ya that is right
When minerals containing iron are exposed to air and water, they can undergo a chemical reaction known as oxidation. This leads to the formation of iron oxide, commonly known as rust. Rusting can degrade the mineral, causing it to become weaker and eventually break down.
Type your answer here... Water from springs containing minerals.
oxidation
Oxidation in chemical weathering causes minerals containing iron to rust or oxidize when exposed to oxygen in the presence of water, resulting in the breakdown of the minerals and alteration of the rock. This process can lead to a reddish or orange color developing in the affected rocks or minerals.
Hydrothermal springs / hydrothermal water.
He had to get oxygon from a gas tank
Acidic water can leak out of mines when it comes into contact with exposed rocks containing sulfide minerals. Through a natural process called oxidation, these minerals react with water and oxygen to produce sulfuric acid, which then flows out of the mine along with other dissolved metals. This acidic water can have negative impacts on the surrounding environment by contaminating water sources and harming aquatic life.
Yes, chlorine can evaporate from water. When water containing chlorine is exposed to air, the chlorine can escape into the atmosphere as a gas.
One type of chemical weathering is oxidation, where minerals containing iron are exposed to oxygen and water, causing the iron to rust and the rock to weaken and break down.
Evaporites are a type of sediment that form from minerals crystallizing from water. This process occurs when the water containing dissolved minerals evaporates, leaving behind the minerals in solid form. Common examples of evaporites include gypsum, halite, and calcite.
Because when it floods, the water (containing minerals) seeps into the ground, and the ground is then has far more minerals then usual. When the water flows / drains away, the minerals are left and the land is very fertile.
The plant needs water, air and soil containing all necessary minerals.