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To produce a children's sticker chart from a provided image, the following code divides it into squares (which can be cut out) and produces further images with matching labels for the reverse side of the printed image and a piece of card onto which the squares can be stuck (you need to provide your own glue).

Loosely speaking, in the Gregorian calendar, Easter falls on the first Sunday following the first full Moon on or after 21 March. There are various algorithms (*Computus*) which can be used to calculate its date, and the cycle of dates repeats every 5.7 million years.
The following code produces a bar chart of the distribution of Easter dates using one of these algorithms.

A linear transformation in two dimensions can be visualized through its effect on the two orthonormal basis vectors $\hat{\imath}$ and $\hat{\jmath}$. In general, it can be represented by a $2 \times 2$ matrix, $\boldsymbol{T}$, which acts on a vector $v$ to map it from a vector space spanned by one basis onto a different vector space spanned by another basis: $\boldsymbol{v'} = \boldsymbol{T}\boldsymbol{v}$. This change of basis can be visualized by drawing the basis vectors in the two-dimensional plane, along with equally-spaced "grid lines" parallel to each of them. A linear transformation keeps the grid lines evenly spaced, and the origin fixed.

The mildly controversial geocoding system What3words encodes the geographic coordinates of a location (to a resolution of 3 m) on the Earth's surface into three dictionary words, through some proprietary algorithm. The idea is that human's find it easier to remember and communicate these words than the sequence of digits that makes up the corresponding latitude and longitude. For example, the Victoria Memorial in front of Buckingham Palace in London is located at (51.50187, -0.14063) in decimal latitude, longitude coordinates, but simply `using.woods.laws`

in the language of What3words.

The magnetic field due to a magnetic dipole moment, $\boldsymbol{m}$ at a point $\boldsymbol{r}$ relative to it may be written $$ \boldsymbol{B}(\boldsymbol{r}) = \frac{\mu_0}{4\pi r^3}[3\boldsymbol{\hat{r}(\boldsymbol{\hat{r}} \cdot \boldsymbol{m}) - \boldsymbol{m}}], $$ where $\mu_0$ is the vacuum permeability. In geomagnetism, it is usual to write the radial and angular components of $\boldsymbol{B}$ as: $$ \begin{align*} B_r & = -2B_0\left(\frac{R_\mathrm{E}}{r}\right)^3\cos\theta, \\ B_\theta & = -B_0\left(\frac{R_\mathrm{E}}{r}\right)^3\sin\theta, \\ B_\phi &= 0, \end{align*} $$ where $\theta$ is polar (colatitude) angle (relative to the magnetic North pole), $\phi$ is the azimuthal angle (longitude), and $R_\mathrm{E}$ is the Earth's radius, about 6370 km. See below for a derivation of these formulae.