Agriculture from the Ground Up
Jun 28, 2026 · 21 min · 14 segments
Why do Scottish farms look so green and productive while many WA Wheatbelt soils are sandy and naturally low in nutrients? The answer isn’t farming skill or climate alone; it’s geology and the age of…
Leonie SmithHost
All right, before we go on our imaginary world tour, I want to give you one big idea that will make sense of everything else you hear today.

Rocks that make soil are either young or old, and that single fact explains most of the differences in fertility, in texture, and management between farming regions anywhere in the world.

Young rocks form soils on recently deposited material, so think fresh glacier sediment, or recent volcanic ash, or alluvium from a river that flooded last century.

They haven't had long to weather, so they still have lots of nutrients locked up in their minerals, ready to be released.

Old rocks that have formed soils like ours in WA have been sitting under hot, wet conditions for millions of years, millions of years.

What's left is mostly quartz, iron oxides, and that kaolinite, which is stable but not very nutritious.

You'll be able to ask, is this parent material that formed this soil young or old? And that alone will tell you most of what you need to know about farming there.

All right, before we go on our imaginary world tour, I want to give you one big idea that will make sense of everything else you hear today.

Rocks that make soil are either young or old, and that single fact explains most of the differences in fertility, in texture, and management between farming regions anywhere in the world.

Young rocks form soils on recently deposited material, so think fresh glacier sediment, or recent volcanic ash, or alluvium from a river that flooded last century.

They haven't had long to weather, so they still have lots of nutrients locked up in their minerals, ready to be released.

Old rocks that have formed soils like ours in WA have been sitting under hot, wet conditions for millions of years, millions of years.

What's left is mostly quartz, iron oxides, and that kaolinite, which is stable but not very nutritious.

You'll be able to ask, is this parent material that formed this soil young or old? And that alone will tell you most of what you need to know about farming there.
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