The present analytical study on the non-Darcian effects on natural convection from a vertical plate embedded in a high-porosity medium shows that the boundary and inertia effects have a significant influence on the velocity profiles and surface heat transfer rate. Both effects are more pronounced in high-porosity media and reduce heat transfer from the heated plate. The boundary effect becomes more noticeable in the region close to the leading edge of the heated plate, while the inertia effect increases with downstream locations on a heated plate. The results also show that as the resistance due to the solid matrix increases, the velocity profile tends toward the conventional exponential form, which results from velocity slip at the boundary.