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How the mountain sundial works
The rod points at the pole
The rod is tilted to point at the celestial pole, the spot in the sky the stars turn round (close to the pole star in the north). The sun goes round that same axis once a day, so the rod’s shadow turns steadily through the day, at the same hour in the same place all year. That is why a bare mountain can’t be a sundial on its own, but a mountain with a rod can.
Why the lines bend over the mountain
Each hour the rod’s shadow lies in one flat slice of space through the rod. Where that slice cuts the plate the line is straight; where it cuts the mountain it follows the ground up ridges and down valleys. The page works out every line on the shape you print, so the shadow lands on them wherever it falls.
The figure-8
A sundial shows the sun’s time, which runs up to 16 minutes ahead of the clock in November and 14 minutes behind in February, because the Earth’s orbit is an ellipse and its axis is tilted. The tip of the rod at 12 o’clock on the clock traces a figure-8 over the year. The date lines show where the tip’s shadow runs on the longest day, the equinoxes and the shortest day.
Made for one latitude
The rod’s tilt and every line depend on how far north or south the sundial stands, so it is made for one place. It tells the right time within about 2° of latitude (around 200 km north or south). The hours are moved for your longitude within your time zone, so it reads the clock’s standard time.
When the shadow falls off the dial
The rod starts at the summit, high above the plate. When the sun is low, early or late in the day or in winter, its shadow can fall past the edge. That is why the summit sits off-centre, towards the equator, as the pointer does on a garden sundial: the shadows fall the other way, so they get most of the plate. The page counts how many sunny hours of the year it can be read, and picks a summit height that keeps that high. Make the summit lower to read it more often, or taller for a grander mountain.
In the classroom
Make one for your school and check it against the clock every week: does the gap follow the figure-8? Why does the noon line not point exactly north? Compare a dial made for your town with one made for a town far north: how do the rod and the lines change?
Elevation: Copernicus DEM GLO-30 (© DLR e.V. & Airbus) and Mapzen Terrain Tiles on AWS (SRTM, GMTED2010, ETOPO1 and others). Map © OpenStreetMap contributors, © CARTO. Sun positions: NOAA’s solar calculator method. More to make: an erupting volcano, a terrain zoetrope, the TerraPrinter app or more 3D map gift ideas.