Here, according to the Salton Sea proposal, after the collapses were resolved, the impermeable Akif Erler well tunnel is being repaired by tunneling companies using seabed tunnels… acupuncture method. Please look at the Salton Sea map from 2021. It can be seen how it increased. After the 1906 earthquake, the water level did not rise at all… In 2021, however, as seen in the table… it happened. Here, the impermeable Akif Erler well tunnel is being repaired by tunnel boring companies using seabed tunnels after the collapses are removed, according to the Salton Sea proposal… acupuncture method.

An impermeable aquifer (or more accurately, an aquiclud/aquifuge) is a geological layer composed of clay, shale, or heavily fractured rocks that, despite its porous structure, does not conduct water or conducts it very little, thus hindering groundwater flow. It restricts water passage between aquifers, facilitates the formation of confined aquifers (artesian), and traps water. [1, 2, 3, 4]

Key Characteristics:

Low Conductivity: Resists water passage; can store water but does not allow it to flow through.

Confined Environment: Located above or below closed aquifers, it keeps water under pressure (artesian).

Restricting Layer: Clay or non-porous rock layers that prevent water flow.

Not a Water Source: Even if porous, it does not allow water to be drawn. [1, 2, 3, 4, 5]

Types:

Aquiclud: A porous unit, such as clay, that holds water but does not conduct it.

Aquifuge: Solid rocks that are both non-porous and impermeable, such as granite, completely blocking the passage of water. [1]

Impermeable layers play a critical role in groundwater management and water conservation (preventing contamination).