Clarification of my statement regarding the Hoek-Brown criterion - this is a method of rock mass shear strength estimation with rock mass being defined as whole rock inclusive of joints and intact rock. The "rock mass" concept is used to downgrade the shear strength from intact rock free of joints in an attempt to account for weakening due to jointing. Note the following shear strength relationship: intact rock >> rock mass > joint strength.
In other words if you do a uniax test on a core of solid rock, then you'd get a very high strength on the order of 100MPa. However, because of the effect of joints (not necessarily daylighted) it is impossible to mobilise strengths of this magnitude. Hence, the rock mass concept. Using the HB method, the intact rock strength is downgraded empirically using GSI which is an index of rock quality. There are other factors as well. The method was developed for analysis of high stress environments primarily in mining where excavations are large and deep. It is not the only method of rock mass shear strength estimation by the way.
For a 25m excavation, stresses are relatively low in comparison with typical rock mass strengths. Another way of saying this is that rock mass failure for a 25m slope is very unlikely to happen unless the rock is altered and very soft. At 25m, the max normal stress is about 0.5MPa - a pittance in comparison with typical rock strength! Sliding along joints (discontinuities, foliation, bedding, faults, etc.) is therefore the mode of failure that is important.
A good start would be to map the joints, measure the orientations, test the shear strength, and do a stereonet analysis.