We consider the matrices \begin{equation*}A=\begin{pmatrix}\cos \phi & -\sin \phi \\ \sin \phi & \cos \phi \end{pmatrix}, B:=\begin{pmatrix}2 & 0 \\ 1 & 1\end{pmatrix} , \ \ \ S:=\begin{pmatrix}0 & -1 \\ 1 & 0\end{pmatrix}\end{equation*}
I want to give the geometric interpretation of the maps $\vec{x}\mapsto B\cdot \vec{x}$, $\vec{x}\mapsto S\cdot \vec{x}$, $\vec{x}\mapsto A^{-1}\cdot \vec{x}$ and $\vec{x}\mapsto B^{-1}\cdot \vec{x}$.
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Let's consider the map $\vec{x}\mapsto B\cdot \vec{x}$.
We have that: \begin{equation*}B\cdot \vec{x}=\begin{pmatrix}2 & 0 \\ 1 & 1\end{pmatrix}\begin{pmatrix}x_1 \\ x_2\end{pmatrix}=\begin{pmatrix}2x_1 \\ x_1+x_2\end{pmatrix}\end{equation*}
Now we consider the map $\vec{x}\mapsto S\cdot \vec{x}$.
We have that: \begin{equation*}S\cdot \vec{x}=\begin{pmatrix}0 & -1 \\ 1 & 0\end{pmatrix}\begin{pmatrix}x_1 \\ x_2\end{pmatrix}=\begin{pmatrix}-x_2 \\ x_1\end{pmatrix}\end{equation*}
To give the geometeic interprtation do we have to check the image of the unit square under these maps?


For the first example stated in simplest terms
$$ (x,\quad y)\rightarrow ( 2x, \quad x+y ) $$ is a transformation function just like geometrical form changes like reflection, magnification, sliding, shear etc.
Applying the above Rule of transformation
$$ (0,\quad0)\rightarrow (0,\quad0) $$ $$ (0,\quad 1)\rightarrow (0,\quad 1) $$
$$ (1,\quad 0)\rightarrow (2,\quad 1) $$ $$ (1,\quad 1)\rightarrow (2, \quad 2) $$
It maps a square to a parallelogram with rotation of elements parallel to x-axis by a shear angle $\tan^{-1}\dfrac12$ and a linear magnification of $ \dfrac{\sqrt 3}{2},$
etc..