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Apollo 16: Charting the Descartes Highlands

A Definitive Exploration of the Fifth Crewed Mission to Land on the Moon.

Mission Overview ๐Ÿ‘‡ Meet the Crew ๐Ÿ‘จโ€๐Ÿš€

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Mission Overview

The Fifth Lunar Landing

Apollo 16, designated as the tenth crewed mission of the Apollo program, marked the fifth lunar landing. It was the second of the program's "J missions," characterized by extended lunar surface stays, a strong emphasis on scientific objectives, and the utilization of the Lunar Roving Vehicle (LRV).

Landing Site: Descartes Highlands

The mission targeted the Descartes Highlands, a region selected for its potential to reveal insights into lunar volcanic activity. While initial hypotheses suggested volcanic origins, the geological samples collected ultimately indicated otherwise, contributing significantly to our understanding of lunar geological processes.

Duration and Scope

The mission spanned 11 days, 1 hour, 51 minutes, and 5 seconds. The crew spent approximately 71 hours on the lunar surface, conducting three extravehicular activities (EVAs) totaling over 20 hours, covering a distance of 26.7 kilometers using the LRV.

The Apollo 16 Crew

Commander: John W. Young

A seasoned astronaut with prior missions including Gemini 3, Gemini 10, and Apollo 10, John Young commanded Apollo 16. At 41, he was a Captain in the U.S. Navy and became the second American to fly in space four times.

Command Module Pilot: Thomas K. Mattingly II

Thomas Mattingly, a Lieutenant Commander in the U.S. Navy, served as the Command Module Pilot. Selected in 1966, he had previously been assigned to Apollo 13 but was replaced due to potential rubella exposure. His role involved orbiting the Moon while Young and Duke were on the surface.

Lunar Module Pilot: Charles M. Duke Jr.

Charles Duke, a Lieutenant Colonel in the U.S. Air Force, was the Lunar Module Pilot for Apollo 16. This was his sole spaceflight, making him the youngest of the twelve astronauts to walk on the Moon at the time of the mission (age 36).

Launch Vehicle & Spacecraft

Saturn V (AS-511)

The mission utilized the powerful Saturn V rocket, designated AS-511. This was the eleventh Saturn V flown and the ninth for a crewed mission. Minor modifications, including the reintroduction of retrorockets on the first stage, were implemented for enhanced safety and mission success.

Command/Service Module (CSM)

The CSM, named Casper, was manufactured by North American Rockwell. It served as the crew's primary living and working space during the translunar coast and lunar orbit phases. Thomas Mattingly piloted Casper during the mission.

Lunar Module (LM)

The Lunar Module, named Orion, was built by Grumman. It was designed for descent to and ascent from the lunar surface. John Young and Charles Duke piloted Orion, successfully landing in the Descartes Highlands.

Lunar Roving Vehicle (LRV)

Apollo 16 was the second mission to deploy the LRV, a four-wheeled electric vehicle. This enabled the crew to explore greater distances from the LM, significantly expanding their scientific reach on the lunar surface. Young and Duke drove the LRV for 26.7 kilometers.

Lunar Surface Operations

Moonwalks (EVAs)

Young and Duke conducted three EVAs, totaling 20 hours, 14 minutes, and 14 seconds. These excursions focused on geological surveys, sample collection, and the deployment of scientific instruments.

  • EVA-1: Focused on deploying the LRV, ALSEP, and initial sample collection near Plum Crater. John Young famously collected the largest Moon rock of the Apollo program, "Big Muley".
  • EVA-2: Explored Stone Mountain, reaching the highest elevation of any Apollo mission. The crew collected samples believed to be from the Descartes Formation.
  • EVA-3: Visited North Ray crater and "House Rock," a large boulder providing crucial evidence against the volcanic hypothesis for the Descartes region. Duke left a family photo and an Air Force medallion.

Geological Exploration

The primary scientific objective was to investigate the Descartes Highlands. The crew collected 95.71 kilograms of lunar samples, including breccias and crystalline rocks. Their findings challenged pre-mission theories about lunar volcanism, suggesting impact processes played a more significant role in shaping the highlands.

ALSEP Deployment

An Apollo Lunar Surface Experiments Package (ALSEP) was deployed, including a Passive Seismic Experiment, Active Seismic Experiment, Lunar Heat Flow Experiment, and Lunar Surface Magnetometer. These instruments continued to transmit data back to Earth long after the crew's departure.

Scientific Discoveries

Challenging Volcanic Theories

Analysis of samples from the Descartes and Cayley Formations provided critical data. Contrary to expectations, the geological evidence did not support the hypothesis of widespread lunar volcanism in this region. This led to a revised understanding of lunar geological evolution, emphasizing impact cratering.

Ultraviolet Astronomy

The mission carried a Far Ultraviolet Camera/Spectrograph, enabling the first astronomical observations from the Moon. This instrument captured images of Earth in ultraviolet light, revealing details of its hydrogen atmosphere and auroral belts.

Lunar Magnetism & Heat Flow

Experiments measured the Moon's weak magnetic field and heat flow from its interior. The Lunar Surface Magnetometer provided data on the lunar magnetic field's strength and variations. The Heat Flow Experiment, despite some difficulties, aimed to measure thermal gradients within the Moon.

Return Journey & Legacy

Trans-Earth Injection

After lunar liftoff and rendezvous with the CSM Casper, the crew jettisoned the LM ascent stage. The Service Module's engine was reignited for the trans-Earth injection burn, propelling them back towards Earth. A minor issue with the engine's backup gimbal system had necessitated a delay in the lunar landing but was successfully worked around for the return.

Deep Space EVA

During the return journey, Ken Mattingly performed an 83-minute Extravehicular Activity (EVA) in deep space to retrieve film cassettes from the Service Module's Scientific Instrument Module bay. This was one of only three such EVAs in the Apollo program.

Splashdown

Apollo 16 splashed down safely in the Pacific Ocean on April 27, 1972, after an 11-day mission. The command module, Casper, was recovered by the USS Ticonderoga. The mission concluded successfully, contributing invaluable data to lunar science.

Artifacts and Astronauts

The command module Casper is now displayed at the U.S. Space & Rocket Center in Huntsville, Alabama. Crew members John Young and Ken Mattingly later commanded Space Shuttle missions, extending their contributions to space exploration.

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References

References

  1.  Brooks, Grimwood, & Swenson 1979, p.ย 261.
A full list of references for this article are available at the Apollo 16 Wikipedia page

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Disclaimer

Important Notice

This content has been generated by an AI model and is based on publicly available information from Wikipedia. While efforts have been made to ensure accuracy and adherence to the source material, it is intended for informational and educational purposes only.

This is not professional advice. The information provided does not constitute expert guidance on space exploration, engineering, or history. Always consult official NASA documentation and qualified experts for definitive information.

The creators of this page are not responsible for any errors, omissions, or actions taken based on the information presented herein.