the area appears to be relatively flat as in river valleys or broad, flat uplands. When relief is high, the area is steep, as in rugged mountainous terrain. Relief determines the contour interval, which is the differences in elevation between adjacent contour lines. A contour line is an imaginary line on the Earth's surface connecting points of the same elevation. Contours can be large for rugged terrain (80 or 100 feet) or they may be small in areas of low relief (10-20 feet). Contour intervals are consistent for a given map, though they may change from map to map. Usually every fifth contour line (an index contour) is printed heavier than the others and bears the elevation above sea level.
In addition to contour lines, heights of many points occur on the map, such as road intersections, summits of hills, lake shorelines, etc. These are spot elevations and are accurate to within the nearest foot or meter. More precisely located and more accurate in elevation are bench marks, points marked by brass plates fixed permanently on the ground. On a topographic map, bench marks are represented by crosses and the elevation, preceded by the letters "BM", is printed in black on the map.
Rules of Contour Lines.-- Some basic rules or facts about
contour lines are listed below.
1. Where a contour line crosses a stream or valley, the
contour bends to form a "V" that points-upstream or-valley.
In the upstream direction the successive contours represent
higher elevations.
2. Contours near the upper parts of hills form closures.
The top of a hill is higher than the highest closed contour.
3. Hollows (depressions) without outlets are shown by closed,
hatched contours. Hatched contours are contours with short
lines on the inside pointing downslope. The bottom of the
hollow is lower than the lowest closed contour.
4. Contours are widely spaced on gentle slopes.
5. Contours are closely spaced on steep slopes.
6. Evenly spaced contours indicate a uniform slope.
7. Contours do not cross or intersect each other, except
in the rare case of an overhanging cliff.
8. All contours eventually close, either on a map or beyond
its margins.
9. A single higher elevation contour never occurs between
two lower ones, and vice versa. A change in slope direction
is always determined by the repetition of the same elevation
either as two different contours of the same value or as
the same contour crossed twice.
Scale -- Scale expresses the relationship between distance on the map and the true distance on the Earth's surface. This is generally expressed as a ratio or a fraction, such as 1 :24,000 or 1/24,000. The numerator, usually 1, represents map distance, and the denominator, a large number, represents ground distance. Thus, 1 :24,000 means that a distance of 1 unit on the map represents 24,000 such units on the ground. The unit here is not important - it could be meters, feet, or inches. What is important is the relationship between the map distance and the true ground distance.
Colors and Symbols-- Each color on a topographic map has significance as follows:
Blue = water features;
Green = woodlands, orchards, etc.;
Red = urban areas, important roads, public-land boundary lines, civil boundaries;
Black = man-made works;
Brown = contour lines.
Purple = new additions in revised versions; usually man-made features
GLOSSARY
bench marks - precisely located points of elevation
marked by brass plates fixed permanently to the ground. On a
topographic map, bench marks are represented by crosses and the
elevation, preceded by the letters BM, is printed in black on the map.
contour interval - the difference in elevation between adjacent contour lines on a map.
contour line - an imaginary line on the Earth's surface connecting points of the same elevation.
index contour - on a topographic map, a contour that is printed heavier than others and is usually labeled with the elevation it represents. Index contours occur at regular intervals, often every fifth or every fourth contour line (depending on the contour interval).
relief - the difference in elevation between any two points.
scale - expresses the relationship between distance on the map and the true distance on the Earth's surface.
spot elevations - elevations of road intersections, summits of hills, lake shorelines, etc. These are accurate to within the nearest foot or meter.
topographic map - the representation on a flat surface of part of the Earth's surface drawn to scale. Most topographic maps also show land boundaries and other man-made features.
QUESTIONS: (To Go With The Attached Map #1)
1) If the first contour line in Map #1 is sea level, what elevation is each of the following points (the contour interval = 10 ft.)?
A_________
B_________
C_________
1_________
2_________
3_________
2) Which is the steepest slope on the hill? (north, south, east, or west) ? How do you know?
3) What is the difference in elevation between the second and fourth layers of your model?
4) If you were to build a house on this hill, where is the flattest part of the land form? Draw a house on the topographic map.
BUILDING A TOPOGRAPHIC MODEL
INTRODUCTION: Topographic maps show the shapes and features of the Earth's surface. A contour line connects places on the map which have the same elevation. To demonstrate the different elevations shown on a two dimensional topographic map, you can build a 3-dimensional model.
PURPOSE:
To make paper models that portray, in three dimensions, features
represented by contour lines on a topographic map.
MATERIALS:
PROCEDURES:
1) Carefully cut the photocopy of the topographic map of
Mount Woodson along the heavy black contour line that
represents the 2000 foot level.
2) Glue this onto a manila folder and cut the folder to match the 2000 foot contour line. This is your template.
3) Trace the outline of your template onto a piece of colored paper. Have a group member carefully cut out the shape.
4) Trace the outline of your template onto a piece of thin cardboard. Have a group member carefully cut out the shape.
5) Glue the colored paper onto the matching thin cardboard
6) Carefully trim the template to the next contour line. This is the next level of your model.
7) Repeat steps 3-6 until you have cut out all of the contour lines.
8) Now you are ready to build your 3-D model. Glue together (in order) the different elevation levels of the model. The spacers (the thickness of the cardboard) represent the increase in elevation between each contour line (contour interval).
Questions about the Mount Woodson model:
1. Look at one of the topographic maps of the San Pasqual quadrangle.
What is the scale of the map?
2. Now find Mt. Woodson. Find the 2000 foot contour interval. Measure the length, along the long axis, of Mt. Woodson from the 2000 foot contour interval on one side to the 2000 foot contour interval on the other side. Looking at your model may help. How many inches?
3. Now, using the scale at the bottom of the topographic maps of the San Pasqual quadrangle, determine how many feet across Mt. Woodson from the 2000 foot contour interval on one side to the 2000 foot contour interval on the other side.
4. Now look at the topographic maps entitled "Ramona". What is the scale of this map?
5. Now find Mt. Woodson. How does the size of Mt. Woodson on the San Pasqual topographic map differ from that of the Ramona topographic map?