Members of the Institute for Gravitational Research (IGR) and the School on Engineering have published an article in Nature titled: “Measurement of the Earth Tides with a MEMS Gravimeter”. The Earth tides are the elastic deformation of the Earth caused by the changing phase of the Sun and the Moon, and the Glasgow microelectromechanical system – or MEMS - is the first such device to measure this phenomenon (see figure 1). This measurement was possible because the device has an incredible stability compared to existing MEMS accelerometers or seismometers. Consequently it is the first MEMS accelerometer that can be classed as a gravimeter. The MEMS device is etched from a single piece of silicon and consists of a central proof mass suspended from three arched anti-springs (see figure 1). The proof mass moves in response to changing gravitational acceleration and the motion is monitored using a simple optical shadow sensor (see figure 2). The combination of the soft springs, the heavy proof mass, and the accuracy of the motion sensor allows the device to measure changes in little g of 40 parts per billion in an integration time of 1 second (40 μGal/√Hz).