The subduction of the Cocos Plate under the North America Plate define
s a high risk seismic zone along the Pacific coast of Mexico. A seismi
c gap has been identified at the Guerrero State as a place where a lar
ge earthquake, up to M(S)=8.2, can occur within the next years. In thi
s area an in-soil radon network, consisting of fixed SSNTD monitoring
stations, has been operated during several years on a monthly exposure
basis. A continuous radon probe that registers data on a short term b
asis is also operating since recently. The results of the two radon de
tection systems are compared and discussed as a function of the local
seismic activity observed at the Guerrero coastal zone.