What If? Lab
What if there were no soil?
Soil is the dark, crumbly ground where plants grow. It is full of tiny living things! What if there were no soil at all? Let's imagine it with Olly.
Soil is broken-down rock mixed with rotted plants and animals, plus water, air and huge numbers of living things. It holds plant roots, feeds them and soaks up rain, and UNEP says about 95 percent of our food comes from it. Under good conditions, one inch of topsoil can take hundreds of years to form. Imagine a world with no soil, and follow what might change.
Soil forms as parent material weathers under the influence of climate, organisms and relief over time (UC Cooperative Extension); one inch of topsoil can take 200 to 1,000 years even under favorable conditions. UNEP notes that 95 percent of food comes from soil. This thought experiment reasons about what might change without it, and how people care for the soil we have.
The big question
Soil is the ground where plants grow. It looks like plain dirt.
But soil is full of life! What if there were no soil anywhere?
Soil might look like plain dirt, but it is a mix of many things. Clemson University's soil guide lists soil particles, organic matter, water, air and living organisms. The particles are bits of broken rock: sand, silt and clay. The organic matter is what is left of plants and animals after they rot.
What if all the soil disappeared, leaving bare rock? In this thought experiment you can follow three paths: what happens to plant roots, what happens to the worms and fungi that live underground, and how soil forms in the first place.
Soil is a variable mixture of weathered minerals and decayed humus (University of Alaska Fairbanks Geophysical Institute), with water, air and living organisms (Clemson Cooperative Extension). Its three main kinds of particle are sand, silt and clay, whose proportions set its texture, which affects how much water and air it holds.
This thought experiment removes soil from the land and asks what might change for plants, soil organisms and the water that falls on the ground. It cannot say how soil might vanish; it reasons only from what soil does today and how slowly it forms.
Explore the idea
Make a prediction
How long can it take to make one inch of new topsoil?
Under good conditions, about how long can it take nature to make one inch of topsoil?
UC Cooperative Extension's estimate for forming one inch of topsoil under favorable conditions is…
- 200 to 1,000 years
- About one week
- About one year
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Established fact
Soil holds plants, feeds them and is full of life.
Soil anchors and feeds plants, stores water and is home to huge numbers of living things; about 95 percent of our food comes from it (UNEP).
Soil supports nearly all food-producing plants, regulates water and hosts immense biodiversity (UNEP; Columbia University's Earth Institute).
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Established fact
New soil takes hundreds of years to make.
Under good conditions, one inch of topsoil takes 200 to 1,000 years to form (UC Cooperative Extension).
Soil formation depends on parent material, climate, organisms, relief and time; UC gives 200 to 1,000 years per inch of topsoil under favorable conditions.
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An idea scientists discuss
A world with no soil is pretend. We imagine what might happen.
What might happen with no soil at all is an idea built from what soil does today.
Every consequence of a soil-free world here is reasoned from present processes and might differ greatly in reality.
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Established fact
Soil is made of tiny bits of rock, rotted plants, water, air and living things.
Soil is made of soil particles (sand, silt and clay), organic matter, water, air and living organisms.
Soil comprises mineral particles (sand, silt, clay), organic matter, water, air and living organisms; particle proportions set its texture (Clemson Cooperative Extension).
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Established fact
Most of the food we eat grows in soil.
About 95 percent of our food comes from soil, the material in which nearly all food plants grow.
Soil is the foundation of the food system: 95 percent of food comes from soil, the medium in which nearly all food-producing plants grow (UNEP).
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Established fact
In space, astronauts grow lettuce in little pillows.
NASA's Veggie garden grows each plant in a pillow filled with a clay-based growth material and fertilizer, which spreads water, nutrients and air around the roots.
Veggie's pillows of clay-based media and fertilizer keep water, nutrients and air balanced around roots, which might otherwise drown in water or be engulfed by air in microgravity (NASA).
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An idea scientists discuss
Without soil, plants might have nowhere to put their roots.
Without soil, most land plants might have nowhere to anchor their roots, and growing enough food might be very hard.
Without soil, food production might depend entirely on engineered growth media; whether that might feed many people cannot be judged here.
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Established fact
A handful of soil can hold millions of tiny living things.
A handful of soil can contain millions of bacteria and fungi, as well as tiny insects and microscopic animals called tardigrades.
A handful of soil can contain millions of bacteria and fungi, tiny insects and tardigrades; an estimated 360,000 animal species live in soil (UNEP, citing a European Commission report).
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Established fact
Worms dig tunnels that let air and water into the soil.
Earthworms, insects, millipedes and other small animals feed on dead plants and burrow, letting in air and making paths for water and roots.
Soil invertebrates (insects, roundworms, millipedes, centipedes, earthworms) decompose plant material and burrow, aerating soil; microbes release CO₂ that helps dissolve minerals (UAF Geophysical Institute).
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Established fact
One acre of soil can hold a lot of worms!
One acre of soil may contain 900 pounds of earthworms, 2,400 pounds of fungi and 1,500 pounds of bacteria.
Per acre, estimates of 900 lb of earthworms, 2,400 lb of fungi, 1,500 lb of bacteria and 133 lb of protozoa; a gram may hold a billion bacteria, 5 percent discovered (Columbia University's Earth Institute).
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An idea scientists discuss
Without soil, worms and fungi might have nowhere to live.
Without soil, worms, fungi and bacteria might lose their home, and dead leaves might pile up and rot much more slowly.
Losing soil organisms might slow decomposition and nutrient return to plants; how fast leaf litter might accumulate cannot be estimated here.
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Established fact
It can take hundreds of years to make one inch of topsoil.
Under good plant cover and the most favorable climate, one inch (about 2.5 centimeters) of topsoil takes 200 to 1,000 years to form.
Under good vegetative cover and favorable climate, an inch of topsoil takes 200 to 1,000 years; strongly developed soils indicate a million or more years of soil building (UC Cooperative Extension).
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Established fact
Where glaciers left piles of rock and gravel, the first signs of soil came in about 15 years.
On ground left by Alaskan glaciers, the first traces of soil can appear in about 15 years, a surface layer in about 250 years, and a full soil in about 2,000 years.
On Alaskan glacial moraines, traces of soil formation appear within about 15 years, a surface loam in about 250 and a full profile in about 2,000 (UAF Geophysical Institute).
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Established fact
People help soil with compost and by keeping plants growing on it.
UNEP suggests adding compost and mulch, keeping the ground covered with plants, and digging and plowing less to keep soil healthy.
UNEP's measures include raising organic matter (groundcover, mulch, compost), minimal tillage, retaining crop residues and year-round groundcover; it reports one third of the world's soil is degraded.
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An idea scientists discuss
If soil were all gone, making it again might take a very long time.
If all soil disappeared, nature might need hundreds or thousands of years to make new soil deep enough for farms.
Rebuilding soil from bare rock might take centuries to millennia, depending on parent material, climate and colonizing organisms; no single figure applies.
In our world
Plants push their roots down into soil. The soil holds them up.
Soil gives roots water and food. Most of the food we eat grows in soil!
Soil holds plant roots in place and gives them nutrients, the chemicals plants need to grow. It also soaks up, releases and cleans water. UNEP says that about 95 percent of our food comes from soil, and that nearly all food crops grow in it.
Soil is also crowded with life. A handful can hold millions of bacteria and fungi, along with tiny insects and microscopic animals called tardigrades. An article from Columbia University's Earth Institute estimates that one acre of soil may contain 900 pounds of earthworms and 2,400 pounds of fungi.
Soil anchors roots, supplies nutrients and absorbs, releases and purifies water (Columbia University's Earth Institute). UNEP calls it the foundation of the food system: 95 percent of our food comes from soil, the medium in which nearly all food-producing plants grow.
Its biodiversity is immense. The Earth Institute article estimates that an acre may hold 900 pounds of earthworms, 2,400 of fungi, 1,500 of bacteria, 133 of protozoa and 890 of arthropods and algae, and that a gram may hold a billion bacteria, only 5 percent of them discovered. UNEP cites an estimate of 360,000 animal species living in soil.
Imagine no soil
Let's pretend all the soil is gone. Only bare rock is left.
Plants might have nowhere to put their roots. Rain might run off the rock. Let's find out why.
Now imagine the land with no soil, just bare rock. Most plants might have nowhere to anchor their roots and nothing to take nutrients from. Farms might not be able to grow crops in fields at all.
Rain might pour off the bare rock instead of soaking in, and the worms, fungi and bacteria that live underground might lose their home. Dead leaves might pile up with fewer living things to break them down. These are ideas: we reason from what soil does today.
Without soil, rooted land plants might lose both anchorage and their nutrient and water supply, and since UNEP traces 95 percent of food to soil, food production might depend on small, managed growth systems instead.
Water might run off rock surfaces rather than infiltrating, removing the absorption and slow release the Earth Institute credits to soil. Decomposition and nutrient cycling might slow sharply with the loss of soil bacteria, fungi and invertebrates. Rebuilding soil might take centuries for each inch, as the next sections show. These are reasoned ideas, not predictions.
How soil forms
Soil starts as rock. Over a very long time, rock breaks into tiny bits.
Plants grow, die and rot. Worms and tiny living things mix it all together. Slowly, it becomes soil.
Soil forms from parent material: rock that has broken down, or loose material carried by water, wind or ice. UC Cooperative Extension lists five things that shape soil: the parent material, the climate, plants and animals, the shape of the land, and time.
Living things do much of the work. Plant roots loosen the ground and add organic matter. Bacteria and fungi break down dead plants. Earthworms, insects, millipedes and other small animals feed on plant bits and burrow, letting in air and making paths for water and roots. Under good conditions, one inch of topsoil can take 200 to 1,000 years to form.
UC Cooperative Extension names five soil-forming factors: parent material, climate, vegetation and animal life, relief, and time. Climate and vegetation are the active forces; relief modifies them through runoff and temperature.
Microorganisms decompose plant matter, producing carbon dioxide that combines with soil moisture to dissolve minerals, and some bacteria fix nitrogen from the air (UAF Geophysical Institute). Soil invertebrates feed on plant material and burrow, aerating the soil. Rates depend on all five factors: UC gives 200 to 1,000 years per inch of topsoil under favorable conditions, while on young Alaskan glacial moraines a surface loam layer can develop in about 250 years.
Caring for soil
People can help soil stay healthy.
They add compost, keep plants growing over the ground, and dig less. Astronauts even grow lettuce in space, in little pillows!
Because soil forms so slowly, people work to protect the soil we have. UNEP suggests adding organic matter with compost and mulch, keeping the ground covered with plants all year, digging and plowing less, and using fertilizers and pesticides carefully.
Plants can grow in other materials too, with a lot of care. NASA's Veggie garden on the International Space Station grows each plant in a small pillow filled with a clay-based growth material and fertilizer. The pillows spread water, nutrients and air around the roots. Astronauts have grown lettuce, kale and zinnia flowers this way.
UNEP reports that one third of the world's soil is degraded, and lists ways to nurture it: raising organic matter through groundcover, mulch and compost; minimal tillage and retaining crop residues; planned rotational grazing; careful, targeted use of fertilizers and pesticides; and aiming for groundcover all year.
In space, plants are grown without garden soil using careful engineering. NASA's Veggie system uses pillows of clay-based growth media and fertilizer to balance water, nutrients and air around roots in microgravity, and has produced three types of lettuce, Chinese cabbage, mizuna mustard, red Russian kale and zinnias.
Amazing facts
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Some soils are very, very old!
Some soils in California show a million or more years of soil building, while soil at a farming area in Alaska is mostly younger than 10,000 years.
UC Cooperative Extension notes that some Ventura County soils, with strongly developed subsoils or hardpans, indicate a million or more years of soil building; UAF's Geophysical Institute notes that soil at the Big Delta agricultural project in Alaska is post-glacial and typically younger than 10,000 years.
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Astronauts have grown flowers in space!
NASA's Veggie garden has grown three types of lettuce, Chinese cabbage, mizuna mustard, red Russian kale and zinnia flowers.
Veggie, about the size of a carry-on bag and typically holding six plants, has grown lettuces, Chinese cabbage, mizuna mustard, red Russian kale and zinnias (NASA).
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Just one gram of soil, a tiny bit, can hold a billion bacteria!
One gram of soil may hold one billion bacteria, and only about 5 percent of them have been discovered.
A gram of soil may hold a billion bacteria, of which only 5 percent have been discovered (Columbia University's Earth Institute).
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Sunshine helps make soil.
Sunshine powers the weathering that breaks rock down and turns it into soil.
UAF's Geophysical Institute notes that sunshine powers both the physical and biochemical weathering needed for soil formation.
Words to know
- soil
- the top layer of the ground, made of bits of rock, rotted living things, water, air and life
- parent material
- the broken rock or loose material that a soil forms from
- weathering
- the slow breaking down of rock into smaller pieces
- humus
- dark material made from rotted plants and animals
- topsoil
- the upper layer of soil, with the most organic matter and tiny living things
- decomposer
- a living thing, such as a fungus or a bacterium, that breaks down dead plants and animals
- compost
- rotted plant scraps that people add to soil to help it
Discovery challenge
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How much of our food comes from soil?
According to UNEP, about how much of our food comes from soil?
UNEP's figure for the share of our food that comes from soil is…
- About 95 percent
- About 5 percent
- None of it
Show the answer
About 95 percent
Almost all of it: about 95 percent!
About 95 percent, because nearly all food crops grow in soil.
…95 percent; soil is the medium for nearly all food-producing plants (UNEP).
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Which animal digs tunnels that let air and water into soil?
Which animal burrows through soil, letting in air and making paths for water and roots?
Which of these soil invertebrates aerates soil by burrowing?
- Earthworms
- Goldfish
- Pigeons
Show the answer
Earthworms
Earthworms! Their tunnels let air and water in.
Earthworms, along with insects, millipedes and other small animals.
Earthworms, with insects, roundworms, millipedes and centipedes (UAF Geophysical Institute).
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How long can one inch of new topsoil take to make?
Under good conditions, how long can one inch of topsoil take to form?
UC Cooperative Extension gives the time to form one inch of topsoil under favorable conditions as…
- 200 to 1,000 years
- About a week
- About a year
Show the answer
200 to 1,000 years
Hundreds of years: 200 to 1,000!
200 to 1,000 years, under good plant cover and climate.
…200 to 1,000 years, depending on the other soil-forming factors.
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In the space garden, what do the plants grow in?
In NASA's Veggie garden on the space station, what does each plant grow in?
NASA's Veggie system supplies roots with water, nutrients and air using…
- A pillow of clay-based material and fertilizer
- A bag of sugar
- A bare metal tray
Show the answer
A pillow of clay-based material and fertilizer
A little pillow full of clay-based material.
A pillow filled with clay-based growth material and fertilizer.
…pillows of clay-based growth media and fertilizer (NASA).
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In a soil jar test, which part sinks to the bottom first?
In a soil jar test, which part settles to the bottom within about a minute?
In Clemson's jar test, the layer that settles within one minute is…
- Sand
- Clay
- Silt
Show the answer
Sand
Sand! It sinks to the bottom in about a minute.
Sand settles first; the silt layer is marked after 2 hours and the clay after 48 hours.
…the coarse sand layer; silt is marked after 2 hours and clay after 48 (Clemson Cooperative Extension).
Experiments to try
- Watch What If? Lab What if volcanoes stopped erupting? Volcanoes build new land, like the island of Surtsey near Iceland, and their rock slowly breaks down into some of the richest soil on Earth. Over millions of years, gases from volcanoes even helped give Earth its air and oceans. Imagine every volcano going quiet, and follow what might change.
- Watch What If? Lab What if Earth had no deserts? About one third of Earth's land is desert. Deserts form where sinking air dries out the sky or mountains block the rain, and they are home to animals found nowhere else. Their dust even blows across an ocean to feed the Amazon rainforest. Imagine Earth with no deserts and see what would change.
- Watch What If? Lab What if all trees disappeared? Trees take in carbon dioxide and store carbon in their wood, put water into the air, hold soil in place and give homes to most kinds of land animals. Follow what would happen without them, and find out why the ocean still makes about half of our oxygen.
- Watch What If? Lab What if hurricanes could be steered? Hurricanes are huge spinning storms that grow over warm ocean water. Nobody can steer or stop one today: a hurricane holds far more energy than people could ever push around. What people can do is forecast where it may go and get ready early. Imagine steering one, then see why forecasts are the real answer.
- Watch What If? Lab What if there were no decomposers? Bacteria, fungi, earthworms and millipedes break down dead leaves, wood and dead plants and animals, and give their nutrients back to the soil. National Geographic calls them Earth's cleanup crew. Imagine a world without them, and follow what might pile up, what might run short, and who does the work.
- Watch What If? Lab What if plants ate insects everywhere? Carnivorous plants catch insects to get nutrients their soggy, poor soil can't give them. They still make food from sunlight. Imagine if every plant everywhere caught insects: would it help them, and why do so few plants bother?
Explore next
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Watch
Animal
Common earthworm
The common earthworm digs deep tunnels in the soil and comes up at night to drag fallen leaves down to eat. It breathes through its damp skin, has red blood and five pairs of heart-like pumps. Its tunnels and droppings help keep soil healthy.
- Watch What If? Lab What if volcanoes stopped erupting? Volcanoes build new land, like the island of Surtsey near Iceland, and their rock slowly breaks down into some of the richest soil on Earth. Over millions of years, gases from volcanoes even helped give Earth its air and oceans. Imagine every volcano going quiet, and follow what might change.
- Watch What If? Lab What if Earth had no deserts? About one third of Earth's land is desert. Deserts form where sinking air dries out the sky or mountains block the rain, and they are home to animals found nowhere else. Their dust even blows across an ocean to feed the Amazon rainforest. Imagine Earth with no deserts and see what would change.
- Watch What If? Lab What if all trees disappeared? Trees take in carbon dioxide and store carbon in their wood, put water into the air, hold soil in place and give homes to most kinds of land animals. Follow what would happen without them, and find out why the ocean still makes about half of our oxygen.
- Watch What If? Lab What if hurricanes could be steered? Hurricanes are huge spinning storms that grow over warm ocean water. Nobody can steer or stop one today: a hurricane holds far more energy than people could ever push around. What people can do is forecast where it may go and get ready early. Imagine steering one, then see why forecasts are the real answer.
- Watch What If? Lab What if there were no decomposers? Bacteria, fungi, earthworms and millipedes break down dead leaves, wood and dead plants and animals, and give their nutrients back to the soil. National Geographic calls them Earth's cleanup crew. Imagine a world without them, and follow what might pile up, what might run short, and who does the work.
- Watch What If? Lab What if plants ate insects everywhere? Carnivorous plants catch insects to get nutrients their soggy, poor soil can't give them. They still make food from sunlight. Imagine if every plant everywhere caught insects: would it help them, and why do so few plants bother?
- Watch Try it What If? Lab What if Earth had no atmosphere? Earth's air works like a jacket: it keeps heat in and carries it around. Take the air away in our model of a sandy patch of ground on the equator, and the coldest part of the night drops from about 13 °C to about 2 °C.
For parents & teachers
What children will learn
- Soil is a mix of rock particles, organic matter, water, air and living organisms.
- Soil anchors and feeds plants, stores water and supports almost all of our food.
- Soil forms slowly from rock through weathering and the work of living things.
- Thought experiments separate known facts from reasoned ideas.
Recommended ages: 7 to 17 ยท About 15 minutes
Talk about it
- What do you think lives in the soil under your feet right now?
- Why might farmers and gardeners add compost and keep plants growing over the ground?
- If soil takes hundreds of years to form, how should we treat the soil we have?
Try at home or in class
- Soil jar test (Clemson Cooperative Extension): a grown-up digs a cup of garden soil and sifts out stones and roots. Fill a clear jar with a lid (plastic is safest) one-third full of soil, top it up with water, close it tightly and shake. Mark the sand layer after 1 minute, the silt after 2 hours and the clay after 48 hours. Wash hands afterward.
- With a grown-up and garden gloves, gently lift a log, stone or pile of leaves in a garden and look for worms, beetles and fungi. Put everything back as you found it, and wash your hands afterward.
Key vocabulary: soil, parent material, weathering, humus, topsoil, decomposer, compost
Where these facts come from
- Formation and Classification of the Soil , UC Cooperative Extension Ventura County (University of California Agriculture and Natural Resources)
- Soil Formation (Alaska Science Forum) , University of Alaska Fairbanks Geophysical Institute
- Why Soil Matters , Columbia Climate School, State of the Planet (Columbia University)
- What's the big deal about dirt? , UN Environment Programme
- Growing Plants in Space , NASA
- Soil Horizons , Soil Science Society of America, Soils 4 Teachers
- Soil Texture Analysis "The Jar Test" , Clemson Cooperative Extension, Home & Garden Information Center
Checked, not yet human-reviewed. Last updated October 24, 2026. Spotted a mistake? Tell us.