SECTIO SEXTA.

[Sidenote: Munst. Frisius.] Sunt in hac Insula montes elati in coelum, quorum vertices perpetua niue candent, radices sempiterno igne æstuant. Primus Occidentem versus est, qui vocatur Hecla, alter crucis, tertius Helga. Item Zieglerus. Rupes siue promontorium Hecla æstuans perpetuis ignibus. Item Saxo. In hac itidem Insula mons est, qui rupem sideream perpetuæ flagrationis æstibus imitatus, incendia sempiterna iugi flammarum eructatione continuat.

Miracula Islandiæ Munsterus & Frisius narraturi mox in vestibulo, magno suo cum incommodo impingunt. Nam quod hic de monte Hecla asserunt, etsi aliquam habet veritatis speciem, tamen quod idem de duobus alijs montibus perpetuo igne æstuantibus dicunt, manifestè erroneum est. Illi enim in Islandia non extant, nec quicquam, quod huic tanto scriptorum errori occasionem dederit, imaginari possumus. Facta tamen est, sed nunc demum Anno 1581. ex monte quodam australis Islandiæ, maritimo, perpetuis niuibus & glacie obducto memorabilis fumi ac flammæ eruptio, magna saxorum ac cineris copia eiecta. Cæterum ille mons longe est ab his tribus, quos authores commemorant, diuersissimus. Porro etsi hæc de montibus ignitis maximè vera narrarent, annon naturaliter ista contingerent? An ad extruendam illam, quæ mox in Munstero, Zieglero & Frisio sequitur, de orco Islandico opinionem aliquid faciunt? Ego sanè nefas esse duco, his vel similibus naturæ miraculis ab absurda asserenda abuti, vel hæc tanquam impossibilia cum quadam impietate mirari. Quasi verò non concurrant in huiusmodi incendijs causæ ad hanc rem satis validæ. Est in horum montium radicibus materia vri aptissima, nempe sulphurea & bituminosa. Accedit aër per poros ac cauernas in terræ viscera ingressus, ac illum maximi incendij fomitem exsufflans vnà cum nitro, qua exsufflatione tanquam follibus quibusdam, ardentissima excitatur flamma. Habet siquidem ignis, his ita conacnientibus, quæ tria ad vrendum sunt necessaria, materiam scilicet, motum, & tandem penetrandi facultatem: Materiam quidem pinguem & humidam ideoque flammas diuturnas alentem: Motum præstat per terræ cauernas admissus aër: Penetrandi facultatem facit ignis vis inuicta, sine respiraculo esse nescientis, & incredibili conatu violenter erumpentis, atque ita (non secus ac in cuniculis machinisue seu tormentis bellicis, globi è ferro maximi, magno cum fragore ac strepitu, à sulphure & nitro, è quibus pyrius puluis conficitur, excitato, eijciuntur) lapides & Saxa in ista voragine ignita, ceu quodam camino, collique facta cum immodica arenæ & cinerum copia, exspuentis & eiaculantis, idque vt plurimum, non sine terræmotu: qui si secundum profunditatem terræ fiat, succussio à Possidoneo appellatur vel hiatus erit, vel pulsus. Hiatu terra dehiscit: pulsu eleuatur intumescens, & nonunquam, vt inquit Plinius [Sidenote: Lib. 2. cap. 20.], motes magnas egerit: Cuiusmodi terræmotus iam mentionem fecimus, maritima Islandiæ Australis Anno 1581 infestantis quíque à Pontano his verbis scitissimè describitur.

Ergo incerta ferens raptim vestigia, anhelus Spiritus incursat, nunc huc, nunc percitus illuc, Explorátque abitum insistens, & singula tentat, Si qua forte queat victis erumpere claustris. Interea tremit ingentem factura ruinam Terra, suis quatiens latas cum moenibus vrbes: Dissiliunt auulsa iugis immania saxa, &c.

Hæc addere libuit, non quòd cuiquam hæc ignota esse existimemus; sed ne nos alij ignorare credant, atque ideo ad suas fabulas, quas hinc extruunt, confugere velle.

Cæterum video quid etiamnum admirationem non exiguam scriptoribus moueat, in his, quos ignoranter fingunt, tribus Islandiæ montibus, videlicet cum eorum basin semper ardere dicant, summitates tamen nunquam niue careant. Porrò id admirari, est præter authoritatem tantorum virorum, quibus Ætnæ incendium optimè notum erat, quæ, cùm secundum Plinium hybernis temporibus niualis sit, noctibus tamen, eodem teste, semper ardet. Quare etiam secundum illos, ille mons, cum adhac niuium copia obducitur, & tamen ardeat sordidarum animarum quoque erit receptaculum: id quod Heclæ propter niues in summo vertice & basin æstuantem, adscribere non dubitarunt. [Sidenote: Cardanus.] Vix autem mirum esse potest, quòd ignis montis radicibus latens, & nunquam, nisi rarissimè erumpens, excelsa montis cacumina, quæ niuibus obducuntur, non collique faciat. Nam & in Caira, altissima montis cacumina niuibus semper candentia esse perhibentur: & in Beragua quidem similiter, sed 5000 passuum in coelum elata, quæ niuibus nunquam liberentur, cum tamen partibus tantum decem ab æquatore distent. Vtrámque hanc prouinciam iuxta Pariam esse sitam accepimus. Quid? quod illa Teneriffæ (quæ vna, est ex insulis Canarijs, quæ & fortunatæ) pyramis, secundum Munsterum, 8 aut 9 milliarium Germanicorum altitudine in aëra assurgens, atque instar Ætnæ iugiter conflagrans, niues, quibus media cingitur, teste Benzone Italo, Indiæ occidentalis Historico, non resoluit. Quod ipsum in nostra Hecla quid est, quod magis miremur? Atque hæc ita breuiter de incendijs montanis.

Nunc illud quoque castigandum arbitramur, quod hos montes in coelum vsque attolli scribant. Habent enim nullam præ cæteris Islandiæ montibus notabilem altitudinem. Precipuè tertius ille Helga à Munstero appellatus, nobis Helgafel. i. Sacer mons, apud monasterium eiusdem nominis, nulla sui parts tempore æstiuo nimbus obductus, nec montis excelsi, sed potius collis humilis nomen meretur, nunquam, vt initio huius sectionis dixi, de incendio suspectus. Nec verò perpetuæ niues Heclæ, vel paucis alijs adscribi debebant: Permultos enim habet eiusmodi montes niuosos Islandia, quos omnes vel toto anno, non facilè collegerit aut connumerarit, horum prædicator & admirator Cosmographus. Quin etiam id non negligendum, quod mons Hecla non occidentem versus, vt à Munstero & Zieglero annotatum est, sed inter meridiem & orientem positus sit. Nec promontorium est: sed mons ferè mediterraneus.

[Sidenote: Annales Islandiæ.] Incendia perpetua ragi, &c. Quicunque perpetuam flammarum cructationem Heclæ adscripserunt, toto coelo errarunt, adeò, vt quoties flammas eructarit, nostrates in annales retulerint, viz. anno Christi 1104. 1157. 1222. 1300. 1341. 1362. & 1389. Neque enim ab illo de montis incendio audire licuit, vsque ad annum 1558. quæ vltima fuit in illo monte eruptio. Interea non nego, fieri posse, quin mons infernè latentes intus flammas & incendia alat, quæ videlicet statis interuallis, vt hactenus annotatum est, eruperint, aut etiam forte posthac erumpant.

The same in English.

THE SIXTH SECTION

[Sidenote: Monsterus. Frisius.] There be in this Iland mountaines lift vp to the skies, whose tops being white with perpetuall snowe, their roots boile with euerlasting fire. The first is towards the West, called Hecla: the other the mountaine of the crosse: and the third Helga. Item Zieglerus. The rocke or promontone of Hecla boileth with continuall fire. Item: Saxo. There is in this Iland also a mountaine, which resembling the starrie firmament, with perpetuall flashings of fire, continueth alwayes burning, by vncessant belching out of flames.

Munster and Frisius being about to report the woonders of Island doe presently stumble, as it were, vpon the thresholde, to the great inconuenience of them both. For that which they heere affirme of mount Hecla, although it hath some shew of trueth: notwithstanding concerning the other two mountaines, that they should burne with perpetuall fire, it is a manifest errour. For there are no such mountaines to be found in Island, nor yet any thing els (so farre foorth as wee can imagine) which might minister occasion of so great an errour vnto writers. Howbeit there was seene (yet very lately) in the yeere 1581 out of a certaine mountaine of South Island lying neere the Sea, and couered ouer with continuall snow and frost, a marueilous eruption of smoke and fire, casting vp abundance of stones and ashes. But this mountaine is farre from the other three, which the sayd authours doe mention. Howbeit, suppose that these things be true which they report of firie mountaines: is it possible therefore that they should seeme strange, or monstrous, whenas they proceed from naturall causes? What? Doe they any whit preuaile to establish that opinion concerning the hell of Island, which followeth next after in Munster, Ziegler, and Frisius? For my part, I thinke it no way tollerable, that men should abuse these, and the like miracles of nature, to auouch absurdities, or, that they should with a kinde of impietie woonder at them, as at matters impossible. As though in these kindes of inflammations, there did not concurre causes of sufficient force for the same purpose. There is in the rootes of these mountaines a matter most apt to be set on fire, comming so neere as it doeth to the nature of brimstone and pitch. There is ayer also which insinuating it selfe by passages, and holes, into the very bowels of the earth, doeth puffe vp the nourishment of so huge a fire, together with Salt-peter, by which puffing (as it were with certeine bellowes) a most ardent flame is kindled. [Sidenote: Three naturall causes of firie mountaines.] For, all these thus concurring fire hath those three things, which necessarily make it burne, that is to say, matter, motion, and force of making passage: matter which is fattie and moyst, and therefore nourisheth lasting flames: motion which the ayer doeth performe, being admitted into the caues of the earth: force of making passage, and that the inuincible might of fire it selfe (which can not be without inspiration of ayre, and can not but breake foorth with an incredible strength) doeth bring to passe: and so (euen as in vndermining trenches and engines or great warrelike ordinance, huge yron bullets are cast foorth with monstrous roaring, and cracking, by the force of kindled Brimstone, and Salt-peeter, whereof Gunne-powder is compounded) chingle and great stones being skorched in that fiery gulfe, as it were in a furnace, together with abundance of sande and ashes, are vomitted vp and discharged, and that for the most part not without an earthquake which, if it commeth from the depth of the earth, (being called by Possidonius, Succussio) it must either be either an opening or a quaking. Opening causeth the earth in some places to gape, and fall a sunder. By quaking the earth is heaued vp and swelleth, and sometimes (as Plinie saith) [Sidenote: Lib. 20. cap. 20.] casteth out huge heaps: such an earth-quake was the same which I euen now mentioned, which in the yere 1581 did so sore trouble the South shore of Island. And this kinde of earth-quake is most clearkely described by Pontanus in these verses:

The stirrng breath runnes on with stealing steppes, vrged now vp, and now enforced downe: For freedome eke tries all, it skips, it leaps, to ridde it selfe from vncouth dungeon. Then quakes the earth as it would burst anon, The earth yquakes, and walled cities quiuer. Strong quarries cracke, and stones from hilles doe shiuer.

I thought good to adde these things, not that I suppose any man to be ignorant thereof: but least other men should thinke that we are ignorant, and therefore that we will runne after their fables, which they do from hence establish. But yet there is somewhat more in these three famed mountaines of Island, which causeth the sayd writers not a little to woonder, namely whereas they say that their foundations are alwayes burning, and yet for all that, their toppes be neuer destitute of snowe. Howbeit, it beseemeth not the authority and learning of such great clearks to marueile at this, who can not but well know the flames of mount Aetna, which (according to Plinie) being full of snowe all Winter, notwithstanding (as the same man witnesseth) it doth alwayes burne. Wherefore, if we will giue credit vnto them, euen this mountaine also, sithens it is couered with snowe, and yet burneth, must be a prison of vncleane soules: which thing they haue not doubted to ascribe vnto Hecla, in regard of the frozen top, and the fine bottome. And it is no marueile that fire lurking so deepe in the roots of a mountaine, and neuer breaking forth except it be very seldome, should not be able continually to melt the snowe couering the toppe of the sayd mountaine. [Sidenote: Cardanus] For in Caira (or Capira) also, the highest toppes of the mountaine are sayd continually to be white with snowe: and those in Veragua likewise, which are fiue miles high, and neuer without snowe, being distant notwithstanding but onely 10 degrees from the equinoctiall. We haue heard that either of the forsayd Prouinces standeth neere vnto Paria. What, if in Teneriffa (which is one of the Canarie or fortunate Islands) the Pike [Footnote: The Peak.] so called, arising into the ayre, according to Munster, eight or nine Germaine miles in height, and continually flaming like Aetna: yet (as Benzo an Italian, and Historiographer of the West Indies witnesseth) is it not able to melt the girdle of snowe embracing the middest thereof. Which thing, what reason haue we more to admire in the mountaine of Hecla? And thus much briefly concerning firie mountaines.

Now that also is to be amended, whereas they write that these mountaines are lifted vp euen vnto the skies. For they haue no extraordinarie height beyond the other mountaines of Island, but especially that third mountaine, called by Munster Helga, and by vs Helgafel, that is the holy mount, standing iust by a monastery of the same name, being couered with snowe, vpon no part thereof in Summer time, neither deserueth it the name of an high mountaine, but rather of an humble hillocke, neuer yet as I sayd in the beginning of this section, so much as once suspected of burning. Neither yet ought perpetuall snowe to be ascribed to Hecla onely, or to a few others; for Island hath very many such snowy mountaines, all which the Cosmographer (who hath so extolled and admired these three) should not easily find out, and reckon vp in a whole yere. And that also is not to be omitted, that mount Hecla standeth not towards the West, as Munster and Ziegler haue noted, but betweene the South and the East: neither is it an headland, but rather a mid-land hill.

[Sidenote: The chronicles of Island.] Continueth alwayes burning &c. whosoeuer they be that haue ascribed vnto Hecla perpetuall belching out of flames, they are farre besides the marke: insomuch that as often as it hath bene enflamed, our countreymen haue recorded it in their yerely Chronicles for a rare accident: namely in the yeeres of Christ 1104, 1157, 1222, 1300, 1341, 1362, and 1389: For from that yeere we neuer heard of the burning of this mountaine vntill the yeere 1558, which was the last breaking foorth of fire in that mountaine. In the meane time I say not that is impossible, but that the bottome of the hill may inwardly breed and nourish flames, which at certaine seasons (as hath bene heretofore obserued) haue burst out, and perhaps may do the like hereafter. [Footnote: The surface of the country is very mountainous, but there are no definite ranges, the isolated volcanic masses being separated by elevated plateaux of greater or less size. The whole centre is, in fact, an almost continuous desert fringed by a belt of pasture land, lying along the coast and running up the valleys of several of the greater riuers. This desert is occupied partly by snow mountains and glaciers, partly by enormous lava streams, partly by undulating plains of black volcanic sand, shingle, and loose stones. This region is of course without verdure, and entirely uninhabited. The rocks are all of igneous origin, but of very different ages, traps, basalts, amygdaloids, tufas, ochres, and porous lavas. The number of active volcanoes is, at present, not great, but hot springs and mud volcanoes testify to the existence of volcanic action along a line running from the extreme south west at Cape Reykjanes to the north coast near Husavik. The only recent well ascertained eruptions have been from Hecla, Aotlugja, Skaptar Vokul, and (in 1874-5) from the mountains to the south-east of Myratu Lake. The eruption of Skaptar in 1783 is the greatest anywhere on record in respect of the quantity of lava and ashes ejected. Earthquakes are not unfrequent. The greatest mountain group is the Vatna or Klofa Yokul, on the south coast, a mass of snow and ice covering many hundred square miles, and sending down prodigious glaciers which almost reach the sea. From one of these a torrent issues, little more than a hundred yards long, and a mile and a half broad. The line of perpetual snow ranges from 2,000 to 3,000 feet. The loftiest summits of this great mountain mass have never been ascended, but the highest point is believed to be the Orefa Yolcal, 6,405 feet. The other considerable peaks in different parts of the island are Herdubreidr (an extinct volcano), 5,290 feet, Eyjafjalla Yokul, 5,579 feet, Snæfels Yokul, 5,965 feet, and Hecla, 5,095 feet.]