Terraqueous Globe were of one uniforme superficies as wee may perceive that in wide Seas their motions are farr less irregular then by Land since the great diversity of Climates Mountains and Lakes varies them exceedingly I have thus farr discours'd of the 4 Principall the Collaterall or Intermediate VVinds if any right judgment could be made of their natures from the Quarters whence they blow might be suppos'd Hot Dry Moist c. as they are farther remov'd or hang nearer towards the Cardinal Point But we are like to expect little satisfaction from the generality of writers concerning the temperature of VVinds For who can with patience hear the impertinence of those Notionall men that enquire no further but declare That the South Wind is allways Hot and Moist the North Cold and Dry the West c. which obliges us in the following discourses to offer at some more accurate account of their Qualitys and the most Universall causes from whence they proceed First VVinds are Moist either because their Constituent parts are made up of Vapid and Aqueous corpuscles such as rain dews watry Clouds or by reason they make long Voyages by Sea or over great Lakes Morish Countrys Fenns and so are tainted with the Qualitys of the Medium through which they passe Those which proceed from Melted Snows have some small allay of the Terrene but approach neerer the Moist The Siccity of VVinds is from their Saline and Terrestriall parts or that arriving from those Parc'ht and Torrid regions neer the Line they are exsiccated as they travell by the Ways of the Sun I shall not dispute whether this has been cautiously enough minded by most writers How many nice circumstances are to be consider'd in judging the Qualitys of VVinds and how difficult it is to make a just Estimate of their severall degrees of Heat and Cold. For there must not only be especiall regard had to the Temperament of our Senses but to the Climes in which they blow and seasons of the year Since those which would seem hot at Christmas comparatively to the winter Cold should the same happen in July when wee had been long accustom'd to a different temperature of our Organs and the Ambient Air would undoubtedly appeare exceedingly Cold. Then wee denominate VVinds either Gelid or Hot in respect of those that usually blow in such Climats as the Southern Blasts with us here in England though they are Colder then the Ambient Air may be reputed Hot comparatively to the N. or N. E. which are much more refrigerative in these parts of the VVorld Thus wee ought not rashly to make judgment of their Qualitys but first consider what Symptoms of Heat they betray in relation to Weather-glasses or the Winds that commonly blow in such Countrys as likewise what mutations happen by them in the Temperature of the Air And afterwards compare all these Circumstances with the present disposition of our Organs least wee determine concerning the positive Qualitys of VVinds from only the Prejudices and Hallucinations of Sense There are severall Causes Productive of Heat As their passage through Hot Regions Or because they consist of the ignite and suffocating Air which infests the Burning Zone where the whole Masse is corrupted with such intolerable heats that the Winds which are either generated therein or only pervade the Torrid regions must needs for some time retain their temperament and Qualitys till at length they loose them in long voyages and the calorifique particles languish and dwindle away by degrees being oppres'd with multitudes of Heterogeneous exhalations in their course Then I think it not improbable but that the Solar rays or whatever parcells beside of the Subtil and Aetheriall matter may by mingling with them actually advance the heat of VVinds. And Lastly The ignite Damps such as wee sometimes discover in Colepits and Mines and all other of the Minerall and Metalline Kingdomes that finding no Vent cause Earthquakes in the Bowells thereof if they escape through the Pores of the Earth occasion Presters and Hot VVinds And those fiery eruptions which in many places of Calabria and Sicily are continually breathing out from the Subterraneall Regions must needs diffuse the seminals of heat through the whole body of the Air and VVinds especially such as come reaking from under Burning Mountains or at least are the results of those Calorifique mixtures by which some Mineralls and salts fermenting together in the Cavitys of the Earth emit Hot fumes Like severall Chymicall preparations such as Oyl of Tartar and spirit of Vitriol which cause a strange Ebullition and Heat by their commistion only And if wee suppose any thing Analogous to these under ground where Nature in her own Elaboratory often exceeds the greatest Sagacity of Art why may not the Tepid Steams and Vapors that ascend from thence be able to produce so considerable a degree of Heat in the Air that might occasion Scorching Winds And happily the Rancounters of Certain Mineralls with each other in those Passages where the VVaters flow may likewise by their mutuall ferments be the most probable cause of many Hot Baths Springs Neverthelesse Fromundus some other Naturalists of late in the Number of which wee may reckon our Countryman Mr. Hobs affirme that all VVinds whatever doe actually refrigerate and oftentimes so intensly that they prove the fittest instruments for the Congelation of Liquids And I must confesse it seldome falls under our observation that in any parts of Europe the VVinds are comparatively hotter then our Sensories or the Ambient Air yet in many Provinces of Afric Arabia but most of all near the Persian Gulf where they come just off from the Burning Sands they are intolerably hot and suffocating as appears from the Relations of the Portugalls first Voyages to the East Indies where they felt Gales of the E. and N. E. Wind so Hot that the Air seem'd to be inflam'd and scorching like fire So likewise Gasparo Balbi in his Travells speaks of four persons that weary'd in their Journy sat down near the Banks of Euphrates to refresh themselves a while and were all stifled by one of these Hot Winds And wee have a more surprising Narrative from Marcus Polo that when the King of Chermain sent an Army of 16 Hundred horse and 5 thousand foot against the Lord of Ormus for not paying his Tribute they all perisht by these Suffocating Blasts But if wee distrust the integrity of these writers Olearius in his Voyage to Persia describes the intemperature of the Air in those Countrys to be such that with the North or East Wind they felt a Cold which depriv'd them of their Limbs and on the Contrary the S. Winds were ready to choak them with the extremity of heat But Della Valle a Nobleman of Rome whose Curiosity led him through most of the Eastern Kingdomes reports that towards Arabia there was a VVind so scorching and Dry that it left behind it like marks of Fire wherever it came
Sun 71. Where to be expected on this side the Tropique 78. The Variation thereof in severall Longitudes 79. Why the Westerly Winds blow most commonly without the Tropiques 86. The Provinciall Winds 90. A discourse concerning the Terrheinos and Viracoins or the Land and Sea-Brises 92. Their History and Cause 93. c. When they come in or cease in the Straights on the Coasts of Guiny the East and West-Indies and what Accidents hasten or retard their approach from p. 99. to 110. Of the Etesian or Anniversary Winds their severall species 111. 112. c. Of the Anniversary Winds in the way to the East-Indies which they call the Monsoons 119. How many months they continue the same Course on the Coasts of Africk and India 121. The Changing or Breaking up of the Monsoons 122. A Discourse concerning the Qualities of Wind p. 131. deriv'd from their Constituent Parts or the Medium through which they passe 131. Some Tryalls for the Explication of this Phaenomenon 133. 134. c. The Great incertainty of these observations and the diversities of their Qualities in severall Climates 138. The Properties of Easterly Winds Vnwholesome in most parts of Europe and yet in America very agreeable and pleasant 141. Of the South Winds 142. Why they magnify Visible objects and cause a stammering in the speech 147. Of the Westerly Winds their exceeding violence in the Isle of Jersy and Coast of Cornwall 150. Of the North Winds their wonderfull impetuosity in Norwey and Island 161. The great Caution to be us'd and what Circumstances are to be consider'd in judging the Qualities of Winds 172. 173. The causes of Hot Winds 174. 175. The Extremity of their Heat toward the Persian Gulf and severall instances of other Scorching Winds in Afric and Arabia where they blow off from the Sands 178. 179. The causes of Cold Winds 181. 182. The sea-Sea-Winds in the Temperate Zones hotter then those which blow over the Land 187. Instances of this Nature in Great Britain the Isle of Jersy Virginia Florida and several other places 188. 189. c. Yet in the Torrid Zone the Sea-Brises cooling and pleasant examples thereof in America 191. Some Unusuall Qualities of Wind. 194. Of the Harmetans in Guiny 195. 196. The Virulent and Destructive Qualities of certain Winds in the West-Indies 201. Some Proposals for a more Accurate Discovery of the Nature and Qualities of Winds in relation to Architecture Navigation and severall Trades and Mechanicall Arts from 209. to 222. Diverse Prognostiques of Wind. 223. Of Whirlwinds in Generall 229. Their severall species 231. Concerning the Tornados a Description of their Nature 236. 237. How many degrees they are to be expected on this side the Aequinoctiall and at what time of the year 246. Most towards the Coasts of Guiny 247. The Tempests near the Cape Bon Esperance 245. The Cause of the Tornados 249. The Presters or Fiery Whirlwinds Examples thereof 251. 254. Hurricanes Some conjectures concerning their cause 257. The Places where they happen 265. 266. Their Prognostiques and Description in diverse Historicall Relations from 269. to 292. c. THe Origines of Winds are no lesse Various then their Motions we ought not to determine positively concerning those Appearances in nature which may be rationally explicated severall ways Though we consult the Placits of the learned Ancients consider also what we owe to the improvements of latter times yet I question whether any Theory was ever yet started on this Argument which will adequately resolve the whole Phaenomenon of VVinds and we must never expect to confine their Originall to any one determinate Cause Most of the Graecian Philosophers agreed in the same Definition of Wind till the Prince of the Peripatetiques was not only ambitious to establish a New Hypothesis of his own but likewise undertook the confutation of his Master Plato the rest of his Predecessors The Philosophicall Monarch thought he could never raign securely in the minds of men unlesse like the Family of the Ottomans he destroy'd all his Bretheren first I have no intention to disparage the Authority of the Ancients but I cannot be so injurious to the many noble productions of our present Age to think that all Science is only to be sought for in the Urns of the Dead we have a more intimate converse with Nature then heretofore which displays her beautifull Bosome and every day affords new Discoveries of usefull knowledge and further conducing to the Benefit of Human life If we consider the successe that Philosophy has met with in the VVorld we shall find that those Opinions which obtain'd most in one Age had their Fatall Periods were as much exploded decry'd in the next it 's as impossible that any one Hypothesis should be calculated to the Gusto of all persons when the sentiments of men are different as their complexions I have therefore taken a larger compasse then the Generallity of writers and deriv'd the Origines of Winds from severall Causes which I rather endeavour to prove from Accounts of our Sea-Voyages and relations of Matters of Fact then to refine on them by any nice speculations of my own For this Philosophy is not to be had in Colleges or Books but must be fetch 't frō both Indies we must traverse the wide Seas be tost to as many points of the Compasse as Columbus or Drake we must climb into the Regions of the Air descend into the Caverns of the Earth to detect the innumerable Causes Qualities of VVinds They are diffus'd like the Universall mind and it requires a kind of ubiquity to understand them How small a portion is it of the vast system of the World that we inhabit and how much lesse of it that we comprehend How Extravagant are the Phaenomena of the large American tracts their Tydes VVinds and other Aeriall impressions how different and irreconcileable to Ours How many noble discoverys have been made in these Countries which the Athenian Sages could never think of in their narrow Porches Gardens They might spin fine webs out of their own bowels but for want of a closer inspection into Nature their Texture Materials are slight And we must acknowledge that even the Stagirite himself has left us no very perfect Theory of VVinds though this Province of late years has been more succesfully undertaken by the Lord Verulam Galileo De Cartes and other illustrious Moderns Aristotle constitutes two species of Exhalations the one vapid or moist the other 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 Fumid or Terrene and as the first is employ'd in Rain Hail or Snow c. So the other furnishes materials for Winds c. The Ancients understand no more by wind then a Motion of the Air Anaximander in Plutarch styles it 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 and some others 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 to which that of Seneca may allude Ventus est Aer Fluens But neither the Prince of the Peripatetics ever supposed
them to consist of Earth though it was always to be most predominant nor the Ancients of Air alone without some allay of other Heterogeneous Elements In the 23. Section of his Problems Aristotle himself denominates Wind 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 Aeris impulsum yet in the 2 d book of Meteors he seems rather to reflect this opinion on his predecessors declaring 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 c. cap. 4. So that Aristotle allows not the simple agitation of Air to be reputed VVind wherein he dissents from the Stoics who held it only Motum aut Fluxionem Aeris And there have not been wanting the most eminent moderns who embrac'd their sentiments as Gassendus Beregard Dorisi c. Mr. Hobs defines it Air mov'd in a direct or undulating motion and to this purpose the learned Isaac Vossius Fournier Varenius many others The modern Peripatetics generally agree in an Hot and Dry exhalation repuls't by the Antiperistasis of the middle Region though I find no footsteps of any such opinion in the Text of Aristotle VVind in the most Generall Acceptation is any Sensible Motion of the Air By Air the Vulgar understand almost any invisible Matter whether Rarify'd vapours or Water though it consists of much grosser parts then that which is employ'd in respiration De Cartes computes that Rarify'd Air requires only thrice but Dilated vapours no lesse then 3000 times as much space as before their expansion wherefore in the Generation of VVinds he preferrs them before Fumid Exhalations or Air as in his Definition pag. 153. Venti nihil sunt nisi Moti Dilatati Vapores It seems to me lesse probable whether we reflect on the opinion of Aristotle or Cartesius that Winds should be always made up of Heterogeneous Exhalations distinct from the Body of the Air For certainly they are sometimes no more then Streams or Currents of Air it self shifting from one part of the Atmosphere to another So that the Air while it continu'd placid and calme may be compar'd to a Pond or Lake and when it 's violently agitated and mov'd it resembles a Torrent or River I have already declar'd that no one Hypothesis how comprehensive soever hath yet been able to resolve all the Incident Phaenomena so various are their Efficients and the Matter of which they consist I shall therefore comprise the Locall Origines of VVind under 3 Generall Heads 1. They are generated in the Intermediate space between the Earth and Clouds and that either by Rarefaction or Repletion and sometimes happily by the Pressure of Clouds Elasticall Vertue of the Air c. 2 ly From the Earth or Seas as by Submarine or Subterraneall Eruptions 3 ly By Descension or Resilition from the Middle Region But I shall explain my self how I desire to be understood of all these in the Following Discourses and then descend to the Matter of which they are Form'd their Limits and Qualities c. My Lord Bacon complains that the first species has been too much neglected by most writers while some seek for them in the Clouds and others in the Caverns of the Earth when as they are more frequently generated in the Intermediate Space which they call the Lower Region of the Atmosphere The Universall Efficient of this sort is the Sun the matter Air or whatever Vapourous Effluxions from the Earth Now imagine those Vapours or Fumes that are continually hovering in this Lower Region which being dilated will possesse so many hundred times more space then they did before the expansion to be attacq't by the quick and Penetrating beams of the Sun what a tumult and mutiny must this necessarily cause in the Atmosphere When all places were full before at least the Voids no way Proportionable to the dilatation whither must the ejected particles retire the spaces they should possesse are overstock't already they must be forc'd to send out Colonies to other parts where equivalent compressions and condensations are made where the spaces lye wast and in a manner destitute of Inhabitants But what Seditions Eddies Undulations must this cause in the whole body of the Air How will the Atmosphere fluctuate and be harrast to and fro and as it were curled with waves the Rarify'd vapours still flying to seek new habitations and so doe impell and bear along with them all they encounter in the way some condens'd bodys deserting their Seats and others as farr Expanded hasting to take possession that there can be no tranquillity or rest 'till the influences of the Sun cease or the vapours be exhausted And what is all this Strugling and Commotion of the Air but Wind For either the Dilatation of the former or too great an Accession of New matter will inchoate the collaterall agitation of VVinds as the Lord Verulam experimented from a crosse of Plumes in a Turret closely shut up when meanes were us'd by the evaporation of water to overstock the space and afterwards by Fire to thinne rarify the vapours the Plumes began to tremble by degrees and at last the motion grew rapid Instar turbinis the Water affording multitudes of vaporous steams the Fire resolving them into VVind It likewise appear'd from another of the Verulamian Experiments that Air of it self when other vapours are wanting will be sufficiently Agitated by Rarefaction For though without some other Auxiliary Exhalations Air alone might seeme able to create but a very feoble and languid VVind yet when it 's dilated into at least 60 times the extent it posses'd before the Expansion it must needs by this means crow'd and superonerate the former Spaces and so cause a considerable emotion of the Atmosphere So that if there be much Superfluous Matter and the Protrusion violent it causes storms and Tempestuous VVinds if it be lesse then are only Engendred those mild refreshing Airs such as use to come off from the Banks of Rivers and Ponds at Day-break De Cartes will scarce admit that Dilated Air exceeds above a quadruple proportion yet a person not lesse sagacious in the contemplation of Nature has prov'd in a late discourse that Air without Heat will be dilated to 13000 times the former extent though with it Mersennus never arriv'd to an 100 And questionlesse in the Atmosphere without the assistence of Art we may suppose it Rarefiable by the Heat of the Sun to incomparably larger Dimensions then De Cartes allows it at least sufficient to create very impetuous VVinds which may be occasion'd from any extraordinary expansion of the Air as we usually observe that in great conflagrations it blows manifestly fresher thereabout then it did before the people of Gascoigny at that time subjects to the Crown of England are said to have petition'd the King against the burning of Heath in Sussex Hampshire which afterwards rais'd a VVind very pernicious to their Vines Another cause which generates Wind is the Superoneration of the Atmosphere Democritus other Ancient Atomists supposing if there were too
W. throughout all India from noon till 12 at night and coming out of the Sea towards the Land are therefore call'd Viracoins or Sea Winds They often stay late and blow but slowly Nearer the Coasts of China you have the Terreinhos out of the West and N. W. S. E. and E. N. E. Being in the North they change to the South and then ensues a calme till the Terreinhos come in The Brises in the Straights begin about 9 or 10 in the Morning blowing freshest at noon and so gradually declining till 4 or 5 at last cease in a Calme which lasts till 10 11 or 12 at night VVhen begins the Land Brise till 5 or 6 and then Calme till the Sea Brise comes in This account I receiv'd from a Sea Captain well vers'd in all parts of the Levant having serv'd under the Venetians severall years in those Seas At the river of Constantinople the VVinds commonly blow thorough but in exceeding fair VVeather you shall have both the Land and Sea Brises as in the Straights If either the Easterly or VVesterly VVinds blow fresh they hinder both the Land and Sea Brises in the Mediterranean of which wee must note They are always the more languid and weaker the later they come in In very hot days and when no other VVinds are stirring you may sometimes observe this alternation between the Land and Sea Brises on the Coasts of England but scarce with any certainty beyond the Latitude of Portugal Brises of all sorts are more constant in Summer then Winter and between the Tropiques then in the Temperate Zones The Etesians or Anniversary VVinds are those which blow constantly at certain seasons of the yeare The most remarkable species begin in Summer about the rise of the Dog starre and last 40 days being preceded by their Prodromi or Fore-runners 8 or 10 days The account of Pliny is not much different from Aristotle as he computes their Etesians in the 2 d book of his Naturall History Not only the Stagirite and Theophrastus but of late De Cartes and many other Moderns derive their Origine from the colliquated snows and ice in the Northerly regions For the long continuance of the Sun neer 6 months together above their Horizon at last overcomes the obstinacy of the cold and dissolves the snows which being attenuated into VVinds make long marches towards the South where they find the Air more yielding and pure then the Foggs and grosse vapors of the North. They were call'd the Sleepy VVinds Venti Delicati Somniculares by reason they intermit in the night time and rise again with the Sun happily because the vapors were then only sufficiently dilated by the celestiall beams though in the night time they subside and hover neare the Earth being too refrigerate and dense to constitute VVinds till they are again quicken'd put in motion by the approaches of the Sun I am willing to acquiesce in the aforesaid cause and I believe wee in England or France might owe our Etesians to Groenland and other parts of the Frozen Zones because wee have no constant visible Fountains of any such VVinds in our own dominions but if the Etesians of Greece according to the sentiments of Aristotle doe allways depend on the resolution of snows in the North they would certainly take Russia Poland or Germany in the way which lye neerer the Artick Pole before they arrive at Greece and yet on the other side of the Taurican hills they are said to have Southerly VVinds about the time of the Graecian Etesians VVee may better make judgement of these Winds that being most Peculiar to this Country they were no Forreigners in their Originall but sprung from particular Fountains within it selfe such as the hills of Macedon and Thrace that have perennial Snows of their own and these being master'd by the scorching heats of Summer may give birth to their Etesian Winds which has this advantage over the other opinion that it clears the difficulty why they are silent in the night and blow with fresher Gusts at Midday when the Sun mounts highest in the Northern Hemisphere I shall only adde not to mention severall others of the modern Naturallists that even * Cabeus himselfe who was a person sufficiently Zealous in asserting the Peripatetique Hypothesis dissents from the opinion of Aristotle will scarce allow the Etesians of Greece a remoter Origine then the neighboring Alps. I shall not insist upon the mistake for which some of his own interpreters have severely enough reflected upon Aristotle That he should first deduce the Origine of these VVinds from the Frozen Zones and afterward assign the reason why they blow stronger in the Day time because the liquefaction of the Snows is interrupted by the Nocturnall Cold when it 's Notorious that in those Countrys the Sun for many Months together is never depres'd below their Horizon Towards the Adriatique and many parts of Asia they have Set Winds which arrive from the N. and N. E. Yet all these which were reputed the Venti Stati blow not from the Northerly Points for in Gascony about the same time with the Etesians of Greece they have rather Southerly Winds which Scaliger who was best able to judge of his own Country observes to be unwholesome and Pestilentiall At Madrid for the most part of the Summer they have a Brise from the Pyreneans or the Adjacent Guadarama which extremely allays the excesse of heat You shall have different sorts of Winds from the same Snowy mountain blowing to severall quarters according to the situation of the Countrys As was observ'd in those Countrys by the foremention'd Cabeus Saepe nobis Boreas Borealibus Auster Spirat It being not unusuall for them in Lombardy to feel a Northerly and at Tirol which is situate on the contrary side of the Alps a Southerly Wind at the same time In Italy they can never fail of Etesians from their own Appennines and so happily on the shoare of Guzarat and the Indian Ocean from mount Caucasus And where ever great Chains or ridges of Hills run along as the Caucasean or Appennine this very often renders an account of most Etesians there about Yet I question whether many Authors may not ascribe too much to this one cause for in some places they have Anniversary Winds that can never possibly have their rise from the Resolution of Snows And I believe it would prove extremely difficult to lay down any tolerable Hypothesis of the Monsoons on the Coasts of Afric and India from the best discoverys wee have yet been able to make of those Parts There are other Stated or Anniversary Winds which they call'd 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 Avicular and White-South Winds either because they were so friendly to the procreation of birds or rather that they return'd with Nightingales or Swallows in the spring beginning to blow after the Summer Solstice by the computation of Aristotle 70 days about the beginning
and Pestilentiall but to certain African Provinces healthfull and Pleasant The Northerly are coldest in our European World and the Southerly on the other side of the Aequinoctiall For the Arctick and Antarctick VVinds must needs be of the same nature blowing from either of the Poles where the cold is equally predominant So that the Qualitys of many VVinds seeme not so much to respect the Points of the compasse as the Course of the Sun The Eastern Winds according to Aristotle are hot and dry nor is their Siccity only remarkable in Greece Palestine Asia the Lesse and most parts of Africk where they make long marches over the parcht and barren sands but likewise in the more temperate climes of Holland and France by reason they passe through Poland Germany other vast tracts of Land and lastly arriving at our Isle they can suffer no considerable alteration in their qualitys by so small a passage over the Narrow Seas They are no very welcome guests to us in England being ominous to our Gardens Fields by blasting the corn and fruits I have known strange destruction done in one Night when they come late in the spring Sometimes they not only blite the leaves and blossoms but kill the Trees with their poysonous breath They bring after them swarms of Caterpillers and other devouring insects or those dry and tabid mists which corrupt the lungs and cause Epilepsys Consumptions c. whether by driving before them the putrid Air from Holland or however they contract that malignity in their natures Nevertheless wee can make no Generall conclusions of their propertys from hence which are chang'd by innumerable acidents For though in these Countrys of Great Britain they are inauspicious both to animals and plants yet in the West Indies the Eastern Brise is refreshing and healthfull above all other VVinds. In Arabia and those Asiatique regions they are exceedingly dry by travelling for many thousand leagues over the sandy desarts yet Blondus observes them to be rather humid in Italy and to occasion a relenting in the Air where they blow immediately from the Adriatique Seas In relation to their degrees of heat though Aristotle declares they are much hotter then the Westerly wee find by experience that with us in England the Easterly are at certain Seasons of the yeare exceeding cold and very often the most freesing winds especially if they hang somewhat towards the North. I need assign no other cause for the frigidity of the Easterly Winds then that they have their first rise from the Continent where the Midland Air is much colder then the Maritime The South Winds are generally reputed Hot and Moist on this side the Line being heated in their entry through the Torrid Zone or because they consist not of melted Snows as the Northern but of the Tepid and Sulphury steams from Africk and other Sunburn'd climes They passe over no Seas of any large extent just crossing the Mediterranean and British yet they moisten and relax the Air and cause wet weather by dissolving the Clouds into rain which are rather dissipated and blown over by the impetuous Norths Yet I think it very irrationall to conclude that all the Southerly should have their rise from the Torrid or the Northerly VVinds from the Frigid Zones Since it is not unknown to the Curious that in part of Italy and Provence they have very often Northerly VVinds rising as is suppos'd from some places about the Alps whereof they are not at all sensible in other Countrys of France through which they must of necessity passe if they came so farre North. In like manner at Marseilles and in the Mediterranean they have oftentimes Southerly VVinds when they blow from contrary points on the African Continent which lyes more to the South I believe very few of the South Winds here in England ever took a longer flight then from the Mediterranean Sea or the lower parts of France and it can scarce be suppos'd that the same Numericall Exhalations could ever travell from between the Tropiques and not be spent in the way long er'e they arrive at the British Coasts yet happily by protruding the Ambient Air and that successively the Contiguous to it the motion may at length be Propagated many hundreds of Miles beyond the reach of those vapors which caus'd the first Agitation So that it is not impossible but that a VVind which began neer the Aequinoctiall may by this means be continued even to the Poles of the VVorld However I shall make no longer digressions concerning their Extent but proceed to the Qualitys which are vulgarly ascrib'd to the Southerly VVinds. They are laxative stupefactive and pestilentiall They cause Epilepsies and pains in the head and were therefore styld 〈◊〉 〈◊〉 〈◊〉 〈◊〉 〈◊〉 by the Grecians They render men Shaagrin and melancholy and in some of the Azores Islands the children are said to sit dejected and leave their playing when they blow For first they open the pores of our bodys by their heat and then insinuate the malignant influences and the parts being pointed and volatile have not only an easy ingression into our blood but thaw and unloose the textures of ice and snow Nay it 's most certain that iron it selfe takes the file much better when the South Wind blows then at other times They many times cause a farre rougher Sea then the most Tempestuous Winds from the North Happily because they blow more obliquely and rake the Surface of the Water when as the Northerly oftentimes descend as from a precipice downwards which immediately deads and weakens their force They magnify visible objects As our Seamen observe their ships to appeare bigger at a distance either in misty weather or when the South Wind blows For the humid and nebulous vapors of which they consist distort the visual beams and by refracting them to the Perpendicular cause more rays of light to enter into the eye which makes the object seeme larger then otherwise would arrive at it in strait lines Many who are naturally inclin'd to Stammering in their speech do find their infirmity evidently worse when the Wind is toward the South Probably because the moisture of the Air causeth a greater relaxation of the Nervs and thereby a tremulous and unstable motion of the muscles at that time Which perhaps hath more power upon the Vocall muscles then others because they lye in the Road and are more expos'd to the invasions of whatever is breath'd in at the mouth or nostrills then others are Whence also wee find the tongue more apt to falter though somewhat in a different manner whensoever it is overmuch bedew'd with strong and vaporous liquors Smells are said to be most Fragrant in these Winds when the Air is humid and lax to convey the odoriferous particles They anticipate the Spring and cause the trees to blossome and bud forth before their time and by this means exhaust their spirits and nutritive juyce They damp linnen and paper though never
of America an Eruption of a Burning Mountain and an Earthquake near the same time which for the memorableness of the event I shall set down in a few lines Thirty five leagues on the South of Lima is situate a Famous Port call'd Hisco and a Town in which most of Noblesse and persons of Qualitie doe reside who perceiving one day that the Sea retir'd all at once from their shoars and left the River dry great Numbers of people flock't together on the shoare to behold so extraordinary a sight little suspecting the ill destiny which was to attend them For presently after they saw a great and suddain tumour of the Sea and perceiv'd the Water to boyl and the waves to swell and rowle one upon another not like Waves but Mountains of water so high that there remain'd no hope of saving their lifes by flight expecting every moment when they should be Swallow'd up by the Sea so that the Ocean quitting it's ordinary Bounds made an excursion for three Hundred leagues overturn'd the houses and trees and left the Country desolate the ships sail'd over the highest walls during this wonderfull Inundation Canama a noted Village distant 230 leagues from Lima was destroy'd with it's Port and many other places more especially the Town of Arica which lost in the Harbour many ships richly laden to the value of a Million in Gold The Mountain Onerate which some years since had vomited out a great quantity of Ashes began a very terrible Conflagration and was follow'd by a suddain Trembling of the Earth which in lesse then a quarter of an hour swallow'd up severall Villages that there was scarce ever a more Dreadfull Earthquake It is not unusuall to have Inundations of the Seas Eruptions of Burning Mountains Earthquakes and then Violent Tempests like Hurricanes to happen about the same time and probably from the same Cause For the Nitro-Sulphureous spirit which causes the Trembling of the Earth and that stupendious commotion of the Seas may afterward break loose into the most Horrid conflagrations and Winds especially in such places that abound with these Thundring Minerals which if we consider their Active nature are the fittest Materials for Hurricanes I know not how farre it may be thought a confirmation of this that Bray-Brook in Northampton-Shire where as was at large describ'd in the last of the Philosophicall Transactions there happen'd that dangerous Whirlwind the last year has been a place much subject to Earthquakes But I return from this digression to the Hurricanes of the West-Indies where it seems to me very odd that they should be so dreadfull in some places of the Caribbe-Islands insomuch that Mevis and St. Christophers have severall times been almost depopulated by them when they never reach to Jamaica on the one side happily as lying without the Vortex of the Whirlwind nor on the other beyond Barbados where they have seldome more then the Tail of an Hurricane though it is not farre situate from St. Christophers Porto Rico Gardaloupe and other Islands where they rage with the greatest violence They are no strangers to the Moluccas and Philippines and we have most incredible relations of the storms in the way to Japan which have carry'd ships a considerable distance from the Sea up the Dry-Land Some have been miserably wrackt buryed in the waves others split in a thousand pieces against the Rocks that scarce one ship in five escapes these diasters in the Tempestuous Months about Autumn or at the change of the Monsoons From hence we may collect this considerable remarque That they never happen but on the Eastern Shoars where they are Fatall to the Chinese and Caribbe-Seas and so as farr as the River of Plate likewise to that part of Afric from the Cape to St. Lawrence the Adjacent Isles when they are altogether unknown to the African Ocean from the Canaries to Cape Bon Esperance are never heard of at New Spain or the Coasts of Peru nor towards any other western parts of America because there the VVinds which blow off from Land make no opposition against the Generall Brise but comply with the Constant motion of the Air between the Tropiques from East to West For the shifting of the Trade-Wind from the Easterly Points is usually the first On-set of an approaching Hurricane Yet however these suspicious of mine be receiv'd I think it cannot be rationally disputed but that those direfull Tempests have their first rise from the Western Continent for we seldome encounter them very remote from Land and the experienc'd Masters-of-ships are never jealous of Hurricanes in the Spacious Ocean or if they perceive them coming immediately make out to Sea where their fury is much lesse then near the Shoars They are most to be dreaded about the end of Summer in the Months of July and August For both the Winds and Seas imitate the Motions of the Sun and being dilated by the Celestiall heat annually revert from North to South and from South to North again so that the Sun hasting from one Tropique to another causes the like suddain Conversions in the Currents and Winds and being the most Universall Efficient must needs be principally concern'd in all vicissitudes of the Sublunary World Hurricanes are usually preceded by an extraordinary Tranquillity of the Heavens and Seas possibly some Counter-Winds may for a short space ballance another bring the Air to an Equal poise So that those who happen to be in the Center of the Whirl-Wind are at first sensible of no disturbance as we see in Eddys or Whirl-pools of water that while the Circumference is violently agitated in the middle it continues for some time quiet and calme I have already too long digres'd from my first design which was to contribute what I could to their History for this end I have collected severall relations which may be of greatest importance to make a fuller discovery of their nature the Miraculous Effects of Hurricanes The first is out of Battista Ramusio and though I am assur'd that the best accounts are to be had from Oviedo and other Spaniards the descriptions they have made of the New-World yet their books are so rarely to be met with that very few of the Spanish Journalls come to our hands but what were first translated into other Modern languages as this of two severall Hurricanes at the Island of Hispaniola I made diligent enquiry after Gonzalo D' Oviedo which is a book fit to be consulted upon this occasion which I at last found in the University Library done into Italian by Gio Battista Ramusio with severall other Portugal and Spanish Journals where I met with the following descriptions of these Hurricanes in one of the Caribbe-Islands Hurricane in the Language of this Island signifies properly a most excessive Tempestuous storme and in effect is nothing else but an extraordinary great Wind and Raine together It happened on Wednesday the third of August in the year 1508 Don Francisco