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NASA Identifies Massive Anorthosite Formation in Madagascar Resembling Lunar Highlands

Науковці NASA виявили великий масив анортозиту в Мадагаскарі, який нагадує гірські райони Місяця. Photo: НВ — Техно

NASA Observes Huge Anorthosite Deposit in Southern Madagascar

Astronauts aboard the International Space Station (ISS) have documented an enormous anorthosite rock formation in southern Madagascar. Covering an area of approximately 100 square kilometers, this rare geological feature closely resembles the bright highland terrains found on the Moon. Known as the Sariryaki massif, this formation dates back to the late Precambrian era—over 600 million years ago—and is linked to the assembly of the ancient supercontinent Gondwana.

The image was captured on October 12 at 21:03 using a Nikon Z9 digital camera equipped with a 400mm lens. Anorthosite, the dominant rock type here, is an intrusive igneous rock that formed deep beneath the Earth's surface. The region lies within a zone of intense tectonic movement, where high pressure and temperature conditions during Gondwana's formation created these distinctive geological structures.

The Geological Importance of Anorthosite

Gondwana once united landmasses that would become Africa, India, Madagascar, and Australia. Neighboring anorthosite deposits were originally part of a single continuous massif that was later stretched and fragmented by tectonic forces. Studying Earth's anorthosite analogs like Madagascar's provides valuable insight into the early crust formation processes of the Moon. Lunar highlands, rich in anorthosite, were formed over 4 billion years ago.

Since lunar soil samples returned by the Apollo missions are limited, examining similar terrestrial formations is crucial for advancing lunar geology. Comparable anorthosite bodies are also found in Montana's mountain ranges, offering additional perspectives on planetary crust development and evolution.

This discovery highlights the critical role of geological research in expanding our understanding of Earth's history as well as that of other celestial bodies, particularly the Moon. Investigating these formations can reveal new information about the origins of planetary crusts and support the planning of future space exploration missions and technology development.