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Surface tension The top molecule on the water forms a skin that will support dust small creatures and even metal objects like needles when they are place on the surface carefully.

Surface tension keeps the water strider afloat, and the water strider long legs only pierce the top skin of the water. A lso, the water strider mass is very little which results in them floating.

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14y ago
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1w ago

Water striders can float on the surface of the water due to their low weight and the surface tension of the water. Their long, hydrophobic legs help them to spread their weight and distribute it, allowing them to stay on the water's surface without sinking.

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Q: Why dont water striders sink?
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What kind of food do water striders eat?

Water striders primarily feed on small insects that fall onto the water surface, such as mosquitoes, flies, and other aquatic insects. They use their long forelegs to capture and consume their prey.


What are the adaptations for water strider?

Water striders have adaptations such as hydrophobic hairs on their legs that trap air, allowing them to float on water's surface tension. Their long legs help distribute their weight and prevent them from breaking the water's surface. Additionally, their bodies are streamlined and lightweight, enabling them to glide effortlessly on the water's surface and capture prey.


How do water striders walk on water?

Water striders use their long legs and low body weight to distribute their weight over a large surface area, allowing them to effectively "skate" on the water's surface tension. This surface tension is created by the cohesive forces between water molecules, which are strong enough to support the water strider's weight without breaking. Their specialized hydrophobic legs also help repel water, preventing them from sinking.


How does the global conveyor belt form?

The global conveyor belt is formed by a combination of surface and deep-ocean currents. It starts with cold, dense water sinking near the poles, which then flows along the ocean bottom towards the equator. This deep water eventually rises back to the surface in regions such as the North Atlantic, creating a continuous loop of circulation.


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