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Robert Burton

The Anatomy of Melancholy

1651 English with a close modern English rendering

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The Anatomy of MelancholyMember 3. Air Corrected. With a Digression on Air.

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1651 English Page · Branch 460 of 1495

Member 3. Air Corrected. With a Digression on Air.

1651 English

247–248

nay, they that dwell in the same parallel line with these Negros, as about the Straights of Magellan, are white coloured, and yet some in Presbyter Johns country in Æthiopia are dun: they in Zeilan and Malabar parallel with them again black: Manamotapa in Africk, and St. Thomas Isle are extreme hot, both under the line, cole black their Inhabitants, whereas in Peru they are quite opposite in colour, very temperate, or rather cold, and yet both alike elevated.

Mosco in 53. degrees of latitude is extreme cold, as those Northern countries usually are, having one perpetuall hard frost all winter long: and in 52. deg. lat. sometimes hard frost and snow all summer, as in Buttons Bay, &c. or by fits; and yet England neere the same Latitude, and Ireland, very moist, warme, and more temperate in Winter than Spain, Italy, or France.

Is it the sea that causeth this difference, and the Aire that comes from it: Why then is Ister so cold neere the Euxine, Pontus, Bithinia, and all Thrace; frigidas regiones Magnus calls them, and yet their latitude is but 42. which should be hot: Quevira, or Nova Albion in America, bordering on the sea, was so cold in July, that our Englishmen could hardly endure it.

At Noremberga in 45. lat. all the sea is frozen Ice, and yet in a more Southern latitude than ours. New England, and the Iland of Cambrioll Colchos, which that noble Gentleman Mr Vaughan, or Orpheus Iunior, describes in his Golden Fleece, is in the same latitude with little Britaine in France, and yet their winter begins not till January, their Spring till May; which search he accounts worthy of an Astrologer:

is this from the Easterly winds, or melting of ice and snow dissolved within the circle Artick; or that the aire being thick, is longer before it be warm by the Sun beams, and once heated like an oven will keep it self from cold?

Our Climes breed lice, Hungary and Ireland malè audiunt in this kinde; come to the Azores, by a secret vertue of that aire they are instantly consumed, and all our European vermine almost, saith Ortelius. Egypt is watred with Nilus not far from the sea, and yet there it seldome or never rains: Rhodes, an Iland of the same nature, yeelds not a cloud, and yet our Ilands ever dropping and inclining to rain.

The Atlantick Ocean is still subject to storms, but in Del Zur, or Mari pacifico, seldome or never any. Is it from Topick stars, apertio portarum, in the Dodecotemories or constellations, the Moons mansions, such aspects of Planets, such winds, or dissolving ayre, or thick ayre, which causeth this and the like differences of heat and cold?

247–248

The Anatomy of Melancholy: Member 3. Air Corrected. With a Digression on Air.

p. 460

Indeed, those who live on the same parallel as these Black people, around the Strait of Magellan, have white complexions; yet some in Prester John’s country in Ethiopia are brown, while the people of Ceylon and Malabar, on a parallel with them, are black again. Monomotapa in Africa and the island of São Tomé are extremely hot, both on the equator, with coal-black inhabitants; whereas in Peru the people are quite the opposite in colour, the climate very temperate or rather cold, and yet the latitude is the same.

Moscow, at fifty-three degrees latitude, is extremely cold, as those northern countries generally are, with one continuous hard frost throughout the winter. At fifty-two degrees latitude there is sometimes hard frost and snow all summer, as in Button’s Bay and elsewhere, or at intervals. Yet England, at nearly the same latitude, and Ireland are very moist, warm, and milder in winter than Spain, Italy, or France.

Is the sea responsible for this difference, and the air that comes from it? Why then is the Danube so cold near the Black Sea, along with Pontus, Bithynia, and all Thrace? Magnus calls them “cold regions,” yet their latitude is only forty-two degrees, which ought to be hot. Quivira, or New Albion in America, bordering the sea, was so cold in July that our Englishmen could scarcely bear it.

At Norumbega, in latitude forty-five degrees, the whole sea is frozen, though it lies farther south than we do. New England and the island of Cambriol Colchos, which that noble gentleman Mr Vaughan, or Orpheus Junior, describes in his Golden Fleece, lie at the same latitude as Brittany in France; yet their winter does not begin until January, and their spring until May. He considers the investigation worthy of an astrologer.

Does this come from easterly winds, or from melting ice and snow within the Arctic Circle? Or is it because the air is dense and takes longer to be warmed by the sun’s rays, but once heated, like an oven, keeps out the cold?

Our climates breed lice; Hungary and Ireland have a bad reputation in this respect. Go to the Azores, and by some hidden power of the air they are instantly destroyed, along with almost all our European vermin, according to Ortelius. Egypt is watered by the Nile not far from the sea, yet there it seldom or never rains. Rhodes, an island of the same nature, produces not a cloud, yet our islands are always dripping and tending towards rain.

The Atlantic Ocean is continually subject to storms, but in the South Sea, or Pacific Ocean, there are seldom or never any. Do these and similar differences of heat and cold come from stars governing particular places, an “opening of the gates” in the divisions of the zodiac or constellations, the mansions of the moon, particular aspects of the planets, particular winds, or air that is dissolving or dense?

460

About This Reading Edition

Robert Burton’s Anatomy ranges across medicine, philosophy, poetry, religion, and everyday life in its inquiry into melancholy. This complete parallel edition pairs the 1651 English text with a close modern English rendering, preserving the three Partitions, Democritus Junior’s address to the reader, verse, and the historical index.

Historical Text and Translation

The historical text follows the sixth edition, printed at Oxford for Henry Cripps in 1651, using the McGill University Library copy. The supplied edition documents missing printed pages 98–99 supplied from another 1651 copy at the Bavarian State Library. Historical folio labels and their irregularities remain visible; web reader numbers identify reflowed passages and do not claim to reproduce PDF pagination.

About Diotimos Editions

Diotimos Editions prepared the close modern English rendering and editorial matter. All 8,755 original and modern passage pairs remain aligned, with verse breaks, italics, continuations, and linked annotations preserved. Burton’s 6,781 historical notes retain their attribution; 6,895 editorial notes remain distinct. The introduction, Note on the Text, contextual lexicon, indexes, source documentation, and bibliography are included. The engraved frontispiece remains available in the original downloads.

Rights

Burton’s historical text is in the public domain. The modern English rendering, introduction, notes, and editorial matter are © 2026 Diotimos Editions and appear with the site owner’s permission. The complete supplied PDF, EPUB, Word, and Markdown files remain available unchanged. The PDF and Word edition preserve the original parallel page layout.