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Key

1-4
1-4

Basic Rigid Motions
Basic Rigid Motions

... Parallel lines in the pre-image remain parallel lines in the image. The parallel lines have the same slope. The location of the pre-image is changed to produce the image through a coordinate rule. Congruent figures are produced in a different location in the plane. The motion begins with a pre-image ...
Chapter 2 Notes - Moore Public Schools
Chapter 2 Notes - Moore Public Schools

Geometry: 1-1 Day 1 Points, Lines and Planes
Geometry: 1-1 Day 1 Points, Lines and Planes

Prove Triangles Congruent by ASA & AAS
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... then the two triangles are congruent AAS Congruence Theorem: If two angles and a non-included side of one triangle are congruent to two angles and the corresponding nonincluded side of a second triangle, then the two triangles are congruent. ...
4.3 Isosceles and Equilateral Triangles
4.3 Isosceles and Equilateral Triangles

... Rock Climbing In one type of rock climbing, climbers tie themselves to a rope that is supported by anchors. The diagram shows a red and a blue anchor in a horizontal slit in a rock face. ROCK CLIMBING The ...
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Mixed Review

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... To find the value of the trig functions of angles that do NOT reference 30°, 45°, or 60°, and are not quadrantal, we will use the calculator. Round your answer to 4 decimal places, if ...
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Old CA citation

Generalization - WordPress.com
Generalization - WordPress.com

defintions and theorems 1 - The Bronx High School of Science
defintions and theorems 1 - The Bronx High School of Science

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Packet 2 for Unit 2 M2 Geo

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Geometry Review Packet for

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GRADE 7 MATHEMATICS

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Plane Geometry Notes Lines and angles Quadrilaterals and

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MATH 301 Survey of Geometries Homework Problems – Week 5

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Angle Chasing - Andrew.cmu.edu

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File - SouthEast Ohio Math Teachers` Circle SEOMTC

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8 th Ch 9 Practice Quiz

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Counter Examples To show that a statement is false it is enough to

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Mathematics Pacing

... Verify experimentally the properties of dilations given by a center and a scale factor: a) A dilation takes a line not passing through the center of the dilation to a parallel line, and leaves a line passing through the center unchanged. b) The dilation of a line segment is longer or shorter in the ...
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Euler angles



The Euler angles are three angles introduced by Leonhard Euler to describe the orientation of a rigid body. To describe such an orientation in 3-dimensional Euclidean space three parameters are required. They can be given in several ways, Euler angles being one of them; see charts on SO(3) for others. Euler angles are also used to describe the orientation of a frame of reference (typically, a coordinate system or basis) relative to another. They are typically denoted as α, β, γ, or φ, θ, ψ.Euler angles represent a sequence of three elemental rotations, i.e. rotations about the axes of a coordinate system. For instance, a first rotation about z by an angle α, a second rotation about x by an angle β, and a last rotation again about z, by an angle γ. These rotations start from a known standard orientation. In physics, this standard initial orientation is typically represented by a motionless (fixed, global, or world) coordinate system; in linear algebra, by a standard basis.Any orientation can be achieved by composing three elemental rotations. The elemental rotations can either occur about the axes of the fixed coordinate system (extrinsic rotations) or about the axes of a rotating coordinate system, which is initially aligned with the fixed one, and modifies its orientation after each elemental rotation (intrinsic rotations). The rotating coordinate system may be imagined to be rigidly attached to a rigid body. In this case, it is sometimes called a local coordinate system. Without considering the possibility of using two different conventions for the definition of the rotation axes (intrinsic or extrinsic), there exist twelve possible sequences of rotation axes, divided in two groups: Proper Euler angles (z-x-z, x-y-x, y-z-y, z-y-z, x-z-x, y-x-y) Tait–Bryan angles (x-y-z, y-z-x, z-x-y, x-z-y, z-y-x, y-x-z). Tait–Bryan angles are also called Cardan angles; nautical angles; heading, elevation, and bank; or yaw, pitch, and roll. Sometimes, both kinds of sequences are called ""Euler angles"". In that case, the sequences of the first group are called proper or classic Euler angles.
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