Sciencey things for kids (young and old) to do at the beach

This may seem a bit geeky, but while you’re at the beach why not check out some of the things that like to live at beaches, or in the sea, the air, beneath the sand or on rocks. There are other things like waves that are pretty cool, especially if you like surfing, boogie-boarding or sailing, or even just looking at them to see how they work.  Scientists ask questions like;

“what is it?”

“how does it work or how does it live?”

“how does it react to other things going on at the beach (including what people do)?”

A diagram showing some of the things you can do at the beach

Waves We can ask all kinds of questions about waves, like how high are they, how fast do they move, or what happens when they break?  (check out this YouTube clip)

How high are the waves? The chances are you won’t have a measuring tape or clock in the water, but no problem. You can estimate the height of waves by using boogie boards, frisbee or beach ball as a scale. You may decide that the waves are 2 frisbees or half a boogie board high; when you get back to the beach or back home you can measure these. You can also use your own height as a guide. If you stand waist deep then that is about half your height, so for example if you are 120cm high, then the part of your body sticking out of the water is about 60cm.

Waves can also bend. The scientific word for this is Refraction. The best place to see this is at a beach that has a point of land or rock jutting out into the sea. If you climb high enough you may see waves bending round the point of land.

shell collage at the beachsciencey things 1

Flotsam and Jetsam. Flotsam is something that is accidently lost overboard; this will often happen during a shipwreck. Jetsam is something that is deliberately thrown overboard by a crew of a ship in distress, usually to lighten the ship’s load so that it won’t sink.  On our beaches you will see:

Wood, plastic bags, old toothbrushes, plastic bottles, glass bottles, plastic and foam beads, rusty tins, tangled rope, fish hooks. Some beaches have lots of this rubbish.

How much plastic can you find? Our oceans have millions of tonnes of plastic floating around. A lot of this plastic has just been thrown away by uncaring people. It kills birds, fish, and sea mammals like dolphins and whales. If you find plastic or glass or old tins can you please put them in a garbage.  Thanks.

Where does all the foam come from?

Sometimes there is so much foam that it blows in great wads up the beach.  It commonly forms

where waves break, in seawater that has organic matter from seaweed, algal blooms, dead critters and so on.  You may have noticed that foam may have a brownish tinge – this is from the organic matter that is dissolved in the seawater or is present as very tiny bits and pieces of organic matter. Good explanation for this at NOAA

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Conjugate fractures and en echelon tension gashes – indicators of brittle failure in Old Red Sandstone, Gougane Barra, County Cork, Ireland.
Mohr-Coulomb failure criteria
A montage of stress transformation paraphernalia and rock deformation
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The Marlborough strike-slip fault array extends north from the dextral Alpine Fault transform; faults continue across Cook Strait to join the North Island Dextral Fault Belt in the Wellington region (central Aotearoa New Zealand). In Marlborough and beneath Cook Strait there are several pull-apart basins formed at releasing bend stepovers. Sandbox analogue models can help us decipher the mechanical and kinematic processes that produce structures like these. Base image from NASA – International Space Station 2003.
Strike-slip analogue models
Scaled sand-box experiments are an ideal medium to observe rock deformation that, in this example, involves synkinematic deposition during rift-like crustal extension. The choice of model materials, in addition to imposed boundary conditions such as strain rates, will determine the outcome of the experiment. Dry sand was chosen for this model because its brittle behaviour under the model conditions is a good representation of natural rock failure. Diagram modified slightly from Eisenstadt and Sims, 2005, Figure 3a.
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The relationship between inertial and gravitational forces expressed by the Froude number (Fr) is reflected by the changes in surface flows and the formation-decay of stationary (standing) waves. Fr < 1 reflects subcritical (tranquil) flow; Fr>1 supercritical flow. Although the Froude number can be determined experimentally, it can also be eased out of a dimensional analysis of the relevant hydrodynamic variables.
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Conjugate fractures and en echelon tension gashes – indicators of brittle failure in Old Red Sandstone, Gougane Barra, County Cork, Ireland.
Mohr-Coulomb failure criteria
A montage of stress transformation paraphernalia and rock deformation
Mohr circles and stress transformation
The Marlborough strike-slip fault array extends north from the dextral Alpine Fault transform; faults continue across Cook Strait to join the North Island Dextral Fault Belt in the Wellington region (central Aotearoa New Zealand). In Marlborough and beneath Cook Strait there are several pull-apart basins formed at releasing bend stepovers. Sandbox analogue models can help us decipher the mechanical and kinematic processes that produce structures like these. Base image from NASA – International Space Station 2003.
Strike-slip analogue models
Scaled sand-box experiments are an ideal medium to observe rock deformation that, in this example, involves synkinematic deposition during rift-like crustal extension. The choice of model materials, in addition to imposed boundary conditions such as strain rates, will determine the outcome of the experiment. Dry sand was chosen for this model because its brittle behaviour under the model conditions is a good representation of natural rock failure. Diagram modified slightly from Eisenstadt and Sims, 2005, Figure 3a.
Analogue structure models: Scaling the materials
The relationship between inertial and gravitational forces expressed by the Froude number (Fr) is reflected by the changes in surface flows and the formation-decay of stationary (standing) waves. Fr < 1 reflects subcritical (tranquil) flow; Fr>1 supercritical flow. Although the Froude number can be determined experimentally, it can also be eased out of a dimensional analysis of the relevant hydrodynamic variables.
Model dimensions and dimensional analysis
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