What features can you see on the Moon with the naked eye, and how did they form?
The shape and size of the Moon, the principal naked-eye surface formations (craters, maria, terrae, mountains, valleys), their origin, and the named features on the lunar disc.
A focused answer to Edexcel GCSE Astronomy statements 2.1 to 2.5, covering the shape and mean diameter of the Moon, the principal naked-eye lunar surface formations (craters, maria, terrae, mountains and valleys) and their origin, and the named features such as the Sea of Tranquility, Tycho and the Apennine mountains.
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What this dot point is asking
Edexcel statements 2.1 to 2.5 want you to know the shape of the Moon and use its mean diameter of 3500 km, to recognise and explain the principal naked-eye lunar surface formations (craters, maria, terrae, mountains and valleys), and to identify named features on the lunar disc such as the Sea of Tranquility, Tycho and the Apennine mountains.
The shape and size of the Moon
The mean diameter is used in ratio and scale questions: comparing the Moon with the Earth and Sun, or working out how large the Moon appears in the sky. Despite the Sun being about 400 times wider than the Moon, the Sun is also about 400 times further away, so the two look almost the same angular size from Earth, which is why total solar eclipses are possible (a synoptic link to Topic 3).
The principal surface formations
The dark and light contrast you see with the naked eye is the maria (dark) against the terrae (light). The maria are younger because the lava resurfaced and smoothed them, so they have fewer craters; the terrae are older original crust, so they are saturated with craters. Recognising each formation, and giving its origin, is a frequent exam requirement.
How craters form and survive
On Earth, wind, rain, oceans and plate tectonics erase craters within millions of years, so few remain. The Moon's airless, dry, dead surface keeps its craters for billions of years, which is why its surface records the early bombardment of the Solar System. Bright streaks (rays) radiating from young craters such as Tycho are ejected material thrown out by the impact.
Named features on the lunar disc
The maria with names beginning "Sea" or "Ocean" are the dark patches; the named craters are bright, with Tycho's ray system especially prominent near full Moon. Being able to place these on a labelled lunar disc, and to say whether a feature is a mare, crater or mountain range, is exactly what the recognition statements (2.3 and 2.5) test.
How Edexcel examines this
This is naked-eye Paper 1 content with both recall and explanation marks. Recognition questions show a lunar disc and ask you to name maria, terrae or specific features such as the Sea of Tranquility or Tycho, so learn their appearance and positions. Explanation questions reward describing the maria as dark, smooth, low lava plains and the terrae as light, rough, cratered highlands, with their origins, and explaining crater formation by impact plus the Moon's lack of atmosphere, water and geological activity that preserves them. The mean diameter feeds ratio and scale calculations with the Earth and Sun. A frequent synoptic link is to Topic 9 (the Moon's far side and origin) and to the near-equal angular sizes that make total solar eclipses possible. The commonest errors are treating the maria as real seas and reversing the dark and light regions, so keep maria dark and terrae light.
Try this
Q1. State what the maria are and how they appear to the naked eye. [1 mark]
- Cue. Large dark smooth plains of solidified lava (they appear dark).
Q2. State why craters last far longer on the Moon than on Earth. [1 mark]
- Cue. The Moon has almost no atmosphere, no liquid water and little geological activity, so very little erosion.
Exam-style practice questions
Practice questions written in the style of Pearson Edexcel exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.
Edexcel 1AS0 20224 marksDescribe the difference between the maria and the terrae on the Moon, and explain how each type of region formed.Show worked answer →
The maria are the large, dark, smooth, low-lying plains on the Moon (1 mark), formed when ancient large impacts were later flooded by molten lava that cooled into dark solidified rock (1 mark). The terrae (highlands) are the lighter, rougher, heavily cratered higher regions (1 mark), which are the older original crust, scarred by many impacts and not resurfaced by lava (1 mark). Markers reward describing the maria as dark, smooth, low plains formed by lava flooding impact basins, and the terrae as light, rough, cratered older highlands. Note that maria appear dark and terrae appear light to the naked eye.
Edexcel 1AS0 20213 marksExplain how an impact crater forms on the Moon, and state why craters are much better preserved on the Moon than on the Earth.Show worked answer →
A crater forms when a meteoroid or asteroid strikes the surface at high speed, and the impact blasts out a roughly circular bowl, often with a raised rim and sometimes a central peak (1 mark). Craters are better preserved on the Moon because the Moon has almost no atmosphere and no liquid water, so there is very little weathering or erosion to wear them away (1 mark), and the Moon is geologically inactive, so there is little resurfacing by volcanism or plate tectonics (1 mark). Markers reward the impact origin and the lack of atmosphere, water and geological activity preserving the craters.
Related dot points
- The rotation and revolution periods of the Moon, the synchronous nature of its orbit, and the causes and effects of lunar libration.
A focused answer to Edexcel GCSE Astronomy statements 2.6 to 2.8, covering the rotation and orbital (revolution) periods of the Moon, why its synchronous (tidally locked) orbit means we always see the same near side, and the causes of lunar libration and its effect of letting us see about 59 percent of the surface over time.
- The shape, size and internal structure of the Earth: the oblate spheroid, the mean diameter of 13000 km, and the crust, mantle, outer core and inner core.
A focused answer to Edexcel GCSE Astronomy statements 1.1 to 1.3, covering why the Earth is an oblate spheroid, how to use its mean diameter of 13000 km, and the four major internal divisions (crust, mantle, outer core and inner core) and their features.
- The Moon's internal structure compared with the Earth's, the differences between the near and far sides, how the far side was mapped, escape velocity, and the theories of the Moon's origin.
A focused answer to Edexcel GCSE Astronomy statements 9.1 to 9.5, covering the Moon's internal divisions compared with the Earth's, the differences between the near and far sides, how the far side was mapped by spacecraft, the need to reach escape velocity using rockets, and the Giant Impact, Capture and Co-accretion theories of the Moon's origin.
- The bodies of the Solar System (planets, dwarf planets and small bodies), the structure and orbits of comets, the Kuiper Belt and Oort Cloud, and the characteristics of the planets.
A focused answer to Edexcel GCSE Astronomy statements 11.1 to 11.6 and 11.10 to 11.11, covering the bodies of the Solar System (planets, dwarf planets and small Solar System objects), the structure and orbits of short-period and long-period comets, the Kuiper Belt, Oort Cloud and heliosphere, and the principal characteristics of the planets.
Sources & how we know this
- Pearson Edexcel Level 1/Level 2 GCSE (9-1) in Astronomy (1AS0) specification — Pearson (2017)