Adventist Youth Honors Answer Book/Recreation/Orienteering (General Conference)

Please note that this honor is not the Orienteering Honour of the South Pacific Division. So for the international sport called Orienteering check out the Separate honour with a different token.

1. Explain what a topographic map is, what you expect to find on it, and three uses for it.
Topographic maps are also commonly called contour maps or "topo maps." Topographic maps conventionally show topography, or land contours, by means of contour lines. Contour lines are curves that connect contiguous points of the same altitude. In other words, every point on the marked line of 100 m elevation is 100 m above mean sea level.

Other than showing elevation via the contours, you can also expect a topographic map to show any important landmarks, such as rivers, lakes, and roads. They will often also show railroad tracks and major power lines (and their towers). Power lines are especially handy because the towers are visible from great distances and each represents a point on a map (whereas a road or river would represent a curved line). These attributes make them ideal for pinpointing position.

Topographic maps have many uses, letting a competent user determine any of the following:
 * Where he is.
 * How to get where he wants to go.
 * What the terrain is like in a given area (steepness, for example).
 * Where a river comes from and goes to.
 * The route a hiking trail follows.
 * The location of campsites.
 * The distance between two points.
 * Elevation of a mountaintop.
 * Latitude and longitude of any point on the map.
 * What areas may be susceptible to avalanches or flooding.

2. Identify at least 20 signs and symbols used on topographic maps.
The U.S Department of the Interior and the U.S. Geological Survey publish a guide to Topographic Map Symbols, it can be found at the URL https://pubs.usgs.gov/gip/TopographicMapSymbols/topomapsymbols.pdf

Note: the National park sybols illustrated here do not appear on topographic maps published by the U.S Department of the Interior or the U.S. Geological Survey.

3. Give the nomenclature of an orienteering compass.


The lensatic compass consists of three major parts: the cover, the base, and the lens.


 * a. Cover: The compass cover protects the floating dial. It contains the sighting wire (front sight) and two luminous sighting slots or dots used for night navigation.


 * b. Base: The body of the compass contains the following movable parts:
 * The floating dial is mounted on a pivot so it can rotate freely when the compass is held level. Printed on the dial in luminous figures are an arrow and the letters E and W. The arrow always points to magnetic north and the letters fall at east (E) 90° and west (W) 270° on the dial. There are two scales; the outer scale denotes mils and the inner scale (normally in red) denotes degrees.
 * Encasing the floating dial is a glass containing a fixed black index line.
 * The bezel ring is a ratchet device that clicks when turned (on some compasses). It contains 120 clicks when rotated fully; each click is equal to 3°. A short luminous line that is used in conjunction with the north-seeking arrow during navigation is contained in the glass face of the bezel ring.
 * The thumb loop is attached to the base of the compass.


 * c. Lens: The lens is used to read the dial, and it contains the rear-sight slot used in conjunction with the front for sighting on objects. The rear sight also serves as a lock and clamps the dial when closed for its protection. The rear sight must be opened more than 45° to allow the dial to float freely.

4. Know the meaning of the following terms

 * a. Elevation: The height of a point in relation to sea level.
 * b. Contour interval: The elevation change between adjacent contour lines on a topographic map. If you travel from one contour line to another, your change in elevation will equal the contour interval.
 * c. Magnetic North: Magnetic North is the direction a compass will point, which is towards the North Magnetic Pole. The North Magnetic Pole is not the same place as the Geographic North Pole.  The North Magnetic Pole is the point on the Earth's surface where the Earth's magnetic field points directly downwards. This pole is constantly wandering; its estimated 2005 position was 82.7° N 114.4° W.
 * d. Declination: The angular difference between magnetic north and true north (defined in reference to the Geographic North Pole), at any particular location on the Earth's surface, is called the magnetic declination. In other words, it's how far off a compass is from True North, or the correction that must be applied to a compass reading.
 * e. Scale: An important property of a map is the scale. It can be indicated by a scale bar and/or a ratio 1:n. This enables the map user to measure a distance on the map and determine the distance on the ground. These days maps are usually produced under the metric system which makes it easy to perform this task. Maps are usually produced at standard scale factors of (say) 1:10,000 or 1:50,000 or 1:100,000 and all you need to do is take a measurement on the map (in mm) and multiply that figure by the scale factor to determine the distance on the ground. However, maps from some countries may use imperial units, especially older maps. These maps displayed scale ratios but often they were of the form 60 chains (a chain is 22 yards, or 66 feet) to 1 inch or 2 miles to 1 inch, etc.
 * f. Measuring: The act of determining distance on a map and Converting it to distance on the ground. In order to do this translation, you must know the map's scale (see above).  Measuring can be done with a ruler or with calipers.
 * g. Back-azimuth: See under azimuth below.
 * h. True North: True North is the direction from any point on the Earth's surface to the Geographic North Pole.
 * i. Azimuth: The azimuth is a compass bearing expressed in degrees.  There are 360° in a circle, and North is, by convention, 0° (or 360°).  East is 90°, South is 180°, and West is 270°.  While azimuth expresses the compass bearing in the direction of interest, the Back Azimuth expresses the compass bearing in exactly the opposite direction.  In other words, azimuth is the direction to which you are going, and back azimuth is the direction from which you are coming.  The back azimuth can be calculated by adding or subtracting 180° from the azimuth.  Add if the azimuth is less than 180°, otherwise subtract.
 * j. Distance: Distance is the measure of length, or how far apart two points are away from each other.
 * k. Ground forms: The surface of the earth; the outer crust of the globe, or some indefinite portion of it.

5. Demonstrate how to shoot a magnetic azimuth.
The techniques employed to find the magnetic azimuth when using the lensatic compass are as follows:

Using the Centerhold Technique
First, open the compass to its fullest so that the cover forms a straightedge with the base. Move the lens (rear sight) to the rearmost position, allowing the dial to float freely. Next, place your thumb through the thumb loop, form a steady base with your third and fourth fingers, and extend your index finger along the side of the compass. Place the thumb of the other hand between the lens (rear sight) and the bezel ring; extend the index finger along the remaining side of the compass, and the remaining fingers around the fingers of the other hand. Pull your elbows firmly into your sides; this will place the compass between your chin and your belt. To measure an azimuth, simply turn your entire body toward the object, pointing the compass cover directly at the object. Once you are pointing at the object, look down and read the azimuth from beneath the fixed black index line. This preferred method offers the following advantages over the sighting technique:
 * 1) It is faster and easier to use.
 * 2) It can be used under all conditions of visibility.
 * 3) It can be used when navigating over any type of terrain.
 * 4) It can be used without putting down other gear; however, any other gear must be slung back out of the way.
 * 5) It can be used without removing eyeglasses.

Using the Compass-to-Cheek Technique
The compass-to-cheek technique is used almost exclusively for sighting, and it is the best technique for this purpose.

Fold the cover of the compass containing the sighting wire to a vertical position; then fold the rear sight slightly forward. Look through the rear-sight slot and align the front-sight hairline with the desired object in the distance. Then glance down at the dial through the eye lens to read the azimuth.

6. Demonstrate how to march on a magnetic azimuth.


Although different models of the lensatic compass vary somewhat in the details of their use, the principles are the same.


 * 1) Hold the compass level in the palm of the hand.
 * 2) Rotate it until the desired azimuth falls under the fixed black index line (for example, 320°), maintaining the azimuth as prescribed.
 * 3) Turn the bezel ring until the luminous line is aligned with the north-seeking arrow. Once the alignment is obtained, the compass is preset.
 * 4) To follow an azimuth, assume the centerhold technique and turn your body until the north-seeking arrow is aligned with the luminous line. Then proceed forward in the direction of the front cover's sighting wire, which is aligned with the fixed black index line that contains the desired azimuth.

Method #1
(These directions assume your orienting arrow lines up with the North indicator on your compass dial, meaning the compass has not been adjusted for declination).

A) Obtain the local magnetic declination for the area represented on your map. At the bottom of every USGS map is a diagram that displays the difference & direction between true north (represented as a star), grid north (abbreviated as “GN”), and magnetic north (abbreviated as “MN”).  Magnetic declination is the number of degrees and direction between true north and magnetic north.  Because declination varies over time, it is advisable to get a reasonably current figure.  If your USGS map is more than 15 years old (the declination date appears in the diagram), here’s an easy-to-use website that gives you only the information you need for your specific area:

http://geomag.nrcan.gc.ca/apps/mdcal-eng.php

If magnetic north is east of true north, the local declination is positive.

If magnetic north is west of true north, the local declination is negative.

B) Draw a line on the map that connects your starting point with the destination (your “map bearing”). Extend the line all the way through the map border (the “neat line”).

C) Distance yourself from any nearby metal such as keys, belt buckle, desk, car, fence, etc. Place the compass on the map so the needle’s pivot point is directly over the intersection of your map bearing and neat line.

D) Rotate the dial until compass ring north agrees with map north. Read your map bearing from the compass dial.  Make sure the bearing agrees with your direction of travel – for example, if you intend to travel due east, the bearing is 90 degrees, not 270 degrees.

E) Do this step mentally – don’t turn the compass dial. If the local declination is positive, then subtract the declination amount from the bearing you just derived.  If the local declination is negative, then add the declination amount to the bearing you just derived.

F) Turn the compass dial until the figure you calculated in step E lines up with the index line.

G) Lift the compass off the map, and with the direction of travel arrow pointing directly away from you, rotate your body and the compass all in one motion until the red magnetic needle overlays the orienting arrow.

H) Sight a landmark along this bearing, and proceed to it. Repeat this step until you reach your destination.

Method #2
(These directions assume your orienting arrow lines up with the North indicator on your compass dial, meaning the compass has not been adjusted for declination).

A) Obtain the local magnetic declination for the area represented on your map. At the bottom of every USGS map is a diagram that displays the difference & direction between true north (represented as a star), grid north (abbreviated as “GN”), and magnetic north (abbreviated as “MN”).  Magnetic declination is the number of degrees and direction between true north and magnetic north.  Because declination varies over time, it is advisable to get a reasonably current figure.  If your USGS map is more than 15 years old (the declination date appears in the diagram), here’s an easy-to-use website that gives you only the information you need:

http://geomag.nrcan.gc.ca/apps/mdcal-eng.php

If magnetic north is east of true north, the local declination is positive

If magnetic north is west of true north, the local declination is negative.

A) Draw a line on the map that connects your starting point with the destination (your “map bearing”).

B) Distance yourself from any nearby metal such as keys, belt buckle, desk, car, fence etc.

C) Place the compass on the map so the baseplate is parallel to the line you drew. Make sure the direction of travel arrow points to your destination.

D) Rotate the dial until compass ring north agrees with map north. Do not move the compass when you rotate the dial.

E) Remove the compass from the map and, with the direction of travel arrow pointing directly away from you, rotate your body and the compass all in one motion until the red magnetic needle overlays the orienting arrow.

F) If local declination is positive, then subtract the declination amount (turn the dial clockwise). If local declination is negative, then add the declination amount (turn the dial counter-clockwise).

G) Again, with the direction of travel arrow pointing directly away from you, rotate your body and compass all in one motion until the red magnetic needle overlays the orienting arrow. Sight a landmark along this direction of travel and proceed to it.  Repeat this step until you reach your destination.

Adjustable Declination Compasses
A compass with adjustable declination allows you to rotate the orienting arrow independently of the compass dial. If you have such a compass, you may calculate your map bearing without adding or subtracting the amount of local magnetic declination. To calibrate your compass in this fashion, rotate the inner liquid capsule (or turn the screw with the key) until the orienting arrow deviates from the compass ring’s north indicator by the amount & direction of the local magnetic declination. For example, if local declination is 10 degrees east of true north, rotate the inner liquid capsule (or turn the screw with the key) until the orienting arrow points to 10 degrees east. If using Method #1, you do not need to add or subtract as indicated in step E; just make sure compass ring north (not the orienting arrow) agrees with map north as directed in step D  If using Method #2, skip steps G and H; again, be sure compass ring north (not the orienting arrow) agrees with map north as directed in step E.

Magnetic Declination Varies Considerably Across The United States
The magnetic needle in a compass is attracted by the magnetism of the Earth, and therefore always points to the constantly shifting Magnetic North Pole. The Geographic North Pole is static and is located about 1200 miles north of the Magnetic Pole. Maps and directions are usually oriented toward the Geographic Pole, also referred to as "True North."

Magnetic declination is the direction and amount of variation between the Magnetic Pole and True North. The amount and direction of declination depends upon how those two poles align relative to a given point on Earth. When the two poles align, declination is zero, and the line of zero declination is termed the agonic line. At points west of the agonic line, a magnetic needle will point east of true north (positive declination). At points east of the agonic line, a magnetic needle will point west of true north (negative declination). There is a pattern, but it does not follow meridians or parallels. Isogonic lines are like magnetic contour lines -they trace a path of constant magnetic declination. 

8. Be able to orient yourself and a map by inspection and by compass.
Place the compass on the map so the baseplate parallels the north-to-south map neat line. Rotate the dial until compass ring North agrees with map North. Add or subtract the amount needed to adjust for local magnetic declination (subtract if local declination is positive, add if local declination is negative); if your adjustable declination compass is already calibrated for local declination, you don’t need to add or subtract, just make sure compass ring North (not the orienting arrow) agrees with map North. Holding the map and compass steadily (the baseplate should still be on the north-to-south map neat line), rotate the map and compass all in one motion until the red magnetic needle overlays the orienting arrow. Again, make sure there is no interference from metal when you perform this (ex: rebar in concrete). Your map and your compass are now oriented to true north. Compare the physical features around you with your map to help derive your location on the map..

9. Explain resection and its use.
Resection is a method of using a compass and a map to determine your current position. The first step is to find a feature of the landscape that you can also identify on the map. This could be a mountain peak, an intersection, a bridge, or even a utility pole (some topographic maps mark where high-voltage lines are, as well as the position of the poles that hold them up). The closer these two landmarks are to 90° offset from one another, the more accurate the resection will be. For instance, if the first landmark is at 115°, choose the second one as close to either 205° (115°+90°) or 25° (115°-90°) as you can. This is not a hard and fast rule, and the prominence of the landmark may well be more important than the 90° offset. Once you have shot an azimuth to the first landmark, calculate the back azimuth, and plot a line on your map from the landmark towards (and past) your current position (which should be somewhere on that line). Be sure to correct for declination when plotting this line. Then shoot the azimuth of the second landmark, and plot it's back azimuth on the map as well, again correcting for declination. If your readings are accurate and your plotting was done carefully, your current position should be very close to where these two lines intersect.