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Includes statements from Development Matters (birth to age five) and the relevant ELGs in full, for the Making ice adult led activity
Includes statements from Development Matters (birth to age five) and the relevant ELGs in full, for the Making ice adult led activity
Play, Be, C Units provide enabling environments with teaching and support from adults. Reflecting on the characteristics of effective teaching and learning, children will have opportunity to learn and develop by:
- Playing and exploring – children investigate and experience things, and ‘have a go’.
- Active learning – children concentrate and keep on trying if they encounter difficulties and enjoy achievements.
- Creating and thinking critically – children have and develop their own ideas, make links between ideas, and develop strategies for doing things.
Early Years Foundation Stage Statutory Framework: accessed November 2024. Available under the Open Government Licence v3.0.
Water, wet, liquid, flowing, pour, fill, freezing, cold, solid, hard, melting, dripping, smooth, shiny, white, crystals, see through, cloudy, same, different
Show the children the glaciologist poster and tell the children that they are going to be glaciologists for this activity.
Ask the children if they know what a glaciologist does. A glaciologist is a scientist who studies glaciers. Glaciers are huge lump of ice found in mountains or near the poles which move slowly towards the sea.
Tell the children of the attributes. Glaciologists are:
Curious: glaciologists want to know more about how the ice in glaciers is made.
Observant: glaciologists look at the ice carefully to see what colour and shape it is.
Resilient: glaciologists need to be able work in cold and windy conditions. They need to be quick to recover and get back out in the cold again each day.
Explain that today they will be curious and observant in their glaciologist task.
Ask the glaciologists if they know how ice is made. Ask them what they think they will need to make some ice.
Show the children the different moulds, bags and trays and the jugs of water. Tell the children that they are going to fill their mould with water and freeze it. Show the children the different moulds, bags and trays and the jugs of water. Tell the children that they are going to fill their mould with water and freeze it.
You could ask:
Ask the children to choose a mould, bag or tray and to observe it carefully.
You could ask:
Get the children to fill their moulds with water and put them in the freezer. You may need to label them or make a list of who had each mould.
The next day, get the ice out of the freezer and return the moulds, bags or trays to the correct child. Get the children to try and get their ice out of the moulds/bags/trays. Tell them they will have to try hard and be resilient, like glaciologists, if they can’t get the ice out the first time.
You could ask:
Remember to refer to the children as glaciologists and praise them for using the attributes. You could say things like:
“You have been observant like a glaciologist and noticed what was the same about your mould and your ice.”
You could use the ice you have made for the Melting ice adult led activity or the Ice towers provocation.
We have put together some useful information about the science of glaciology to accompany this activity. Don’t worry, this is for your information only and to help you answer any questions children may have. We don’t expect you to explain this to the children in your setting!
The molecules in water are constantly moving. In a liquid, the molecules move more, and faster, than in a solid. As the liquid cools down the molecule movement slows down. When the water temperature reaches around 0°C, the molecules are closer together and weak bonds form between them. They form a solid that we call ice.
Glaciers form in places where more snow falls than melts. Soon after snow falls, it becomes more tightly packed, turning into ice pellets. These ice pellets get covered by even more snow and become more compressed. This results in a grainy ice forming. Every year as snow falls, layers of this granular ice fall on top of each other. When the pile grows to about 50m thick, the granular ice fuses together into a huge lump of ice.