This book provides a reinterpretation of early modern clock and watch dials on the basis of use. Between 1550 and the emergence of a standard format in 1770, dials represented combinations of calendrical, lunar and astronomical information using multiple concentric rings, subsidiary dials and apertures. Change was gradual, but significant. Over the course of eight chapters and with reference to thirty-five exceptional images, this book unlocks the meaning embedded within these early combinations. The true significance of dial change can only be fully understood by comparing dials with printed paper sources such as almanacs, diagrams and craft pamphlets. Clock and watch makers drew on traditional communication methods, utilised different formats to generate trust in their work, and tried to be help users in different contexts. The calendar, lunar and astronomical functions were useful as a memory prompt for astrology up until the mid-late seventeenth century. After the decline of this practice, the three functions continued to be useful for other purposes, but eventually declined.

Traces intertribal trade relations of the Iroquois and the impact Europeans had on this in the seventeenth century.

The Sun is nowadays observed using di?erent techniques that provide an almost instantaneous 3-D map of its structure. Of particular interest is the studyofthevariabilityinthesolaroutputproducedbythedissipationofm- netic energy on di?erent spatial and temporal scales – the so-called magnetic activity. The 11-year cycle is the main feature describing this phenomenon. Apart from its intrinsic scienti?c interest, this topic is worth studying because of the interaction of such processes with the terrestrial environment. A ?eet of space and ground-based observatories are currently monitoring the behaviour of our star on a daily basis. However, solar activity varies not only on this decadal time-scale, as has been attested mainly through two methods: (a) records of the number of sunspots observed on the solar surface from 1610, and (b) the records of 14 10 cosmogenic isotopes, such as Cand Be, measured in tree-rings and i- cores, respectively. The study of the long-term behaviour of solar activity may be comp- mented by the study of historical accounts describing phenomena directly or indirectly related to solar activity. Numerous scienti?c and non-scienti?c d- uments have reported these events and we can make use of them as a proxy of solar activity in past times.