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https://www.youtube.com/watch?v=41fqhfI5mVs

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https://drive.google.com/file/d/0B8aFB01t6r9ydlRPMXVheHFydmM/view

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https://www.boundless.com/biology/textbooks/boundless-biology-textbook/the-chemical-foundation-of-life-2/water-51/water-s-states-gas-liquid-and-solid-282-11415/
http://chemistry.elmhurst.edu/vchembook/122Adensityice.html

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Ice, snow, hail and other forms of solid water are all important parts of the water cycle. Water is often stored in icebergs and frozen all over the world. Also it is transported from the one place to another in the same way rain does but in the form of snow, sleet, or hail.

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https://water.usgs.gov/edu/surface-tension.html
https://chem.libretexts.org/Core/Physical_and_Theoretical_Chemistry/Physical_Properties_of_Matter/States_of_Matter/Properties_of_Liquids/Surface_Tension

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Rain drops have a lot of surface tension allowing them to keep there shape when falling and surfaces like windows.

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When adding a substance to water it creates rings in the water. the rings show the surface tension breaking.

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The density of water is 1 g/cm³ and if something has a greater density than water it would sink. If it  has a smaller density than that, it will sink. The density of ice is 0.9340 g which explains why in colder climates you see ice floating at the top instead of sinking to the bottom and making sea levels rise more and cause flooding.

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When water freezes the water molecules form a crystal like structure, due to hydrogen bonding, making the structure of ice less dense than that of water.

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The water molecules are tightly bonded together by cohesive forces at the top of an area.

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Little bugs are sometimes able to walk on water because the weight of the bugs are not heavy enough to break to surface tension and fall through.

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We use the density of water to find out if something would float in water for example if you have ever noticed that ice cubes float to the top of water in a glass instead of sinking

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Water molecules at the surface have a stronger bond to each other than the ones below it.

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the degree of compactness of a substance