We investigate in detail the low-temperature structural and physical properties of the trilayer nickelates (, Pr, and Nd), which crystallize with a monoclinic symmetry (space group ) and undergo a metal-to-metal transition (MMT) near = (Pr), and (Nd). Using a high-resolution synchrotron powder x-ray diffraction technique, we show that the lattice parameters in all cases exhibit an anomalous behavior at , however, without any sign of change in the lattice symmetry. Unambiguous signature of MMT is also observed in the magnetic and transport data, suggesting a strong coupling between the electronic, magnetic, and structural degrees of freedom. Analysis of thermal expansion yields hydrostatic pressure dependence of MMT in close agreement with previous high-pressure experiments. In , the ions located in the rocksalt (RS) layers order magnetically near , which is significantly suppressed compared to . In contrast, ions in the perovskite-block (PB) layers exhibit a crystal field (CF) induced nonmagnetic singlet ground state. In , on the other hand, the CF ground state of ions in both RS and PB layers is a Kramers doublet. The heat capacity of shows a pronounced Schottky-like anomaly near , and a sharp upturn indicating short-range correlations between the Nd-moments below . However, no signs of long-range ordering of Nd-moments could be found down to despite a sizable value of . The strongly suppressed magnetic long-range ordering in both and Nd suggests the presence of strong magnetic frustration in these compounds. In the presence of an overwhelming Schottky contribution, the electronic term in the specific heat of and appears highly inflated, which can be falsely interpreted as a sign of heavy fermion behavior as is done in a recent study on . Accordingly, the low-temperature resistivity of these compounds is found to follow a rather than a dependence.