ORBIT Solar System Explorer

Natural satellite Nereid

Nereid

An elongated orbit with a changing view

Its highly eccentric orbit brings large changes in distance from Neptune, unlike regular moons on nearly circular orbits.

Rendered view of Nereid
Illustrative surface and shape · Image credits
Mean radius
170 km
Mean diameter
340 km
Orbital semimajor axis
5,513,900 km

01 / Overview

Meet Nereid

Nereid's highly eccentric orbit produces large changes in its distance from Neptune. This differs strongly from close, nearly circular regular-moon orbits. Far less surface detail is known than for Triton, so orbital information provides a firmer introduction to this distant small world than a purported global map.

02 / Key data

Core parameters

Mean radius
170 km
Mean diameter
340 km
Orbital semimajor axis
5,513,900 km
Orbital period
360.13 d
Parent planet
Neptune
Data and calculation notes

Radii are mean values; orbital data describe each world’s scale and motion.

03 / Further reading

A closer look

What makes this world distinctive5
  • Gerard Kuiper discovered Nereid in 1949.

  • Nereid's orbit has an eccentricity around 0.75 and is highly elongated.

  • Nereid takes nearly an Earth year to orbit Neptune.

  • Nereid's distance from Neptune varies greatly along its orbit.

  • Nereid's elongated orbit contrasts with Triton's nearly circular one.

Gravity and the interior14
  • A natural satellite forms naturally and orbits a larger body; an artificial satellite is built by people.

  • Tidal locking matches rotation to orbital motion; it does not mean no rotation.

  • A moon's orbit need not lie in the same plane as its planet's orbit around the Sun.

  • Differences in gravity across a moon can deform it through tides.

  • Repeated tidal deformation can turn orbital energy into internal heat.

  • Orbital resonance means periods near simple integer ratios, allowing repeated pulls between moons to build up.

  • Some moons formed in discs around planets; others may have been captured later.

  • Small moons are often irregular because their gravity cannot overcome the strength of their materials.

  • Large moons tend to be rounder because gravity shapes them.

  • Icy moons may have liquid oceans under their shells; a frozen surface does not mean a fully frozen interior.

  • Finding water or organic molecules is not the same as finding life.

  • A planet and moon both orbit their common center of mass; the heavier body's wobble is usually smaller.

  • Other bodies perturb a moon's orbit; a fixed ellipse is only an approximation.

  • Moons can be larger than some planets; classification is not based on diameter alone.

Surface and observation11
  • Its highly eccentric orbit brings large changes in distance from Neptune, unlike regular moons on nearly circular orbits.

  • A moon's visible brightness usually comes from reflected sunlight.

  • Moons have sunlit and dark sides too; the side facing away from the planet is not permanently dark.

  • Crater counts help estimate surface ages, but resurfacing and the impact environment also matter.

  • A moon hiding a background star causes an occultation, useful for measuring size or probing an atmosphere.

  • A moon entering its planet's shadow experiences an eclipse, depending on the orbits' spatial alignment.

  • Tiny changes in a spacecraft's speed can reveal a moon's mass and gravity field.

  • Composition, grain size, and lighting all affect surface color; enhanced-color images differ from naked-eye views.

  • The day–night boundary is the terminator; long shadows nearby bring out terrain.

  • Surfaces with little or no atmosphere lack strong weather erosion and preserve old impact scars more easily.

  • A moon's observed phases come from changing angles between the Sun, moon, and observer.

04 / Sources

Trusted sources

NASA Science — NereidJPL — Orbital data

Image credits

Images reproject and light existing textures; they are not live observations.

Surface texture:cubicApocalypse / CelestiaContent · License · Rendered by ORBIT

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