Depth of groundwater table is unknown

Hello everyone!

I am trying to conduct the flow-deformation analysis for slope stability assessment under transient boundary conditions. However, the problem is that at the study site, we do not know the depth of the groundwater table. We are assuming that the groundwater table is quite deep based on the fact that there was no evidence of groundwater at the landslide when it occurred. Can anyone please suggest the best way to tackle such a situation?

Thank you in advance.

Best Regards,

Sam