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Australia's beaches show off the unique journey and makeup of sand

A small clear wave breaks onto the sandy shores.

Waves continuously churn, breaking down sand and reshaping the stories it carries. (ABC Midwest Wheatbelt: Chris Lewis)

Aussies love the beach and with our nation ringed by coastline, it's easy to see why. 

But have you ever looked closely at the sand and wondered how it got there?

Every grain tells a story of time and transformation.

Pinky hue sand granules on the left, an electronic microscope in the middle, pale creamy coloured sand granules on the right.

These two sand types, though just 300 metres apart, are distinctly different under the microscope. (ABC Midwest Wheatbelt: Chris Lewis)

While it may look pale from afar, up close it's a colourful mix of minerals and fragments.

University of WA school of earth sciences professor Annette George says, in geology terms, sand refers to "particles between 0.06 and 2 millimetres".

To unlock its secrets, you need to magnify it.

From bush to beach

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Professor George says much of our beach sand starts as inland rock, broken down and carried by rivers to the coast.

"Once that sediment reaches the coast, the material gets distributed by waves and currents."

Sunrise over the Greenough River as brown water flows into the sea.

As rivers flow from the bush to the sea, they carry a mix of rocks, sand and other materials. (ABC Midwest Wheatbelt: Chris Lewis)

In Geraldton, 420 kilometre north of Perth, the beach near Chapman River has pink, sparkly grains that have come from rocks further inland carried by the river — linking bush to beach in a dynamic cycle.

Under the microscope, these grains resemble tiny, intricate rocks.

A close up of the pinky sand with some small shell fragments on the surface.

The sparkling, pinkish sand near the Chapman River mouth originates from inland rocks that have eroded. (ABC Midwest Wheatbelt: Chris Lewis)

Nature's sand factory

Marine engineer Wade Greenaway says about 60 per cent of Geraldton's fine sand is biogenic (produced by living organisms) and is formed from marine life in seagrass meadows.

"Little creatures break down in seagrass beds. Seagrasses are really important. They're a sediment source," Mr Greenaway says.

"Limestone is a bit more of an ancient material but that does break down as well."

Sunlight gently lights up the seagrass under water.

Seagrass meadows play a vital role in sand formation. (ABC Midwest Wheatbelt: Chris Lewis)

Unique beaches

No two beaches are the same.

"For nine months of the year the sand moves from south to north and that's typical of the WA coastline," Mr Greenaway says.

"As the infrastructure on the coast has built up, it causes that interference with that long shore drift."

An aerial view of a big wave crashing onto shore, the water is a greeny colour and the sand golden brown.

Ocean swells and currents constantly shape the coastline, keeping it dynamic and ever-changing. (ABC Midwest Wheatbelt: Chris Lewis)

He says to restore balance, Midwest Ports transfers sand each year between beaches.

"When the port and wharf expanded, it blocked that natural flow, causing sand to build up," Mr Greenaway says.

"It's like a conveyor belt — we now have to manually feed it to restore natural sediment pathways."

An aerial shot of a wide sandy beach that sits alongside the Geraldton harbor.

Fine sand gathers on this beach in Geraldton and is manually transported to northern shores. (ABC Midwest Wheatbelt: Chris Lewis)

Midwest Ports also monitors sand composition annually.

"We're measuring the size and makeup of the sand to understand beach conditions like wind or wave energy," Mr Greenaway says.

"It supports our sand bypassing program and helps maintain consistency across the coastline."

A large truck tips white sand onto a beach with a bulldozer next to it scattering the sand.

Each year, sand is relocated from a southern beach to a northern beach to sustain the natural flow of sand drift. (ABC Midwest Wheatbelt: Chris Lewis)

History and human impact

Geraldton's coastal dynamics have long shaped its development.

Mr Greenaway's late grandfather, Gordon Greenaway, recalled sediment issues as far back as the early 20th century, when the railway jetty first altered natural sand movement.

Two people in orange high-vis on a beach are collecting beach sand into small glass jars.

Sand is analysed to assess particle sizes and beach conditions, ensuring natural sand drift continues. (ABC Midwest Wheatbelt: Chris Lewis)

Chosen as a port in the 1850s for its natural harbour, Geraldton has evolved, with deeper berths and regular dredging to suit larger ships.

Wade Greenaway says people often overlooked the complex, shifting nature of beaches.

"You always hear people say the beach isn't where it used to be, but it's always changing. We only see a small snapshot in our lifetimes," he says.

Wade is smiling at the camera, he is wearing a navy blue polo short

Wade Greenaway says beaches are forever changing. (ABC Midwest Wheatbelt: Chris Lewis)

Sand's never-ending journey

The story of sand doesn't stop at the shoreline.

Professor George says, over time, sand grains may become sandstone, rise again through geological uplift, and erode, starting the cycle anew.

Lots of tiny rock looking material, mostly pale looking but a small mix of darker tones.

Under the microscope, beach sand appears as tiny rock fragments. (ABC Midwest Wheatbelt: Chris Lewis)

"Once buried [1.5 to 2km below the Earth's surface] the sand basically becomes a rock and it keeps being buried," she says.

"Then eventually if it's lucky enough it will come back up to Earth's surface and then that process begins again."

As Mr Greenaway puts it, managing sand sustainably is vital: not just for ports, but for preserving the natural beauty we all love.

A close up of many small multicolored rocks and shells along the shoreline.

Small rocks wash up along the coast and gradually break down, transforming into sand. (ABC Midwest Wheatbelt: Chris Lewis)