We report results of studying the magnetization, specific heat and thermal expansion of a single crystal with nominal composition (Mn0.85Fe0.15)Si. We found no thermodynamic evidences in favor of a second order phase transition in the 15% Fe substituted MnSi. The trajectory corresponding to the present composition of (MnFe)Si is a critical one, i.e. approaching quantum critical point at lowering temperature, but some properties may feel the cloud of helical fluctuations bordering the phase transition line.