Volcanoes associated with midocean ridges have lava that is:

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Volcanoes associated with midocean ridges have lava that is fluid with little gas and mafic. This is because midocean ridges are places where two tectonic plates are moving apart, allowing magma to rise from the mantle and form new crust. The magma is typically mafic, meaning it has a low silica content, which makes it less viscous and more fluid. Additionally, there is less gas in mafic lava compared to felsic lava, which tends to be more explosive due to its high gas content.

Volcanoes Associated with Midocean Ridges Have Lava That Is