2. Deep-sea waters are underground waters appearing
deeply below the surface of earth, separated from it
entirely. They aren't renewable. As a rule they have a
high mineralization and on that account aren't sending
at consumer targets themselves. They are often salted.

3. Types of deep-sea waters depending on their genesis:
relict - originating from former geological eras:
sedimentary - ancient waters infiltracyjne, imprisoned in consolidated settlements,
infiltracyjne - imprisoned in rocks in past geological eras to the effect e.g. of mass
movements,
juwenilne - waters aftermagma coming from the condensation of steam being
released from exhalation volcanic;
metamorphic - coming into existence in processes of transforming rocks.

4. Surface water is water on the surface of the planet such as in
a stream, river, lake, wetland, or ocean. It can be contrasted
with groundwater and atmospheric water.
Non-saline surface water is replenished by precipitation and by
recruitment from ground-water. It is lost
through evaporation, seepage into the ground where it becomes
ground-water, used by plants for transpiration, abstracted by
mankind for agriculture, living, industry etc. or discharged to the sea
where it becomes saline.

5. Groundwater is the water located beneath the earth's surface
in soil pore spaces and in the fractures of rock formations. A unit of
rock or an unconsolidated deposit is called an aquiferwhen it can yield a
usable quantity of water. The depth at which soil pore spaces or
fractures and voids in rock become completely saturated with water is
called the water table. Groundwater is recharged from, and eventually
flows to, the surface naturally; natural discharge often occurs
at springs and seeps, and can form oases or wetlands. Groundwater is
also often withdrawn for agricultural, municipal, and industrial use by
constructing and operating extraction wells. The study of the
distribution and movement of groundwater is hydrogeology, also called
groundwater hydrology.

6. Typically, groundwater is thought of as liquid water flowing through
shallow aquifers, but, in the technical sense, it can also includesoil
moisture, permafrost (frozen soil), immobile water in very low
permeability bedrock, and deep geothermal or oil formation water.
Groundwater is hypothesized to provide lubrication that can possibly
influence the movement of faults. It is likely that much of the Earth's
subsurface contains some water, which may be mixed with other fluids
in some instances. Groundwater may not be confined only to the
Earth. The formation of some of the landforms observed
on Mars may have been influenced by groundwater. There is also
evidence that liquid water may also exist in the subsurface of Jupiter's
moon Europa.

7. GROUP 1
Anna Woszczyk - Poland
Maja Gewald -Poland
Natalia Baczewska - Poland
Noelia Afonso Martín - Spain
Gorka Arnay Esteban - Spain
María Samara Ascanio Castro - Spain
Lucía Castañeda Benites - Spain
Andrea Candelaria Domínguez Medina - Spain
Adil José El Founti Afonso - Spain
Philip - Germany