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France most commonly records the date using the day-month-year order with an oblique stroke or slash (”/”) as the separator with numerical values, for example, 31/12/1992. The 24-hour clock is used to express time, using the lowercase letter "h" as the separator in between hours and minutes, for example, 14 h 05.
Short-term forecasts tend to use seismic or multiple monitoring data with long term forecasting involving the study of the previous history of local volcanism. [ 13 ] : 1 However, volcanology forecasting does not just involve predicting the next initial onset time of an eruption, as it might also address the size of a future eruption, and ...
The word volcanologist (or vulcanologist) is derived from the English volcanology (volcano + -logy), which was derived from the French volcanologie (or vulcanologie), which was further derived from the French word volcan (volcano), which was even further derived from Vulcanus, the Latin name of the Roman god of fire and metalworking.
French phonology is the sound system of French.This article discusses mainly the phonology of all the varieties of Standard French.Notable phonological features include the uvular r present in some accents, nasal vowels, and three processes affecting word-final sounds:
French orthography encompasses the spelling and punctuation of the French language.It is based on a combination of phonemic and historical principles. The spelling of words is largely based on the pronunciation of Old French c. 1100 –1200 AD, and has stayed more or less the same since then, despite enormous changes to the pronunciation of the language in the intervening years.
lit. "present yourself" or "proceed to"; a meeting, appointment, or date in French. In English, it generally endorses a mysterious overtone and refers to a one-on-one meeting with someone for another purpose than a date. Always hyphenated in French: rendez-vous. Its only accepted abbreviation in French is RDV. reprise
Name Elevation Location Last eruption m ft Coordinates; Chaîne des Puys: Puy de Côme: 1252: 4108: 5760 BC Puy de Dôme: 1464: 4803: 8700 BC Puy de Lassolas: 1183: 3881
Phreatomagmatic ash is formed by the same mechanisms across a wide range of compositions, basic and acidic. Blocky and equant clasts with low vesicle content are formed. [2] ...