Earth has much water. 

Earth is a blue planet. 

Water can be in the air. It can be under the ground. It is even inside plants and animals. Most of the water is salty. Only a tiny bit is fresh.
Water moves in a circle. Heat from the sun moves water. It turns water into vapor. This vapor goes up into the air. Then it falls as rain or snow.
This water has been here for a long time. It has been around for 4 billion years. The water does not leave the Earth. It just moves from place to place.
We need water to live. It is a basic need for all life. It is a very special part of our world.
The hydrosphere is all the water on our planet. 
Most of Earth's water is salt water. It makes up 97.5% of all water. Only 2.5% is fresh water. Most fresh water is frozen in ice or snow. Only a tiny part is in lakes and rivers. This is the water we can easily use.
Water moves in a set of steps called the water cycle. Heat from the sun moves water. It turns water into vapor. This is called evaporation. Water also moves from snow and ice. This is called sublimation. Trees also let out water through tiny holes. This is called transpiration.
Water has been on Earth for 4 billion years. It is not created or destroyed. It just moves from place to place. 
Humans change the water cycle. We build dams to block rivers. We also use too much water for farms. This can make some water sources run dry.
The hydrosphere is the name for all the water on our planet. 
Water moves through a process called the water cycle. 
Scientists have studied this system for a long time. The word hydrosphere was brought into English in 1887. It comes from a German term introduced by Eduard Suess. We know the hydrosphere has been around for about 4 billion years. Long ago, as the Earth cooled, water vapor turned into rain. This rain filled deep holes in the ground to form our oceans. The first living things actually began their lives in these early oceans.
There is a huge amount of water on Earth. It is estimated that there are 1.386 billion cubic kilometres of water. Most of this is saltwater, which makes up 97.5% of the total. Only 2.5% is fresh water. Most of that fresh water is locked away as ice or snow. Only 0.3% of fresh water is in easy places like lakes and rivers. The total mass of the hydrosphere is about 1.4 x 10^18 tonnes.
Even though there is much water, humans change how it works. We build dams that block and redirect the paths of rivers. We also take water from underground sources like the Ogallala Aquifer in the United States. This can cause some water sources to run dry. Some water, like deep groundwater, can take 1,500 years to refill. Other water, like rivers, can recharge in just 16 days. It is important to remember that water is a basic necessity for everyone.
The hydrosphere is the combined body of water found on, under, and above the surface of a planet. On Earth, this system includes oceans, seas, lakes, rivers, and streams. It also encompasses groundwater, soil moisture, and permafrost within the Earth's crust. Even the water vapor, droplets, and crystals in the air are part of this system. 
Water moves through a continuous process known as the water cycle. This cycle transfers water between different reservoirs, such as the atmosphere, oceans, and groundwater. Solar energy, provided as heat and light, drives much of this movement. Gravity also plays a vital role in moving water back to the surface. Most evaporation occurs from the oceans, returning water to the atmosphere. Water can also move through sublimation, which is evaporation directly from snow and ice. Additionally, trees release water through tiny pores called stomata in a process called transpiration. Hydrologists use the term evapotranspiration to describe these three processes—evaporation, sublimation, and transpiration—working together.

History shows that the hydrosphere has been a changing part of Earth for about 4 billion years. The word itself was brought into English in 1887. It is a translation of the German term *hydrosphäre*, which was introduced by Eduard Suess. Scientists believe the oceans formed as the early Earth cooled. Initially, the atmosphere was thin and rich in hydrogen and helium. As the planet cooled, water vapor released from volcanoes and the cooling Earth condensed. This vapor fell as rain, filling depressions on the surface to create the oceans. This process likely occurred around 4,000 million years ago.
Understanding the scale of the hydrosphere requires looking at specific measurements. There are an estimated 1.386 billion cubic kilometers of water on Earth. The oceans cover about 361 million square kilometers of the surface. The average salinity of these oceans is about 35 grams of salt per kilogram of seawater. The turnover of water is also a massive process. Every year, 577,000 km³ of water evaporates from the ocean and land. This is balanced by 577,000 km³ of precipitation falling back to Earth. This movement ensures that water is constantly migrating through the system.
The hydrosphere is part of a closed system. This means that while water moves and changes form, the total amount of water on Earth has almost certainly not changed since geological times. Water is neither created nor destroyed; it only migrates between reservoirs. This system is deeply connected to the biosphere, where the first life forms began in the oceans. Early organisms did not breathe oxygen, but later, the evolution of cyanobacteria changed everything. These organisms began converting carbon dioxide into food and oxygen, which fundamentally altered the composition of the atmosphere.

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