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Rigid motions in  
\[\mathbb{R}^n\]
  are mappings that preserve distances, and by implication, areas and volumes. If  
\[f\]
  is a rigid motion on  
\[\mathbb{R}^n\]
  then for any  
\[\mathbf{x}, \; \mathbf{y} \in \mathbb{R}^n\]
,  
\[\left| f\mathbf{y} - \mathbf{x} \right| = \left| y-x \right|\]
.
Any rigid motion in  
\[\mathbb{R}^n\]
  is an orthogonal mapping, that preserves angles and lengths, and a translation.
Relative to an orthonormal basis, the matrix of any orthogonal mappings of  
\[\mathbb{R}^2\]
  has one of the forms  
\[A= \left( \begin{array}{cc} cos \theta & - sin \theta \\ sin \theta & cos \theta \end{array} \right), \; B= \left( \begin{array}{cc} cos \theta & sin \theta \\ sin \theta & -cos \theta \end{array} \right) \]

Matrix  
\[A\]
  represents rotation anticlockwise by an angle  
\[\theta\]
  and matrix  
\[B\]
  represents reflection in the line making an anticlockwise angle  
\[\frac{\theta}{2}\]
  with the positive  
\[x\]
  axis.
Rotation about an arbitrary point  
\[Q\]
  can be represented as a translation  
\[\mathbf{QO}\]
  followed by the rotation followed by the translation  
\[\mathbf{OQ}\]
. We can write this as  
\[F(P)=A(P-Q)+Q\]
.
Reflection in an arbitrary line  
\[\mathbf{r}=\mathbf{OQ} + t \mathbf{v}\]
  can be represented as a translation  
\[\mathbf{QO}\]
  followed by the rotation followed by the translation  
\[\mathbf{OQ}\]
. We can write this as  
\[F(P)=A(P-Q)+OQ\]
.
Glide reflection along an arbitrary line  
\[\mathbf{r}=\mathbf{OQ} + t \mathbf{v}\]
  can be represented as a reflection in the line followed by a translation  
\[k \mathbf{v}\]
. We can write  
\[F(P)=BP+ k \mathbf{v}\]
.