"Larger than if it cools quickly" is about all that's definitively possible to say.
cools slowly.
crystal
Cooled slowly underground the pseudo crystals of columnar basalt, such as the Giants Causeway in Ireland may be in a metre size range.
the crystals are large
It is mineral
if lava cools slowly, it will have a lot of crystals. When it cools fast, there will be little to no crystals what s ever.
Large crystals with a coarse crystal grain texture.
The rate at which magma cools determines the size of the mineral crystal.
large ones
Not enough information. Some crystals will break if they cool rapidly, some crystals will not form correctly if the solution cools too quickly.
Overall mineral crystal size depends on how fast a solution cools. Slower cooling allows more time for mineral crystals to grow larger, while rapid cooling results in smaller crystal sizes. Additionally, the chemical composition of the solution and the presence of impurities can also influence crystal size.
The size of the crystals in igneous rocks depends on the cooling rate of the magma or lava. When magma cools slowly, typically beneath the Earth's surface, larger crystals form due to the longer time allowed for crystal growth, resulting in intrusive igneous rocks like granite. Conversely, when lava cools rapidly on the surface, smaller crystals form, leading to extrusive igneous rocks like basalt. Thus, the cooling rate directly influences the texture and crystal size of the resulting rock.