The Need for Vibration-Free Cryogenics The measurement of local gravitational fields requires continuous, high precision and extremely stable measurements. In 1968, the development of the superconducting gravity meter (SG)[1] vastly improved the state of the art. In contrast to mechanical quartz or metal springs, SGs use a superconducting sphere levitated in an ultra-stable magnetic field generated by persistent currents in a pair of superconducting coils. This cryogenic design enabled sensitivities that can exceed 10-10 m/sec2 (i.e., 0.01 ppb of the earth’s gravitational field) and drifts less than 60 nm/sec2/year. Many gravity measurements (hydrology, volcanology, geothermal energy and postglacial rebound) require durations that last years, and, in many cases, decades. To fulfill this need, extremely long hold time cryostats were developed to maintain the SG at operational temperatures close to 4 K. Special techniques were also developed to prevent cryocooler-induced accelerations from contaminating the geophysical signals of interest. While most superconducting quantum interference device (SQUID) measurement systems[2] do not require multiyear measurement times, they benefit from improved cryogenic systems that minimize or eliminate the expenditure of liquid helium.