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What material was the lunar module made of?

What material was the lunar module made of?

The landing gear folds out after launch and is partly made of a crushable aluminum-honeycomb material to absorb the force of moon landing. There are four legs, one with a ladder and porch allowing astronauts access to the lunar surface.

What was the lunar modules used for?

The Lunar Module (LM) was used for descent to the lunar surface and served as a base while the astronauts were on the Moon. A separate ascent stage, comprising the top portion of the Lunar Module, lifted the astronauts from the Moon’s surface to rendezvous and dock with the command module, orbiting the Moon.

What is the lunar core made of?

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At the center is the Moon’s dense, metallic core. The core is largely composed of iron and some nickel. The inner core is a solid mass about 480 km in diameter. Surrounding the solid inner core is a fluid outer core, that brings the total diameter of the core to about 660 km.

What materials are spacecrafts made of?

This is why Aluminum and aluminum composite materials are used on spacecraft. Aluminum is light but also very sturdy. Using titanium alloys can also strengthen the body of the ship. The space shuttle also had very special thermal protection tiles, which helped it survive the heat of re-entry.

How did Apollo 13 use the lunar module?

The Apollo 13 continued on to the Moon, and the LM descent engine was used to accelerate the spacecraft around the Moon and back to Earth. The LM re-entered and burned in the Earth’s atmosphere over the southwest Pacific, any surviving pieces impacted in the deep ocean off the coast of New Zealand.

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What two main materials is the core made of?

Core. At the center of the Earth is the core, which has two parts. The solid, inner core of iron has a radius of about 760 miles (about 1,220 km), according to NASA. It is surrounded by a liquid, outer core composed of a nickel-iron alloy.

What materials does the core contain?

having to do with the physical formations of the Earth. change in a celestial body’s magnetic field so that the magnetic North and South Poles are switched. gradual change in temperature from the Earth’s core (hot) to its crust (cool), about 25° Celsus per kilometer of depth (1° Fahrenheit per 70 feet of depth).