Beginner Geometry
Steps to develop practices, or skills and concepts, with minimal theory, or
very short chains of reason. That is, prerequisites for each practice
are minimal. Each practice may appear to be obvious to students, so that
minimal justification is needed after their introduction.
Steps or Topics
- Geometry and Formula Evaluation
- Geometry in or with maps,
plans and designs
- Length,
Areas and/Or Volume Scale Factors Backwards and Forwards
for Maps, Plans and Models in 2 and 3D
- Right Triangle Trigonometry
upto law of sines
- Rectangular and Polar
Coordinates with unsigned and then signed numbers -
- More Geometry
with maps - Navigation and Orienteering.
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Commentary.
Geometry began the art of measurement on land or in
the plane. That measurement can be done directly with surveying instruments,
tape measures and angle measuring devices included. Superposition of line
segments intersecting at interior and/or points allows a comparison of
angles and provides a basis for measurement of angles using protractors
in terms of degrees. Length and angle
measurement can be done indirectly with maps and plans drawn to scale.
When the scale is identical in all directions, drawn angles equal the
actual angles (real or intended) but actual (absolute) lengths are proportional.
The scale factor is or gives the proportionality constant for all
lengths. The scale factor gives the ratio of actual and drawn unit
length in reality and on the map or plan.
Working with With the use
of such unit lengths, if a distance or curve has length d real-world
unit (in actuality then it has length d drawn units. Thus relative measures of
distances and curves are identical while actual (absolute) measures differ. Likewise,
relative measures of areas are identical, even though actual (absolute) measures
differ. If
the proportionality constant for distances is K then the proportionality
constant for areas is K2. Maps and plans can be used to obtain the relative measures, and from
them, actual (or absolute) measures can be obtained and seen to be proportional. Maps
and plans are useful in navigation
over land or sea - draw your route on the map and then obtain lengths and
positions from the map instead of real-life measurements. Plans
are useful in design and construction of buildings clothes and circuits.
The fact that relative lengths and areas are preserved means that two
different diagrams or maps of the same planar figures, for instance by
two in a classroom, students and teacher included, will lead to the same
relative lengths and areas.
Like Shapes in Elementary School. In reading and writing letters and in seeing objects as they
exist or on paper, we recognize letters and objects which have the same shape
or nearly the same shape but different sizes. Size but not shape varies
as we move to or away from the letters or object. Size thus depends on
distance. The geometric theory of optics says or suggest
how.
Similarity theory in geometry says when two polygonal
figures have the same shape. Two planar polygonal figures (triangles) are similar when and
only when (i) corresponding angles are equal (have the same measure) and
(ii) corresponding sides are proportional. The latter codifies the notion of two
planar regions or curves in plane having the same shape, incompletely as
only polygonal curves and regions are considered, but that is good enough for
the further needs of high school mathematics. The further study of
trigonometry with right triangles is based on the similarity of triangles. Similarity theory
for right triangles would be sufficient for trigonometry with right
triangles..
Working With Maps and Plans. Planar triangles can be drawn and duplicated from
side and angle data, namely the lengths of three sides, from the lengths of
two sides and the measure of included angle, and from the measures of
two angles and the included length. Planar triangles can be drawn to
scale from side and angle data, namely the lengths of three sides, from
the lengths of two sides and the measure of included angle, and from the
measures of two angles and the included length. Drawing to scale gives a
similar triangle. Once the triangle is drawn and duplicated in full or to
scale, missing lengths and angles can be measured and thus found from
the drawing or image of a actual or intended triangle. The triangle of
interest may be in a horizontal, vertical or slanted plane
How to avoid or minimize the use of trig.
Right Triangles and Pythagorean Theorem:
If two sides of a right triangle are given then the length of the third
side, a hypotenuse or leg. is given by the direct or indirect use of the Pythagorean
identity.
Planar right- angle triangles can be also drawn and
duplicated from side and angle data with one or two simplification: (a) One of
the angles, namely the right angle is given; and (b) the sum of the angles is
180 degrees. Thus a right triangle can be drawn or duplicated as is or
to scale, given the length of one side and one acute angle, or given the
lengths of three sides. Then missing lengths and angles can be measured
or calculated. In the case of right triangles, missing lengths may also be
found (calculated) from the forward and backward use of the Pythagorean
identity appearing (where else?) in the Pythagorean theorem.
In surveying and navigation, and even in planning, there may
be sufficient data to draw a right or scalene triangle to scale in order to
find a length or missing angle. The triangle is drawn or selected
so that the missing length is a side or the missing angle is between two of it
sides. Then missing lengths and angles can be
measured or calculated indirectly using a drawing of a triangle.
Why do trig for Triangles
But obtaining measurement of missing lengths and
angles etc requires maps and plans to drawn with great
precision. Otherwise, drawing errors (distortions) will lead to
incorrect results. Exact calculations using similarity
properties or trigonometry provide an alternative, so sketches can be
used in place of exact maps and plans. Or, calculations with
trig for triangles may lessen the need for measurement on a map -
imagine a ruler or tape measure is not available.
Right Triangle Trigonometry: In a pair of
similar triangles, right or not, the corresponding sides are proportional
and hence each ratios of sides in one triangle equals the ratio of the
corresponding sides in the other. Both angles in a right triangle are
determined by giving one of the two acute angles in it. All right
triangles with the same acute angle A in them are similar. Whence
fractions given the ratio of sides (opp/adj, opp/hyp, adj/opp) in
each equals the ratio of corresponding sides in any other. Each faction
(a trig fraction or ratio) depends on the acute angle A. Each of the
foregoing fraction has a name: sine, cosine and tangent. Each side
occurs in two of the ratios. The value of the foregoing
fractions or ratios do not change if they are calculated using relative
or actual (absolute) measures of lengths.
There are now three ways to find missing lengths and a
right triangle, given one of its acute angles, say A, and a single side
(hypotenuse or not). The first method is draw a similar triangle
using the acute angle A, compute the ratios (opp/adj, opp/hyp, adj/opp)
of adjacent sides in the drawn triangle, and then use the equality of
these ratios to the ratios of the corresponding sides in the original
triangle. Then leads to three equations, two of which involve the given
side, and it is those two can be used to find the lengths of the missing
side. The second method is tabulate the value of the ratios (opp/adj, opp/hyp,
adj/opp) of adjacent sides in many drawn triangle, one for many angles A
between 0 and 90 degrees, then use the table exactly or via interpolation
to look up the values of the required ratios. Once the table is prepared,
there is no need to draw an second triangle, similar to original one, the
one whose missing sides are needed. A third method, calculator
methods give values of the fractions (opp/adj, opp/hyp, adj/opp) or
their reciprocals at the push of a few buttons. The calculator built-in
algorithms for this us arithmetic instead of diagrams to compute the
values of the fractions.
In trig, the concept or role of fractions and ratios is
enlarged. Before trig, fractions or ratios involve whole numbers as
ratio members or as fraction numerator and denominators. In trig, those
members, numerators and denominators involve real numbers (or real
numbers) as well as whole numbers. The fractions
(opp/adj, opp/hyp, adj/opp) may be proper ( less than 1), improper
(greater than one) or equal to 1.
Similarity of Arcs and Sectors of Circles:
Arcs and sectors of circles can be compared using their
central angles and the radius of the circles containing the arc.
Two arcs or sectors are isometric if their radii and central angles are
equal. Two arcs or sectors appear to be similar if their central
angles are equal. Direct Measurement as well as map drawing
implies corresponding lengths in similar arcs are proportional.
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The algebraic description of length and areas of triangles, squares,
rectangles, trapezoids, parallelograms, circles and fractions of circles
provides formulas for student to evaluate. Detail formatting rules
for the evaluation of geometric formulas, diagram drawing and labeling
included, show students how to show work - how to communicate the setting,
the steps in their reasoning and results in the evaluation of geometric formulas
in an observable and correctable manner on paper. That is a performance
objective easily understood and met..
The use or role of letters
or more generally symbols as placeholders in formulas and identifiers (labels)
on diagrams provides a starting point for algebraic ways of writing and
reasoning in general where letters or symbols or expression are placeholders
for numbers and quantities without an immediate geometric significance.
Examples:
- Give Formula Evaluation Exercises for areas of squares, rectangles,
triangles, parallelograms and circles with justification where possible of
all except for the formula for the area of the circle. That latter requires
calculus (or a numerical study of how the area of of circles is proportional
to the square of the radius).
- Give Formula Evaluation Exercises for perimeters of squares, rectangles,
circles and semicircles, triangles, parallelograms, regular polygons.
justification where possible of all except for the formula for the area of
the circle. The justification of the circle perimeter formula requires
calculus (or a numerical study of how the perimeter of a circle is
proportional to its radius).
Teachable Moment (painful): Recognition that multiplying by a half gives the
same result as dividing by a half is an example of the notion that different formulas when evaluated will
give the same result, or in brief the notion that two different expression may
be equal or have the same value. The idea for this come from a student
painful objection to my writing two formulas for the area of triangle- one using
the factor one half and the other using division by two. I was not being
consistent. Consistent use of one or the other formula might have avoided the
issue.
Maps, plans, designs and drawings made to scales less than, equal or greater
than 1 may be used for locating objects and for describing movements
along trails or paths, actual or intended.
- Maps: In maps drawn or redrawn, the image of a straight line segments and circular
arcs are also straight line segments and circular arcs. Whence the
images of figures made of straight line segments and circular arcs are also made
of straight line segments and circular arcs. Image element are seen to be
proportional to their pre-images in the original figures. All the
foregoing can be shown or implied by many examples, and then assumed as a drawing and
design shortcut or tool.
There is an innate ability to recognize like shapes, close-up
and far-way, within the level resolution capabilities of eyes - a level that
may vary. The ability to read and write letters, digits and further symbols,
and to recognize (read) and draw line segments, squares, circles and
semi-circles depends on that ability. The abiltiy to recognize shapes
and figures in pictures and diagrams also depends on this
ability. Primary students and teachers learning to read and write, and
learning geometry, may recognize like or similar shapes without any mention
of the formal characterization of similarity that appears say in secondary
school mathematics. Geometric optics suggest two figures, polygonal or not,
in different maps have the same shape if one is the projection or scale
drawing of the other - undistorted. Distortions would follow
from different scales on different axes. The secondary level discussion and
definition of similarity of polygons and circles in a single plane or
appearing on different maps characterizes and codifies similarity in terms
of corresponding angles being equal and corresponding lengths being
proportional formalizes or codifies that innate ability but not fully as the
geometric optics projection, perspective geometry and/or scale drawing
viewpoint. The equivalence of the latter to the primary
school identification of geometric figures and curves having like or same
shapes is incomplete as the formal discussion only involves polygonal
figures.
- Map Drawing or Construction: In drawing maps of physical
situations and objects or points there-in,, students may determine the image
of an object or map in the map by using physical measurements to determine
the location of the point relative the bottom-left corner of the map with
the aid of real-life unsigned rectangular and/or polar coordinates. For
example, students may be asked to draw or map to scale, their current
classroom and the location of key objects there-in - desk and chairs,
blackboards, doors, windows, etc. Line segments, squares and
rectangles, and part of circles, may be used to depict the latter objects on
the map. Desk should be drawn in proportion - so that aspect ratio of
their sides (top view) is maintained. Teachers could introduce four
objects with a triangular top view in the classroom and get students
to plot them in a room map or plan with the aid of (i) three vertex
coordinates, (ii) the coordinates of the end points of one side
(top view) and the use of the SSS, SAS and ASA physical measures to
draw the images of the objects (triangular top view) in the map.
Division of the room and map into corresponding grids may help.
- Why Measure or Calculate Distances and areas with Maps and Plans. Students
may measure the drawn, on-map distance between two points on a map using a
ruler or a tape measure, and then determine the pre-image points with by
multiplying by a scale factor (proportionality constant). Let
the unit length in the map be the image of an actual or real-life unit
length. Then map unit square is the image of the actual or real-life
unit square. Simple examples may imply that measure relative to the unit
lengths and areas are invariant - that is the same in the map and in
actuality. Whence lengths and areas of a figure or its map image can be
measured or calculated relative to unit length and area on the map or in
real life. The advantage of maps, plans and drawing in calculating
lengths and measures, and in route planning, appears when the actual or real
life actual (absolute) measures are not feasible. In other words, maps, drawing
and plans provide a means for the indirect measurement as relative lengths
and areas are invariant. Whence on-map (on drawing or on-plan) measurements
provide an alternative to real or actual measurements. For
surveying and navigation, information that is sufficient to draw a length or
figure to scale allows the missing dimensions and areas in the figure to be
determined from the drawing.
The foregoing may be done before the use of coordinates and then after.
See the introduction of coordinates below.
- Measuring lengths and areas with relative and actual (absolute)
measures: Suppose we take 1 meter to be the unit length for
measurement of distance. Then a curve or length with actual or actual (absolute)
length of 5 meters has a length of 5 relative to the unit length of
one meter. Further a region with actual or actual (absolute) area of 14 square
meters, that is, 14m2 has area 14 relative to the unit area of m2
or 1 square meter.
- Relative lengths are invariant: Suppose a line segment 8 m (8
meters) long is drawn on a map with a scale of 10 to 1. Then the drawing of
the line segment will be 8 dm (8 decimeters) long. The original unit
length, that is one meter, is gives or corresponds to a 1 decimeter
unit length. The original line segment and its image both have
relative length 8 with respect to the original unit length (1 meter) and the
unit length (1 dm) on the map. So relative lengths are
unchanged. Likewise, if a sequence of line segments forms a piecewise
linear path in the original plane, then the images of the sequence drawn on
the map forms the image path, piecewise linear too, in the map.
Both paths will have different actual (absolute) lengths, but identical lengths
relative to the unit length in the physical situation and in the map.
So again, relative lengths are invariant.
Finally and optionally, if the relative length of a curve in
a physical plane is the limit of the lengths of sequence of piecewise linear
approximation to it, the original curve, then the image curve in a map
will be the limit the lengths of sequence of corresponding piecewise linear
approximation to IT, the image curve, and vice-versa. Whence the image curve
and the original curve will have the same lengths. The piecewise
approximation can be taken with zero error (to be exact) on any portion of
the curve which is linear.
- Relative areas are invariant: Suppose a rectangle with
dimension 3 meters by 4 meters is drawn on a scale of 1 to 10 on a map. The
image is a rectangle of dimensions 3 dm by 4 dm. The actual (absolute)
or
actual area of the original square is 12 square meters or 12m2
while the area of the image is 12 square dm or 12 dm2.
Observe that the image of a the unit of area, that is a square meter, is the
unit of area, a square decimeter, in the map. Here we see the area 12
of the original rectangle relative to the original unit area equals the area
12 of the its image rectangle on the map with respect to the map unit area =
the image of the original unit area. So area of the rectangular region
and its image defined relative to the unit squares and its image is
the same. Likewise, the areas of square and their images relative to
the unit areas in the pre-image and image planes are equal. The key
word here is relative.
Finally and optionally, areas of regions in the original
plane can be approximate relative to the unit square in the original plane
by covering the region by small squares and finding the limit in relative or
actual (absolute) terms. Do the same in for the image of the region and using the
images of those small squares gives the same sequence of approximations for
the relative area of the image and hence, in the limit, the image region has
the same relative area as its pre-image - the original region.
Application to Note Taking: A teacher draws a parallelogram on
a board with height of 5 units and a base length of 4 units. Each note
taking student in the class draws a similar parallelogram with height 5
units and base 4 units, but the unit length used in all drawings of the
students and their one teacher are not the same. None the less, the students
and teacher all see that their version of the parallelogram, the original
and all its images, have a common area of 20 = 5 x 4 relative to their unit
of measure. In all calculations of area of a figures, figures whose
corresponding dimensions relative to a unit length in the diagram or map
containing the figure are identical, all have the same relative area.
Whence relative area calculation for a single figure - the original - may
done with a figure that is similar to it. We may same for composite figures
- figures that can be decomposed or split into smaller similar figures, so that the
sum of the areas, actual or relative, equals that of the original
composite. TASK: Say or rewrite the foregoing in a clearer
manner.
Extension: In a like manner, when 3 dimensional objects are designed
or mapped, relative lengths, relative surface areas and relative volumes are
invariant, that is, equal for each original object and any similar object that models it.
- Scale Factors K, K2 and K3 for actual (absolute)
Measures:
In mapping or modeling a 1, 2 or 3 D object or figure, the original
unit length corresponds to an image unit length = K times the original
unit length. We take that image unit length to the unit length for the map
or model, and thus for the calculation of unit area for 2D regions or
surfaces, and for the calculation of unit volume for 3D models of 3D
objects. Whence
image unit length = K * original unit length
image unit area = (K * original unit length)2
= K2 (original unit length)2 = K2 original
unit area
and
image unit volume = (K * original unit length)3
= K3 (original unit length)3 = K3 original
unit volume.
That is
image unit length = K * original unit length
image unit area = K2 original
unit area
and
image unit volume = K3 original
unit volume.
For corresponding lengths, surface areas and/or volumes, the relative
measures are equal by previous arguments. Whence
image actual (absolute) length = K * original length
or Limage = K Loriginal
image actual (absolute) area = K2 original actual (absolute)
area
or Aimage = K2 Aoriginal
and
image actual (absolute) volume = K3 original
actual (absolute) volume or Vimage = K3 Voriginal
Remark 1: The numbers are scale factors or
proportionality constants for length, area and volume respectively. When one
is calculated or obtainable, then so are the others via arithmetic
operations of squaring, cubing, taking square roots and/or taking cube
roots. Moreover, if the ratio of a pair of image and original lengths,
areas or volumes is known, then one of the scale factors K, K2 and K3
and hence all may be calculated. See site discussion of forwards and
backwards use of formulas and proportionality relations to learn more.
Remark 2: Memorization of squares and cube roots of 1, 2, 3, 4
and 5 may help in the backward calculation of the scale factors in exercises
that develop or encourage forward, backwards and sideways use of the
proportionality between lengths, areas and volumes in maps and models, and
in real life.
Remark 3: The proportionality factors K, K2 and K3
also apply to quantities that are proportional to length, area and volume in
the building of models to part, full or oversized scale. Exercise: Explain
why.
Remark 4: Say the scale of a map or plan is 1 to 10000 then 1
cm on the map corresponds to 100 meters =10000 cm on the map. Now let d =
distance measured on the map = n cm. Let D = the corresponding distance in
practice (actuality) measure in meters. Then we expect 1 to 10000 = d
to D or 10000 to 1 = D to d. So 10000 = D/d or 10000 d = D. Now
d = n cm gives D = 10000 (n cm) = 100 x n 100 cm = n 100 meters. Thus
the "unit distance" 1 cm on the map corresponds to the unit
distance of 100 meters in actuality.
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Similarity by Design: If two artificial bodies S and S' appear to
have the same shape, then it likely but not guaranteed that there is a
common plan
Preparation for Trig and Alternative to Trig: Suppose S is a 2D or 3D figure
that is similar to another figure S'. Then similarity or proportionality implies the ratio
of any two sides, areas or volumes in the figure equals the ratio of the
corresponding sides, areas or volumes in any similar figure S'. If
one aspect of figure S is too large to measure, the construction of a
similar figure may make that aspect measurable with the aid of a
proportionality constant.
A Message to Repeat in Class: All trig formulas may be used forwards
and backwards alone or in combination with other trig formulas and the
Pythagorean theorem to find missing angles and sides in triangles that are
alone, adjacent to further triangles, or implicit in a diagram.
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For angles q between 0 and 90
degrees, similarity of right triangles implies the trig fractions

are independent of the choice of right triangles used to compute
them. if you replace the unit circle right triangle by a similar
right triangle. The latter formulas for may be used to
compute
with any right triangle where sides are labeled opposite and adjacent
for an angle q The
further trig functions may be defined as follows.


when the divisors are nonzero. Exercise: Express these further
trig functions as ratios of the sides opposite, adjacent and/or
hypotenuse of the above right triangle.
Trig functions link the ratio of two sides of a
right triangle to cosines, sines and tangents of an angle. Knowledge
of two sides in right triangle gives knowledge of the third by means
of Pythagorean theorem, and of the values of the trig functions for
the angles in the triangle. Computation of unknown side lengths,
unknown hypotenuse lengths and unknown angles is useful in land
measurement (geo - metry) and also in navigation.
From one-to-one properties of trig functions for
angles between 0 and 90 degrees or ½p, one
can define (say how to compute) inverse trig functions (more
functions on your calculator) to compute the angles from the
ratio of sides.
The forward use of the above formula calculates trig functions for an
acute angle q from the lengths of sides
(legs) of right triangles. A backward use of one of these formulas would
determine the length of a leg from the value of or a trig and the
length of a side. Another backward use would be to find the angle
given the value of one of the trig functions directly, or through the
calculation of trig fraction.

Trig functions link the ratio of two sides of a right
triangle to cosines, sines and tangents of an angle. Knowledge of two sides in
right triangle gives knowledge of the third by means of Pythagorean theorem,
and of the values of the trig functions for the angles in the triangle.
Computation of unknown side lengths, unknown hypotenuse lengths and unknown
angles is useful in land measurement (geo - metry) and also in navigation.
From one-to-one properties of trig functions for angles
between 0 and 90 degrees or ½p, one can define
(say how to compute) inverse trig functions (more functions on
your calculator) to compute the angles from the ratio of sides.
The forward use of the above formula calculates trig functions for an acute
angle q from the lengths of sides (legs) of
right triangles. A backward use of one of these formulas would determine the
length of a leg from the value of or a trig and the length of a
side. Another backward use would be to find the angle given the value of
one of the trig functions directly, or through the calculation of trig
fraction.
Remark: The cosine law can be left to after a discussion of the unit
circle definition or redefinition of trig functions to obtain values for trig
functions for angles that are not acute.
Calculation
One may define trig functions by saying how to compute them in principle as
above, but then one computes or approximates them in practice from tables and
slide rules (old fashioned approach) or using calculators (the new approach).
Unfortunately in this practice, the tables, slide rules or calculation
devices are black boxes which provide results, but whose derivation or
justification is not commonly known. This departs from the principle of
understanding the computations one does, but the numbers computed by these
black boxes can be checked in simple cases involving 30-60-90 right angles
(obtained by bisecting angle in an equilateral triangle) and involving
45-45-90 degree triangles obtained by SAS construction using two sides of
equal length, and taking 90 degrees to be the included angle.
Remark: Understanding how to do exact arithmetic with whole
numbers and square roots to represent the sines and cosines of 30, 45
and 60 degrees using 30-60-90 and 45-45-90 right triangles is must do in the
high school preparation for calculus.
Background Information: Solving Triangles Using Similarity or Trig Functions: Show
how right triangle trig provides an alternative to similarity analysis in
solving triangles. Given a large right triangle with determined (explain
why) by SAS with the aid acute angle A and the measure of one its sides
(opposite, adjacent or hypotenuse), a triangle with sides that cannot
be measured directly, we can find the lengths of the remaining sides by (i)
drawing a similar right triangle and measuring (similarity implies the
ratio of any two sides in a figure equals the ratio of the corresponding
sides in any similar figure) or (ii) using tabulated or electronic
calculator given values of right triangle trigonometry functions cos(A), sin
(A) or tan(A) found without immediately drawing a similar right triangle,
but found in principle from drawing many right triangles and tabulating the
results. In other words, the use of trig functions hides or buries the
use of similarity in solving right triangles with missing lengths in the
earlier link of trig functions values for acute angles to the
ratios of adjacent sides of right triangles.
The SAS triangle area formula

The foregoing suggests the following SAS method for calculating the area of
a triangle given two sides d and D and the included acute angle q
between them.
Area S = ½ (length of side)(length of another side) sin (included
angle)
Call the latter the SAS triangle area formula.
Extension to the Obtuse Angle Case

Here sin q = h/a and hence h =
a sin q .
Therefore
Triangle Area S = ½ c h = ½ c a sin q
Now put sin b = sin q
= sin (180o - b)
when b is between 90 and 180 degrees.
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Commentary.
Similarity theory in geometry says when two polygonal
figures have the same shape. Two planar polygonal figures (triangles) are similar when and
only when (i) corresponding angles are equal (have the same measure) and
(ii) corresponding sides are proportional. The latter codifies the notion of two
planar regions or curves in plane having the same shape, incompletely as
only polygonal curves and regions are considered, but that is good enough for
the further needs of high school mathematics. The further study of
trigonometry with right triangles is based on the similarity of triangles. Similarity theory
for right triangles would be sufficient for trigonometry with right
triangles..
Working With Maps and Plans. Planar triangles can be drawn and duplicated from
side and angle data, namely the lengths of three sides, from the lengths of
two sides and the measure of included angle, and from the measures of
two angles and the included length. Planar triangles can be drawn to
scale from side and angle data, namely the lengths of three sides, from
the lengths of two sides and the measure of included angle, and from the
measures of two angles and the included length. Drawing to scale gives a
similar triangle. Once the triangle is drawn and duplicated in full or to
scale, missing lengths and angles can be measured and thus found from
the drawing or image of a actual or intended triangle. The triangle of
interest may be in a horizontal, vertical or slanted plane
How to avoid or minimize the use of trig.
Right Triangles and Pythagorean Theorem:
If two sides of a right triangle are given then the length of the third
side, a hypotenuse or leg. is given by the direct or indirect use of the Pythagorean
identity.
Planar right- angle triangles can be also drawn and
duplicated from side and angle data with one or two simplification: (a) One of
the angles, namely the right angle is given; and (b) the sum of the angles is
180 degrees. Thus a right triangle can be drawn or duplicated as is or
to scale, given the length of one side and one acute angle, or given the
lengths of three sides. Then missing lengths and angles can be measured
or calculated. In the case of right triangles, missing lengths may also be
found (calculated) from the forward and backward use of the Pythagorean
identity appearing (where else?) in the Pythagorean theorem.
In surveying and navigation, and even in planning, there may
be sufficient data to draw a right or scalene triangle to scale in order to
find a length or missing angle. The triangle is drawn or selected
so that the missing length is a side or the missing angle is between two of it
sides. Then missing lengths and angles can be
measured or calculated indirectly using a drawing of a triangle.
Why do trig for Triangles
But obtaining measurement of missing lengths and
angles etc requires maps and plans to drawn with great
precision. Otherwise, drawing errors (distortions) will lead to
incorrect results. Exact calculations using similarity
properties or trigonometry provide an alternative, so sketches can be
used in place of exact maps and plans. Or, calculations with
trig for triangles may lessen the need for measurement on a map -
imagine a ruler or tape measure is not available.
Right Triangle Trigonometry: In a pair of
similar triangles, right or not, the corresponding sides are proportional
and hence each ratios of sides in one triangle equals the ratio of the
corresponding sides in the other. Both angles in a right triangle are
determined by giving one of the two acute angles in it. All right
triangles with the same acute angle A in them are similar. Whence
fractions given the ratio of sides (opp/adj, opp/hyp, adj/opp) in
each equals the ratio of corresponding sides in any other. Each faction
(a trig fraction or ratio) depends on the acute angle A. Each of the
foregoing fraction has a name: sine, cosine and tangent. Each side
occurs in two of the ratios. The value of the foregoing
fractions or ratios do not change if they are calculated using relative
or actual (absolute) measures of lengths.
There are now three ways to find missing lengths and a
right triangle, given one of its acute angles, say A, and a single side
(hypotenuse or not). The first method is draw a similar triangle
using the acute angle A, compute the ratios (opp/adj, opp/hyp, adj/opp)
of adjacent sides in the drawn triangle, and then use the equality of
these ratios to the ratios of the corresponding sides in the original
triangle. Then leads to three equations, two of which involve the given
side, and it is those two can be used to find the lengths of the missing
side. The second method is tabulate the value of the ratios (opp/adj, opp/hyp,
adj/opp) of adjacent sides in many drawn triangle, one for many angles A
between 0 and 90 degrees, then use the table exactly or via interpolation
to look up the values of the required ratios. Once the table is prepared,
there is no need to draw an second triangle, similar to original one, the
one whose missing sides are needed. A third method, calculator
methods give values of the fractions (opp/adj, opp/hyp, adj/opp) or
their reciprocals at the push of a few buttons. The calculator built-in
algorithms for this us arithmetic instead of diagrams to compute the
values of the fractions.
In trig, the concept or role of fractions and ratios is
enlarged. Before trig, fractions or ratios involve whole numbers as
ratio members or as fraction numerator and denominators. In trig, those
members, numerators and denominators involve real numbers (or real
numbers) as well as whole numbers. The fractions
(opp/adj, opp/hyp, adj/opp) may be proper ( less than 1), improper
(greater than one) or equal to 1.
Similarity of Arcs and Sectors of Circles:
Arcs and sectors of circles can be compared using their
central angles and the radius of the circles containing the arc.
Two arcs or sectors are isometric if their radii and central angles are
equal. Two arcs or sectors appear to be similar if their central
angles are equal. Direct Measurement as well as map drawing
implies corresponding lengths in similar arcs are proportional.
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The latter implies
Triangle Area S = ½ c h = ½ c a sin b
By putting sin b = sin q
= sin (180o - b) when b is between 90 and 180 degrees., the
previous formula triangle area = The latter half the product of two
sides times the sine of the included angle. is extended to the
case where the included angle is obtuse.
Note: A triangle is half a kite or parallelogram. So the foregoing also implies
SAS formulas for the areas of kites and parallelograms which can be developed
in class notes or in exercises.
Derivation of The sine law:

From the SAS triangle area formula, the area of triangle ABC
is given by S = ½ ac sin B where B in an overuse of the symbol
B, denotes the angle at vertex B. In general, there are three formulas
- S = ½ bc sin A
- S = ½ ac sin B
- S = ½ ab sin C
Equality of the first two formulas ½ bc sin A = ½ ac sin B
gives bc sin A = ac sin B and hence
b sin A = a sin B. The latter in turn (divide both
sides by ab) gives
Equality of the last formulas ½ ac sin B = ½ ab sin C
likewise gives
Likewise equality of the first and last formulas give
Now instead of writting (I), (II) and (III) separately, we write the
simultaneous equalities
sin A
a |
= |
sin B
b |
= |
sin C
c |
The latter expression is called the sine law, and its a brief form of
stating (I), (II) and (III).
Remark: Formula (I) involves four quantities, namely two lengths and
two angles. The backward use of (I) as is, or rewritten as an equality
of reciprocals, which ever is most convenient, means that whenever three of
the four quantities is given, the fourth can be found. Formulas (II) and
(III) likewise involve four quantities. They too can be used in a
backward manner.
Sine Law Application Ideas: Use the unit circle introduction of trig
functions and reflection about vertical axis to show that sin(180 - A) = sin
(A) for acute and obtuse angles A. Next prove the sine law for triangles,
scalene or not. Interpret the sine law in the case of right triangles
and imply it works, with some overlap or redundancy [to do: redundancy
to be spelled out.] Next apply the sine law forwards, backwards and
side ways to solve right triangles. Point out the option of drawing
similar triangles and measuring in each way the law is used.
Preparing for the Use of Coordinates and Arrows (to Represent Displacements) on Maps and Plans
Easily Covered Background Information.
The introduction of rectangular and polar coordinates may be done here, in
the development of algebra or with the further discussion of advanced geometry
- Rectangular Coordinates for Maps with unsigned numbers:
Ordered Pairs [a,b] of Mixed numbers, proper and improper fractions and
decimals with square brackets may be introduced as coordinates to locate
points on rectangular maps when the origin of this unsigned coordinate
system is place at say the bottom-left corner of each map. The introduction
of coordinates is based on the introduction of unit lengths - keep it the
same for horizontal and vertical directions - and based on the introduction
of a square grid covering the map. Each square in the grid can itself by
covered by a grid of smaller squares, and so on, ad infinitum.
Note: the foregoing coordinates [a, b] are relative to the
choice of unit length. actual (absolute) coordinates would use
coordinates of the form [A, B] = [a units, b units] with ordered pairs of
mixed number multiples of units (quantities).
- Rectangular Coordinates for maps with Signs:
Ordered Pairs [a,b] of Mixed numbers, proper and improper fractions and
decimals with plus and minus signs as prefixes may be introduced as
coordinates to locate points on rectangular maps when the origin of this
unsigned coordinate system is not placed at the bottom-left corner of each
map. As before, the introduction of coordinates is based on the introduction
of unit lengths - keep it the same for horizontal and vertical directions -
and based on the introduction of a grid of unit squares covering the map.
Each square in the grid can itself by covered by a grid of smaller squares,
and so on, ad infinitum. The boundaries of the map need not be aligned
with grid elements. Make sure that students are aware that the coordinates
of a point are relative to the length of unit vectors.
- Polar Coordinates with unsigned numbers: Ordered Pairs (r,
q) of Mixed numbers, proper and improper fractions and decimals with
round brackets may be introduced as coordinates to locate points P on
rectangular maps when the origin of this unsigned coordinate system is place
at say the bottom-left corner of each map. The introduction of coordinates
is based on the introduction of unit lengths - keep it the same for
horizontal and vertical directions. Here r = the distance of the point
P from the origin while q = angle of the ray from the origin to the point P.
The angle would be between 0 and 90 degrees for points in the first
quadrant, and between 90 and 360 degrees for points in other quadrants.
Note: the foregoing coordinates (r, q) are partially relative
to the choice of unit length for distance and actual (absolute) for degree
measure. actual (absolute) coordinates would use polar
coordinates of the form (R, q) = (r units, q ) with R being the actual
(absolute) quantity r units, and q (still) being the actual (absolute)
degree measure of angle.
Note: The angle q of a point is determined modulo 360 degrees.
One might speak of the angle, modulo 360 degrees, for the sake of having a
"unique angle". That angle might be identified with a point
on a unit circle.
Remark for Items 1, 2 and 3 above: It can be implied or suggested in Euclidean
Geometry that rectangular coordinates [a,b] of point in a rectangular region
of the plane which includes the origin [0,0] uniquely
determine a right triangle with one leg on the horizontal axis and a
hypotenuse given by the straight line segment between the origin [0,0] and
point [a,b]. Then the length of the hypotenuse gives R = r units while the
standard angle it makes with the horizontal axis gives angle q.
Conversely, the polar coordinates of a point determines the legs of a right
triangle with one leg on the horizontal axis. The lengths of those
legs and the identification of the quadrant in which point lies determines
the points rectangular coordinates [a,b].
- Map Mastery Exercises: Student mastery of rectangular and
polar coordinates may be developed and verified by exercises which
require them to locate and plot individual points (dots) from point
coordinates. Student comprehension of rectangular coordinates may be
further developed and verified by exercises which require students to join
the points or dots that form the figure of a person, object cute animal or
form a trail or path in the map with some amusing significance - path out of
a maze, path between two cities following a road network, path to
buried treasure, etc, etc - where the etc, etc means I have run out of
imagination. The introduction of coordinates is based on the introduction of
unit lengths - keep it the same for horizontal and vertical
directions.
- Map Usage: From measurement and scaling of map coordinates,
students may find the physical location of a point, or its image on another
map. Maps may also be used to draw and plan routes. From
measurement and scaling of map lengths with rulers, threads and measuring
wheels (official name?), students may obtain the physical length of
routes. Bearing (angles) of a distance object and the endpoints of the
line segment joining two bearings would allow students to locate on the map
the distant object using the ASA method. The foregoing may be combined with
more map mastery exercises.
Running Out of Steam: When this site author is sufficiently
energized, the following will be reconsidered.
Question: Running out of Steam refers to what means of
locomotion?
- Arrows and Navigation: Actual or potential path (trips, voyages,
routes) may shown on maps by curves - smooth or piecewise linear. The net
result of a trip is a movement or displacement from the initial point
(origin of the path) to the terminal point that can represented (drawn) as
an arrow or vector with tail at the initial point and head at the terminal
point. Paths that involve a sequence of net movements from one point to a
next can be represent by piecewise linear curves in which linear part, an
actual or net linear displacement, is represented by an arrow.
The observation of a first displacement and then a second displacement and
then a third displacement, etc, leads to the adding of displacements or
arrows or vectors in a head to tail manner. Diagrams imply that
addition is clearly associative.
Technical Remark:
The Head to Tail Addition of a sequence of displacements (arrows), where subsequences
are replaced by a net result (resultant vector) is associative.
[insert picture to demonstrate] Moreover, adjacent element of the sequence
(subsequences) can be grouped and replaced by a single resultant arrow, all
without changing the net displacement from the initial point of the route to
the terminal point of the route.
- Orienteering: Walking through parks and bush with the aid of
maps and compass may introduce veering-off strategy of aiming for one side of
a desired destination instead of heading directly for it. For example
if the destination is on a stream and there is some uncertainty or
impossibility of heading directly for that destination, the orienteer would
set a course or direction that guarantees hitting the stream above (or
below) the destination, and then plan to walk downstream (respectively
upstream) to the desired destination. The alternative might lead the
orienteer to the stream without being certain of being upstream or
downstream of the target location.
- Plans and Maps in Design and Navigation: Students may be
shown how to solve geometric design and navigation problems by drawing
objects and paths to scale and then measuring lengths on the drawing to
compute actual lengths and from them compute areas, and other quantities
proportional to length and area. Here is a context for the introduction and
study of similarity since corresponding Angles are preserved and
corresponding lengths are proportional in the drawing, design and use
of shapes and routes on maps and plans. The study of similarity
may focus on the use of scale drawing to draw conclusion about real or
imagine world situations and applications with the aid of geometric formulas
and real or on-map measurements. Applications may appear in interior design
- the painting and design of rooms in homes and offices, and the calculation
of quantities based on length, area and even volume. Application may also
appear in surveying - determining heights of building from angle
measurements and horizontal distances. Application may also appear in
navigation - route planning for vehicles on land, on water, or over and
under land and water. The common theme may drawing to scale on map or
plans, and then rescaling map measurements to get or estimate real world
measures.
- Navigation and Movements with arrows and vectors on Maps.
The planning of routes at sea and in the air may involve straight line
segments with an initial and terminal point. Each segment may be
depicted by an arrow or vector with a tail starting at the initial point and
a head ending at the terminal point. A piecewise linear route (top view) in
the plane may be represented by a sequence of arrows, with the tail of the
first arrow at the initial point of the route, and the tail at each further
arrow at the head of is predecessor. Each arrow represents a displacement from its initial point or tail to its terminal point or
head. The arrow points in the direction of movement. So an arrow in
depicting a displacement has a length (magnitude) and direction. The arrow
also has an initial position (the tip of its tail) and a terminal position -
the tip of its head. The head to tail placement of arrows represent a pair or
sequence of displacements, a route in which the end of one displacement is
the start of the next. The net displacement of a such a sequence is the
arrow from the initial point of the route to the terminal
point. That arrow represents the net displacement of two to several
displacements. In particular, the net
result (sum or resultant) of two adjacent arrows or displacements in the
route may be represented by a third arrow or displacement that starts at the
initial point of the first arrow and ends at the terminal point of the
second arrow.
A sequence of movements (displacements) plotted as arrows may
give or approximate an actual or planned route. The map location of heads
and tails may correspond to points on the route where bearing were taken to
determine location on the map, or those map location may represent the
intended location. Maps and charts may show the intended and actual
route of a vessel or vehicle across the sea or land.
Remark on Parallelism: On maps and plans, the practice of
indicating
true North or Magnetic North provides a reference for describing the
direction of line segments and movement. Two movement are declared to be
parallel if they make the same bearing or angle with respect to true North
or magnetic North. Parallel movements are thus indicated by compass
readings. Implicit here is theorem that could be stated and shown in
particular cases, if not in general, in
Euclidean Geometry: Namely, if at two distinct points are
located on parallel lines, and rays issuing from the points make congruent
angles with the parallel lines, then the two rays and lines extending them
are parallel. Likewise, the practice of covering maps and plans with
grid also provides a reference for describing the
direction of line segments and movement. How these practices are possible
might be a subject of discussion in Euclidean Geometry - the applied math view
of it.
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