Des porte-parole protestants au chevet de l'édit de Nantes moribond

This article shows how the Edict of Nantes (1598), that had been criticized by French Protestants when it came out, progressively became the symbol of their belonging to the French nation and the acceptance of their religious particularity. But it is finally after its revocation (1685) that this Edict appears to make most sense to the Huguenot spokesmen. Thinking from a theological point of view as well as an historical, juridical and philosophical one, they consider it as a symbol of religious freedom. However, it is only by giving up their former status lost with the Revocation that they manage to develop an original thinking on the relationship between the State and individuals. In order to achieve this, they must distinguish between the subject or the citizen on one hand, and the believer on the other. But this distinction implies the renunciation of the nostalgia for aProtestant body, recognized as such in the kingdom of France.     

The significance of pockmarks to understanding fluid flow processes and geohazards

Underwater gas and liquid escape from the seafloor has long been treated as a mere curiosity. It was only after the advent of the side‐scan sonar and the subsequent discovery of pockmarks that the scale of fluid escape and the moon‐like terrain on parts of the ocean floor became generally known. Today, pockmarks ranging in size from the ‘unit pockmark’ (1–10 m wide, < 0.6 m deep) to the normal pockmark (10–700 m wide, up to 45 m deep) are known to occur in most seas, oceans, lakes and in many diverse geological settings. In addition to indicating areas of the seabed that are ‘hydraulically active’, pockmarks are known to occur on continental slopes with gas hydrates and in association with slides and slumps. However, possibly their potentially greatest significance is as an indicator of deep fluid pressure build‐up prior to earthquakes. Whereas only a few locations containing active (bubbling) pockmarks are known, those that become active a few days prior to major earthquakes may be important precursors that have been overlooked. Pockmark fields and individual pockmarks need to be instrumented with temperature and pressure sensors, and monitoring should continue over years. The scale of such research calls for a multinational project in several pockmark fields in various geological settings.