ISRO scientists estimated the age of the Shiv Shakti point, the Chandrayaan-3 landing site on the Moon's south pole, to be 3.7 billion years old. Using high-end imaging techniques, they studied 25 craters and identified distinct terrain types, concluding that the low-relief smooth plains are that old.
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Picture Courtesy: INDIAN EXPRESS
Indian Space Research Organisation (ISRO) scientists have estimated the age of the Shiv Shakti point to be 3.7 billion years old.
The Shiv Shakti point is the name given to the Chandrayaan-3 landing site on the Moon's south pole, where India successfully achieved a soft landing on August 23, 2023.
The region around the landing site was mainly formed by the ejecta (material ejected during impacts) from the Manzinus and Boguslawsky craters. The Schomberger crater, with its well-preserved structures, also contributed to the terrain. |
A study by scientists from ISRO’s Physical Research Laboratory (PRL) estimates the age of the region around the Shiv Shakti point to be about 3.7 billion years, which coincides with the period when primitive microbial life first emerged on Earth.
Scientists used high-end imaging techniques, such as the Lunar Reconnaissance Orbiter wide-angle camera and terrain camera, to analyze craters and rock distributions. They studied 25 craters (500-1,150 meters in diameter) in the low-relief smooth plains, where the landing site is located, to estimate the age.
The low-relief smooth plains, which host the landing site, were found to be around 3.7 billion years old.
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PRACTICE QUESTION Q.Consider the following statements about the Shiv Shakti Point:
How many of the above statements are correct? A) Only one B) Only two C) All three D) None Answer: C Statement 1 is correct: Chandrayaan-3's Vikram lander successfully touched down near the lunar south pole at Shiv Shakti Point on August 23, 2023. Statement 2 is correct: Studies by ISRO's Physical Research Laboratory have determined that the area around the landing site is approximately 3.7 billion years old. Statement 3 is correct: Morphological analyses suggest that the local terrain around the landing site was largely formed by ejecta from the nearby Manzinus and Boguslawsky craters. |
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