
Chapter 8 -
... When you borrow money a fee is charged ( an interest ). When we calculate the interest with I = Prt, we call it a simple interest. There are other ways to calculate an interest. Need : M = P + I, M is the maturity value, P = principal, I = interest ...
... When you borrow money a fee is charged ( an interest ). When we calculate the interest with I = Prt, we call it a simple interest. There are other ways to calculate an interest. Need : M = P + I, M is the maturity value, P = principal, I = interest ...
Geometry Fall 2011 Lesson 17 (S.A.S. Postulate)
... Definition: Two polygons are similar if their vertices can be paired so that 1) Corresponding angles are congruent 2) Corresponding sides are in proportion The symbol for similarity is ~. What is the ratio of the lengths of any two corresponding sides in the similar polygons at right? Definition: Th ...
... Definition: Two polygons are similar if their vertices can be paired so that 1) Corresponding angles are congruent 2) Corresponding sides are in proportion The symbol for similarity is ~. What is the ratio of the lengths of any two corresponding sides in the similar polygons at right? Definition: Th ...
We are dismissed early if there is a teacher`s meeting
... Two-column proof: proof with numbered statements and reasons that show the logical order of an argument. Properties of Segment Congruence Reflexive: For any segment AB, AB = AB. Symmetric: If AB = CD, then CD = AB. Transitive: If AB = CD and CD = EF, then AB = EF. ...
... Two-column proof: proof with numbered statements and reasons that show the logical order of an argument. Properties of Segment Congruence Reflexive: For any segment AB, AB = AB. Symmetric: If AB = CD, then CD = AB. Transitive: If AB = CD and CD = EF, then AB = EF. ...
Illustrative Mathematics 8.G, G-GPE, G-SRT, G
... theorem and its converse. Also at the eighth grade level, rigid motions of the plane can be applied to the quadrilateral so that its angles are shown to be congruent to angles made by horizontal and vertical grid lines. At the high school level, one way to show that an angle is a right angle is to m ...
... theorem and its converse. Also at the eighth grade level, rigid motions of the plane can be applied to the quadrilateral so that its angles are shown to be congruent to angles made by horizontal and vertical grid lines. At the high school level, one way to show that an angle is a right angle is to m ...
12-1 Define and Use Sequences and Series
... *Angles in Standard Position In a coordinate plane, an angle can be formed by fixing one ray, called the initial side, and rotating the other ray, called the terminal side, about the vertex. An angle is in standard position if its vertex is at origin and its initial side lies on the positive x-axis. ...
... *Angles in Standard Position In a coordinate plane, an angle can be formed by fixing one ray, called the initial side, and rotating the other ray, called the terminal side, about the vertex. An angle is in standard position if its vertex is at origin and its initial side lies on the positive x-axis. ...
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.