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GALÁPAGOS ISLANDS

GALÁPAGOS ISLANDS

Why in News?

According to a recent study, Cold ocean currents have sheltered the Galápagos Islands from global warming.

The Galapagos Islands, spread over almost 60,000 sq km, are a part of Ecuador. These are located in the Pacific Ocean around 1,000 km away from the South American continent.

Protection Status:

Ecuador made a part of the Galapagos a wildlife sanctuary in 1935, and the sanctuary became the Galapagos National Park in 1959. In 1978, the islands became UNESCO’s first World Heritage Site.

Wildlife:

It contains aquatic species such as manta rays and sharks which have been endangered by commercial fishing. It also hosts a wide array of aquatic wildlife, including marine iguanas, and waved albatrosses. Galápagos is home to the critically endangered — Galápagos penguin, Galápagos fur seal and Galápagos sea lion. Also, the giant tortoises found here – 'Galápagos' in old Spanish – give the islands its name.

Significance:

The British naturalist Charles Darwin made key observations in 1835 that shaped his theory of evolution. Darwin described the islands as a “world in itself”. Corals do not bleach and die in these waters off the west coast of Ecuador.

Ocean Currents - Ocean currents are the continuous, predictable, directional movement of seawater. It is a massive movement of ocean water that is caused and influenced by various forces. They are like river flows in oceans.

Factors that Influences Ocean Current

• Heating by solar energy: Heating by solar energy causes the water to expand. That is why, near the equator the ocean water is about 8 cm higher in level than in the middle latitudes. This causes a very slight gradient and water tends to flow down the slope.
• Wind: Wind blowing on the surface of the ocean pushes the water to move. Friction between the wind and the water surface affects the movement of the water body in its course.
• Gravity: Gravity tends to pull the water down the pile and create gradient variation.
• Coriolis Force: The Coriolis force intervenes and causes the water to move to the right in the northern hemisphere and to the left in the southern hemisphere.
• Differences in Water Density: Water with high salinity is denser than water with low salinity and in the same way cold water is denser than warm water. Denser water tends to sink, while relatively lighter water tends to rise.
• Temperature of Water: Cold-water Ocean currents occur when the cold water at the poles sinks and slowly moves towards the equator. Warm-water currents travel out from the equator along the surface, flowing towards the poles to replace the sinking cold water.
• Differences in Water Density: Water with high salinity is denser than water with low salinity and in the same way cold water is denser than warm water. Denser water tends to sink, while relatively lighter water tends to rise.
• Temperature of Water: Cold-water Ocean currents occur when the cold water at the poles sinks and slowly moves towards the equator. Warm-water currents travel out from the equator along the surface, flowing towards the poles to replace the sinking cold water.