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Focusing on the Eastern Adriatic region, from Zadar in the north to Corfu in the south, the background information supporting our knowledge of the seismicity in the time-span 14th to early 19th centur...
This paper is a comparative study of the three strongest 19th century earthquakes in Mexico and their effects and impact mainly in Mexico City. The research is based on historical sources and previous...
The Dead Sea Fault and its junction with the southern segment of the East Anatolian fault zone, despite their high tectonic activity have been relatively quiescent in the last two centuries. Historica...
Many seismological observatories began to record and store seismic events in the early years of the twentieth century, contributing to the compilation of very valued databases of both phase pickings ...
The Italian earthquake catalogue is considered to be fairly complete starting from the 17th century and for classes of earthquakes of magnitude greater than 5.5. However, dedicated historical researc...
Culture in Catalonia and, specifically, science had an important rebirth in the second half of the 19th century. But, due to the lack of State support, development of earth physical sciences in Catalo...
Giovanni Santini was appointed director of the Astronomical Observatory of Padova from 1817 to 1877. His scientific correspondence covers a period from 1807 to 1874. Most of the letters are from Itali...
The paper describes Finnish attempts to understand phenomena in the near Earth space by using ground-based observations and later observations from space. The geophysical observatories and networks o...
In this paper we discuss the development of the seismological instrumentation, the facilities for seismological research and the most important or the pioneering studies in the different branches of t...
The development of non-seismic aspects of solid Earth geophysics in Finland is described along five major lines: geomagnetic research at observatories, applied geophysics to assist mineral prospectin...
The Earth was considered to be a sphere until the end of the 17th century. Only then, the concept of an Earth flattened at the poles was beginning to gain support among scientists. A powerful influe...

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