“…While gabbros and mantle rocks are well exposed along the Wadi, basalts, and sheeted dikes are generally only present as small hills within the lower Wadi plain. Based on field observations and structural data (Mock, Ildefonse, et al., 2021), the profile can be divided into the following units (from top to bottom): Axial melt lens, AML, ∼5.0 km h.a.M. (height above the mantle‐crust transition zone, for calculation of h.a.M., see Section 2.1), Varitextured gabbros, VG, ∼4.1–5.0 km h.a.M., Upper foliated gabbros, UFG; ∼3.5–4.1 km h.a.M., Lower foliated gabbros, LFG, ∼2.6–3.5 km h.a.M., Layered gabbros, LG, ∼0.2–2.6 km h.a.M., mantle‐crust transition zone, MTZ, ∼0–0.2 km h.a.M.…”