Mapped: The Geology of the Moon in Astronomical Detail
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Mapped: The Geology of the Moon in Astronomical Detail

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View the medium resolution version of this map (9mb) | View the full resolution version of this map (47mb)

Geology of the Moon Map

View the medium resolution version of this map (9mb) | View the full resolution version of this map (47mb)

Mapped: The Geology of the Moon in Astronomical Detail

If you were to land on the Moon, where would you go?

Today’s post is the incredible Unified Geologic Map of the Moon from the USGS, which combines information from six regional lunar maps created during the Apollo era, as well as recent spacecraft observations.

Feet on the Ground, Head in the Sky

Since the beginning of humankind, the Moon has captured our collective imagination. It is one of the few celestial bodies visible to the naked eye from Earth. Over time different cultures wrapped the Moon in their own myths. To the Egyptians it was the god Thoth, to the Greeks, the goddess Artemis, and to the Hindus, Chandra.

Thoth was portrayed as a wise counselor who solved disputes and invented writing and the 365-day calendar. A headdress with a lunar disk sitting atop a crescent moon denoted Thoth as the arbiter of times and seasons.

Artemis was the twin sister of the sun god Apollo, and in Greek mythology she presided over childbirth, fertility, and the hunt. Just like her brother that illuminated the day, she was referred to as the torch bringer during the dark of night.

Chandra means the “Moon” in Sanskrit, Hindi, and other Indian languages. According to one Hindu legend, Ganesha—an elephant-headed deity—was returning home on a full moon night after a feast. On the journey, a snake crossed his pathway, frightening his horse. An overstuffed Ganesha fell to the ground on his stomach, vomiting out his dinner. On observing this, Chandra laughed, causing Ganesha to lose his temper. He broke off one of his tusks and hurled it toward the Moon, cursing him so that he would never be whole again. This legend describes the Moon’s waxing and waning including the big crater on the Moon, visible from Earth.

Such lunar myths have waned as technology has evolved, removing the mystery of the Moon but also opening up scientific debate.

Celestial Evolution: Two Theories

The pot marks on the Moon can be easily seen from the Earth’s surface with the naked eye, and it has led to numerous theories as to the history of the Moon. Recent scientific study brings forward two primary ideas.

One opinion of those who have studied the Moon is that it was once a liquid mass, and that its craters represent widespread and prolonged volcanic activity, when the gases and lava of the heated interior exploded to the surface.

However, there is another explanation for these lunar craters. According to G. K. Gilbert, of the USGS, the Moon was formed by the joining of a ring of meteorites which once encircled the Earth, and after the formation of the lunar sphere, the impact of meteors produced “craters” instead of arising from volcanic activity.

Either way, mapping the current contours of the lunar landscape will guide future human missions to the Moon by revealing regions that may be rich in useful resources or areas that need more detailed mapping to land a spacecraft safely .

Lay of the Land: Reading the Contours of the Moon

This map is a 1:5,000,000-scale geologic map built from six separate digital maps. The goal was to create a resource for science research and analysis to support future geologic mapping efforts.

Mapping purposes divide the Moon into the near side and far side. The far side of the Moon is the side that always faces away from the Earth, while the near side faces towards the Earth.

The most visible topographic feature is the giant far side South Pole-Aitken basin, which possesses the lowest elevations of the Moon. The highest elevations are found just to the northeast of this basin. Other large impact basins, such as the Maria Imbrium, Serenitatis, Crisium, Smythii, and Orientale, also have low elevations and elevated rims.

Shapes of Craters

The colors on the map help to define regional features while also highlighting consistent patterns across the lunar surface. Each one of these regions hosts the potential for resources.

Lunar Resources

Only further study will resolve the evolution of the Moon, but it is clear that there are resources earthlings can exploit. Hydrogen, oxygen, silicon, iron, magnesium, calcium, aluminum, manganese, and titanium are some of the metals and minerals on the Moon.

Interestingly, oxygen is the most abundant element on the Moon. It’s a primary component found in rocks, and this oxygen can be converted to a breathable gas with current technology. A more practical question would be how to best power this process.

Lunar soil is the easiest to mine, it can provide protection from radiation and meteoroids as material for construction. Ice can provide water for radiation shielding, life support, oxygen, and rocket propellant feed stock. Compounds from permanently shadowed craters could provide methane, ammonia, carbon dioxide, and carbon monoxide.

This is just the beginning—as more missions are sent to the Moon, there is more to discover.

Space Faring Humans

NASA plans to land astronauts—one female, one male—to the Moon by 2024 as part of the Artemis 3 mission, and after that, about once each year. It’s the beginning of an unfulfilled promise to make humans a space-faring civilization.

The Moon is just the beginning…the skills learned to map Near-Earth Objects will be the foundation for further exploration and discovery of the universe.

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Energy

The Periodic Table of Commodity Returns (2012-2021)

Energy fuels led the way as commodity prices surged in 2021, with only precious metals providing negative returns.

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commodity returns 2021 preview

The Periodic Table of Commodity Returns (2022 Edition)

For investors, 2021 was a year in which nearly every asset class finished in the green, with commodities providing some of the best returns.

The S&P Goldman Sachs Commodity Index (GSCI) was the third best-performing asset class in 2021, returning 37.1% and beating out real estate and all major equity indices.

This graphic from U.S. Global Investors tracks individual commodity returns over the past decade, ranking them based on their individual performance each year.

Commodity Prices Surge in 2021

After a strong performance from commodities (metals especially) in the year prior, 2021 was all about energy commodities.

The top three performers for 2021 were energy fuels, with coal providing the single best annual return of any commodity over the past 10 years at 160.6%. According to U.S. Global Investors, coal was also the least volatile commodity of 2021, meaning investors had a smooth ride as the fossil fuel surged in price.

Commodity2021 Returns
Coal160.61%
Crude Oil55.01%
Gas46.91%
Aluminum42.18%
Zinc31.53%
Nickel26.14%
Copper25.70%
Corn22.57%
Wheat20.34%
Lead18.32%
Gold-3.64%
Platinum-9.64%
Silver-11.72%
Palladium-22.21%

Source: U.S. Global Investors

The only commodities in the red this year were precious metals, which failed to stay positive despite rising inflation across goods and asset prices. Gold and silver had returns of -3.6% and -11.7% respectively, with platinum returning -9.6% and palladium, the worst performing commodity of 2021, at -22.2%.

Aside from the precious metals, every other commodity managed double-digit positive returns, with four commodities (crude oil, coal, aluminum, and wheat) having their best single-year performances of the past decade.

Energy Commodities Outperform as the World Reopens

The partial resumption of travel and the reopening of businesses in 2021 were both powerful catalysts that fueled the price rise of energy commodities.

After crude oil’s dip into negative prices in April 2020, black gold had a strong comeback in 2021 as it returned 55.01% while being the most volatile commodity of the year.

Natural gas prices also rose significantly (46.91%), with the UK and Europe’s natural gas prices rising even more as supply constraints came up against the winter demand surge.

Energy commodity returns 2021

Despite being the second worst performer of 2020 with the clean energy transition on the horizon, coal was 2021’s best commodity.

High electricity demand saw coal return in style, especially in China which accounts for one-third of global coal consumption.

Base Metals Beat out Precious Metals

2021 was a tale of two metals, as precious metals and base metals had opposing returns.

Copper, nickel, zinc, aluminum, and lead, all essential for the clean energy transition, kept up last year’s positive returns as the EV batteries and renewable energy technologies caught investors’ attention.

Demand for these energy metals looks set to continue in 2022, with Tesla having already signed a $1.5 billion deal for 75,000 tonnes of nickel with Talon Metals.

Metals price performance 2021

On the other end of the spectrum, precious metals simply sunk like a rock last year.

Investors turned to equities, real estate, and even cryptocurrencies to preserve and grow their investments, rather than the traditionally favorable gold (-3.64%) and silver (-11.72%). Platinum and palladium also lagged behind other commodities, only returning -9.64% and -22.21% respectively.

Grains Bring Steady Gains

In a year of over and underperformers, grains kept up their steady track record and notched their fifth year in a row of positive returns.

Both corn and wheat provided double-digit returns, with corn reaching eight-year highs and wheat reaching prices not seen in over nine years. Overall, these two grains followed 2021’s trend of increasing food prices, as the UN Food and Agriculture Organization’s food price index reached a 10-year high, rising by 17.8% over the course of the year.

Grains price performance 2021

As inflation across commodities, assets, and consumer goods surged in 2021, investors will now be keeping a sharp eye for a pullback in 2022. We’ll have to wait and see whether or not the Fed’s plans to increase rates and taper asset purchases will manage to provide price stability in commodities.

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Mining

Visualizing the Scale and Composition of the Earth’s Crust

This animation shows the handful of minerals and elements that constitute the Earth’s crust.

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Visualizing the Scale and Composition of the Earth’s Crust

For as long as humans have been wandering the top of Earth’s crust, we’ve been fascinated with what’s inside.

And Earth’s composition has been vital for our advancement. From finding the right kinds of rocks to make tools, all the way to making efficient batteries and circuit boards, we rely on minerals in Earth’s crust to fuel innovation and technology.

This animation by Dr. James O’Donoghue, a planetary researcher at the Japan Aerospace Exploration Agency (JAXA) and NASA, is a visual comparison of Earth’s outer layers and their major constituents by mass.

What is the Composition of Earth’s Crust?

The combined mass of Earth’s surface water and crust, the stiff outermost layer of our planet, is less than half a percent of the total mass of the Earth.

There are over 90 elements found in Earth’s crust. But only a small handful make up the majority of rocks, minerals, soil, and water we interact with daily.

1. Silicon

Most abundant in the crust is silicon dioxide (SiO2), found in pure form as the mineral quartz. We use quartz in the manufacturing of glass, electronics, and abrasives.

Why is silicon dioxide so abundant? It can easily combine with other elements to form “silicates,” a group of minerals that make up over 90% of Earth’s crust.

Clay is one of the better-known silicates and micas are silicate minerals used in paints and cosmetics to make them sparkle and shimmer.

MineralMajor ElementsPercentage of Crust
Plagioclase FeldsparO, Si, Al, Ca, Na39%
Alkali FeldsparO, Si, Al, Na, K12%
QuartzO, Si12%
PyroxeneO, Si, Mg, Fe11%
AmphiboleO, Si, Mg, Fe5%
Non-silicatesVariable8%
MicasO, Si, Al, Mg, Fe, Ca, Na, K5%
Clay MineralsO, Si, Al, Mg, Fe, Ca, Na, K5%
Other SilicatesO, Si3%

2. Aluminum and Calcium

SiO2 bonds very easily with aluminum and calcium, our next most abundant constituents. Together with some sodium and potassium, they form feldspar, a mineral that makes up 41% of rocks on Earth’s surface.

While you may not have heard of feldspar, you use it every day; it’s an important ingredient in ceramics and it lowers the melting point of glass, making it cheaper and easier to produce screens, windows, and drinking glasses.

3. Iron and Magnesium

Iron and magnesium each make up just under 5% of the crust’s mass, but they combine with SiO2 and other elements to form pyroxenes and amphiboles. These two important mineral groups constitute around 16% of crustal rocks.

Maybe the best known of these minerals are the two varieties of jade, jadeite (pyroxene) and nephrite (amphibole). Jade minerals have been prized for their beauty for centuries, and are commonly used in counter-tops, construction, and landscaping.

Some asbestos minerals, now largely banned for their cancer-causing properties, belong to the amphibole mineral group. They were once in high demand for their insulating and fire-retardant properties and were even used in brake pads, cigarette filters, and as artificial snow.

4. Water

Surprisingly, even though it covers almost three quarters of Earth’s surface, water (H2O) makes up less than 5% of the crust’s mass. This is partly because water is significantly less dense than other crustal constituents, meaning it has less mass per volume.

Breaking Earth’s Crust Down by Element

Though there are many different components that form the Earth’s crust, all of the above notably include oxygen.

When breaking down the crust by element, oxygen is indeed the most abundant element at just under half the mass of Earth’s crust. It is followed by silicon, aluminum, iron, calcium, and sodium.

All other remaining elements make up just over 5% of the crust’s mass. But that small section includes all the metals and rare earth elements that we use in construction and technology, which is why discovering and economically extracting them is so crucial.

What Lies Below?

As the crust is only the outermost layer of Earth, there are other layers left to contemplate and discover. While we have never directly interacted with the Earth’s mantle or core, we do know quite a bit about their structure and composition thanks to seismic tomography.

The Upper Mantle

At a few specific spots on Earth, volcanic eruptions and earthquakes have been strong enough to expose pieces of the upper mantle, which are also made of mostly silicates.

The mineral olivine makes up about 55% of the upper mantle composition and causes its greenish color. Pyroxene comes in second at 35%, and calcium-rich feldspar and other calcium and aluminum silicates make up between 5–10%.

Going Even Deeper

Beyond the upper mantle, Earth’s composition is not as well known.

Deep-mantle minerals have only been found on Earth’s surface as components of extra-terrestrial meteorites and as part of diamonds brought up from the deep mantle.

One thing the lower mantle is thought to contain is the silicate mineral bridgmanite, at an abundance of up to 75%. Earth’s core, meanwhile, is believed to be made up of iron and nickel with small amounts of oxygen, silicon, and sulphur.

As technology improves, we will be able to discover more about the mineral and elemental makeup of the Earth and have an even better understanding of the place we all call home.

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