Sun Path
where light meets land, right now
listening for the sun…
drag to rotate · tap a gold pin to read its alignment
Walk through time
The four turnings drift. Earth's tilt creeps by a fraction of a degree each millennium, so the spot where the solstice sun breaks the horizon slides along it. Pick a monument and walk the years — watch the sun pull away from where its builders aimed. (At the equinox they all agree: due east and due west, within two degrees.)
A calendar of turnings
The four hinges of the year, each marked across cultures by walks, processions, and gatherings.
The sun's figure of eight
Stand at solar noon every day for a year and trace where the sun is. The shape it draws is the analemma — a slow, elegant figure-of-eight written by Earth's tilted, elliptical orbit.
How long the dark lasts
Every section above asks what the sun does. This one asks what its absence gives you: the hours of true dark — the sun a full 18° below the horizon, deep enough for the faintest stars. At the equator that is the same length every night of the year. Further north it swings, and past about 48½° it stops coming at all for part of the summer.
Where dawn comes from
At the equator the sun rises within 23½° of due east all year. The further from the equator, the wider its swing — until at high latitudes there are months when it never rises at all.
Walk to the sun
Tomorrow vs today
Around the equinoxes, the day grows or shrinks by 2–3 minutes every 24 hours. Around the solstices, almost nothing — solstice is Latin for "the sun stands still."
If you're walking a pilgrimage stage, The Light Budget turns this into a usable answer — pick a route, set a pace, see whether today's light holds.
The Moon Path shows where the moon stands at any coord — phase, tide curve, lunar standstill — a companion instrument for night walks and coastal stages.
Add to your calendar (.ics) or subscribe, and new years arrive on their own: Apple & Outlook · Google Calendar
Add to your calendar (.ics) or subscribe, and new years arrive on their own: Apple & Outlook · Google Calendar
Add to your calendar (.ics) or subscribe, and new years arrive on their own: Apple & Outlook · Google Calendar
How this is computed
The sun's position uses the NOAA Solar Calculator's equations — declination within 0.004°, the equation of time within 4 seconds, against JPL Horizons for 2000–2050. The moon and the deep-time scrubber use Meeus, Astronomical Algorithms (2nd ed.). Ancient solar and lunar alignments are pinned from archaeological literature (Ruggles, Astronomy in Prehistoric Britain and Ireland), not derived from the model. Good for contemplation, not for navigation. The deep-time horizon uses each year's obliquity (valid roughly 3000 BC–3000 AD) for the sunrise/sunset azimuth, against a fixed alignment bearing: Stonehenge's solstitial axis (Lockyer & Penrose 1901; Ruggles 1997) and the great-circle bearing from Ōmori-Katsuyama to Mt. Iwaki's summit, whose winter-solstice sunset is documented by Kaner (World Archaeology 115, 2022) and the UNESCO Jōmon listing. Azimuths assume a flat sea-level horizon and ignore atmospheric refraction (~0.5°) and disc radius, so they mark the geometric event, not the first gleam.