

Earth's climate has swung between ice ages and warmer periods for millions of years, driven by subtle changes in our planet's orbit and axial tilt. These variations, known as Milankovitch cycles, occur because Earth doesn't orbit the sun in isolation. The gravitational pull of other planets constantly tugs at Earth, slowly altering its orbital path, the tilt of its axis, and the direction its poles point.
Medical News
|15th Jan, 2026
|phys.org
Medical News
|15th Jan, 2026
|phys.org
Medical News
|15th Jan, 2026
|phys.org
Medical News
|15th Jan, 2026
|phys.org
Medical News
|15th Jan, 2026
|phys.org
Medical News
|15th Jan, 2026
|phys.org
Medical News
|15th Jan, 2026
|phys.org