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A: With E:
[tex]\boxed{\begin{array}{cc} \sf \normalsize Lava \: domes \: form \: during \: the \: volcanic \\ \sf \normalsize \: eruptions \: in \: which \: highly \: viscous \: on \\\sf \normalsize \: magma \: accumulates \: in \: the \: \\\sf \normalsize near-vent \: region. \\ \\\sf \normalsize During \: the \: gas \: pressure \: it \: being \: build \\ \sf \normalsize \: up \: in \: the \: lava \: dome \: or \: shallow \: conduit \\ \sf \normalsize \: region \: can \: destabilize \: the \: structure \\ \sf \normalsize \: and \: it \: can \: be \: trigger \: transitions \: to \\ \sf \normalsize \: explosive \: eruptions \: or \: lava \: dome \: it \\\sf \normalsize \: has \: been \: collapse.\end{array}}[/tex]
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