History of Civilization in England, Vol. 1 of 3

136

Wilkinson's Ancient Egyptians, vol. ii. pp. 175–178. See also on the abundance of dates, the extracts from an Arabian geographer in Quatremère, Recherches sur l'Egypte, pp. 220, 221.

137

On their relation to the laws of climate, see the remarks respecting the geographical limits of their power of ripening, in Jussieu's Botany, edit. Wilson, 1849, p. 734.

138

‘In the valley of the Nile, a feddan (1¾ acre) is sometimes planted with 400 trees.’ Wilkinson's Ancient Egyptians, vol. ii. p. 178. At Moorzuk an entire date-palm is only worth about a shilling. Richardson's Central Africa, vol. i. p. 111.

139

On the remarkable fertility of the Said, see Abd-Allatif, Relation de l'Egypte, p. 3.

140

The superiority of the ruins in Southern Egypt over those in the northern part is noticed by Heeren (African Nations, vol. ii. p. 69), and must, indeed, be obvious to whoever has studied the monuments. In the Said the Coptic was preserved longer than in Lower Egypt, and is known to philologists by the name of Misr. See Quatremère, Recherches sur la Langue de l'Egypte, pp. 20, 41, 42. See also on the Saidic, pp. 134–140, and some good remarks by Dr. Prichard (Physical Hist. vol. ii. p. 202); who, however, adopts the paradoxical opinion of Georgi respecting the origin of the language of the Thebaid.

141

Abd-Allatif (Relation de l'Egypte, p. 32) says, that in his time it was only cultivated in the Said. This curious work by Abd-Allatif was written in a. d. 1203. Relation, p. 423. Meiners thinks that Herodotus and other ancient writers refer to the dhourra without mentioning it: ‘diese Durra muss daher im Herodot wie in andern alten Schriftstellern vorzüglich verstanden werden, wenn von hundert, zwey hundert, und mehrfältigen Früchten, welche die Erde trage, die Rede ist.’ Meiners, Fruchtbarkeit der Länder, vol. i. p. 139. According to Volney, it is the Holcus Arundinaceus of Linnæus, and appears to be similar to millet; and though that accurate traveller distinguishes between them, I observe that Captain Haines, in a recent memoir, speaks of them as being the same. Compare Haines in Journal of Geog. Soc. vol. xv. p. 118, with Volney, Voyage en Egypte, vol. i. p. 195.

142

‘The return is in general not less than 240 for one; and the average price is about 3s. 9d. the ardeb, which is scarcely 3d. per bushel.’ Hamilton's Æqyptiaca, p. 420. In Upper Egypt, ‘the doura constitutes almost the whole subsistence of the peasantry,’ p. 419. At p. 96, Hamilton says, ‘I have frequently counted 3,000 grains in one ear of doura, and each stalk has in general four or five ears.’ For an account, of the dhourra bread, see Volney, Voyage en Egypte, vol. i. p. 161.

143

Ἐπεὰν πλήρης γένηται ὁ ποταμὸς, καὶ τὰ πεδία πελαγίσῃ, φύεται ἐν τῷ ὅδατι κρίνεα πολλὰ, τὰ Αἰγύπτιοι καλέουσι λωτόν⋅ ταῦτα ἐπεὰν δρέψωσι, αὐαίνουσι πρὸς ἥλιον⋅ καὶ ἔπειτα τὸ ἐκ τοῦ μέσου τοῦ λωτοῦ τῇ μήκωνι ἐὸν ἐμφερὲς, πτίσαντες ποιεῦνται ἐξ αὐτοῦ ᾰρτους ὀπτοὺς πυρίπυρί. Herodot. ii. 92, vol. i. p. 688.

144

Wilkinson's Ancient Egyptians, vol. ii. pp. 370–372, 400, vol. iv. p. 59. Abd-Allatif gives a curious account of the different vegetables grown in Egypt early in the thirteenth century. Relation, pp. 16–36, and the notes of De Sacy, pp. 37–134. On the κύαμσς of Herodotus there are some botanical remarks worth reading in the Correspondence of Sir J. E. Smith, vol. ii. pp. 224–232; but I doubt the assertion, p. 227, that Herodotus ‘knew nothing of any other kind of κύαμσς in Egypt than that of the ordinary bean.’

145

‘When Alexandria was taken by Amer, the lieutenant of the Caliph Omer, no less than 4,000 persons were engaged in selling vegetables in that city.’ Wilkinson's Ancient Egyptians, vol. ii. p. 372, and see vol. i. p. 277, vol. iv. p. 60. Niebuhr (Description de l'Arabie, p. 136) says that the neighbourhood of Alexandria is so fertile, that ‘le froment y rend le centuple.’ See also on its rich vegetation, Matter, Histoire de l'Ecole d'Alexandrie, vol. i. p. 52.

146

The encouragement given to the increase of population by the fertility arising from the inundation of the Nile, is observed by many writers, but by none so judiciously as Malthus; Essay on Population, vol. i. pp. 161–163. This great work, the principles of which have been grossly misrepresented, is still the best which has been written on the important subject of population, though the author, from a want of sufficient reading, often errs in his illustrations; while he, unfortunately, had no acquaintance with those branches of physical knowledge which are intimately connected with economical inquiries.

147

Τρέφουσι δὲ τὰ παιδία μετά τινος εὐχερείας ἀαπάνου, καὶ παντελῶς ἀπίστον … ἀνυποδέτων δὲ τῶν πλείστων καὶ γυμνῶν τρεφομένων διὰ τὴν εὐκρασιαν τῶν τόπων, τὴν πᾶσαν δαπάνην οἱ γονεῒς, ᾰχρις ἂν εἰς ἡλικίαν ἒλθῃ τὸ τέκνον, οὐ πλείω ποιοῦσι δραχμῶν εῐκοσι, δἰ ἂς αἰτς μάλιστα τὴν Αἴγυπτον συμβαίνει πολυανθρωπίᾳ διαθέρειν, καὶ διὰ τοῦτο πλείστας ἔχειν μεγάλων ἔργωνκατασκευάς. Bibliothec. Hist. book i. chap. lxxx. vol. i. p. 238.

148

Frederick Schlegel (Philos. of Hist. p. 247, London, 1846) truly says, ‘The deeper and more comprehensive the researches of the moderns have been on ancient history, the more have their regard and esteem for Herodotus increased.’ His minute information respecting Egypt and Asia Minor is now admitted by all competent geographers; and I may add, that a recent and very able traveller has given some curious proofs of his knowledge even of the western parts of Siberia. See Erman's valuable work, Travels in Siberia, vol. i. pp. 211, 297–301.

149

Ἐπ᾽ Ἀμάσιος δὲ βασιλέος λέγεται Αἴγυπτος μάλισ-α δὴτότε εὐδαιμονῆσαι, καὶ τὰ ἀπὸ τοῦ ποταμοῦ τῇ χώρῃς τοῒσι ἀνθρπισι. καὶ πόλις ἐν αὐτῇγενέσθαι τὰς ἁπάσας τότε δισμνρίας τὰς οἰκεομένας. Herodot. book ii. chap. clxxvii. vol. i. pp. 881, 882.

150

Diodorus, who, though an honest and painstaking man, was in every respect inferior to Herodotus, says, impertinently enough, ὅσα μὲν οὖν Ἠόδοτος καί τινες τῶν τὰς Αἀγυπτίων πδάξεις συνταξαμένων ἐσχεδιάκασιν, ἑκουσίως προκρίναντες τῆς ἀληθείας τὸ παραδοξολογεῖν, καὶ μύθους πλάττειν φυχαγωγίας ἕνεκα, παρήσομεν. Biblioth. Hist. book i. chap. lxix. vol. i. p. 207. In other places he alludes to Herodotus in the same tone, without actually mentioning him.

151

Πολυανθρωπία δὲ τὸ μὲν παλαιὸν πολὺ προέσχε πάντων τῶν γνωριζομένων τόπων κατὰ τὴν οἰκουμένην, καὶ καθ᾽ ἡμᾶς δὲ οὐδενὸς τῶν ᾰλλων δοκεῒ λείπεσθαι. ἐπὶ μὲν γὰρ τῶν ἀχαίων χρόνων ἔσχε κώμας ἀξιολόγους, καὶ πόλεις πλείους τῶν μυρίων καὶ ὀκτακισχιλίων, ὡ ἐν ταῒς ἀναγραφαῖς ὁρᾶν ἐστι κατακεχωρισμένον. Diod. Sic. Biblioth. Hist. book i. chap. xxxi. vol. i. p. 89.

152

Notwithstanding the positive assertions of M. Matter (Hist. de l'Ecole d'Alexandrie, vol. ii. p. 285; compare Hist. du Gnosticisme, vol. i. p. 48), there is no good evidence for the supposed travels in Egypt of the earlier Greeks, and it is even questionable if Plato ever visited that country. (‘Whether he ever was in Egypt is doubtful.’ Bunsen's Egypt, vol. i. p. 60.) The Romans took little interest in the subject (Bunsen, vol. i. pp. 152–158); and, says M. Bunsen, p. 152, ‘with Diodorus all systematic inquiry into the history of Egypt ceases, not only on the part of the Greeks, but of the ancients in general.’ Mr. Leake, in an essay on the Quorra, arrives at the conclusion, that after the time of Ptolemy, the ancients made no additions to their knowledge of African geography. Journal of Geographical Society, vol. ii. p. 9.

153

See on this some good remarks in Heeren's African Nations, vol. ii. pp. 202–207; and as to the difference between the traditions of Thebes and Memphis, see Matter, Histoire de l'Ecole d'Alexandrie, vol. i. p. 7. The power and importance of the two cities fluctuated, both being at different periods the capital. Bunsen's Egypt, vol. ii. pp. 54, 55, 244, 445, 446; Vyse on the Pyramids, vol. iii. pp. 27, 100; Sharpe's History of Egypt, vol. i. pp. 9, 19, 24, 34, 167, 185.

154

Sir John Herschel (Disc. on Natural Philosophy, p. 60) calculates that the great pyramid weighs twelve thousand seven hundred and sixty million pounds. Compare Lyell's Principles of Geology, p. 459, where the still larger estimate of six million tons is given. But according to Perring, the present quantity of masonry is 6,316,000 tons, or 82,110,000 cubic feet. See Bunsen's Egypt, vol. ii. p. 155, London, 1854, and Vyse on the Pyramids, 1840, vol. ii. p. 113.

155

Many fanciful hypotheses have been put forward as to the purpose for which the pyramids were built; but it is now admitted that they were neither more nor less than tombs for the Egyptian kings! See Bunsen's Egypt, vol. ii. pp. xvii. 88, 105, 372, 389; and Sharpe's History of Egypt, vol. i. p. 21.

156

For an estimate of the expense at which, one of the pyramids could be built in our time by European workmen, see Vyse on the Pyramids, vol. ii. p. 268. On account, however, of the number of disturbing causes, such calculations have little value.

157

Those who complain that in Europe this interval is still too great, may derive a species of satisfaction from studying the old extra-European civilizations.

158

Wilkinson's Ancient Egyptians, vol. ii. pp. 8, 9. ‘Nor was any one permitted to meddle with political affairs, or to hold any civil office in the state.’ … ‘If any artizan meddled with political affairs, or engaged in any other employment than the one to which he had been brought up, a severe punishment was instantly inflicted upon him.’ Compare Diod. Sic. Bibliothec. Hist. book i. chap. lxxiv. vol. i. p. 223.

159

Wilkinson's Ancient Egyptians, vol. i. p. 263, vol. ii. p. 2; Sharpe's History of Egypt, vol. ii. p. 24.

160

Wilkinson's Ancient Egyptians, vol. ii. pp. 41, 42, vol. iii. p. 69, vol. iv. p. 131. Compare Ammianus Marcellinus, in Hamilton's Ægyptiaca, p. 309.

161

Vyse on the Pyramids, vol. i. p. 61, vol. ii. p. 92.

162

‘Ein König ahmte den andern nach, oder suchte ihn zu übertreffen; indess das gutmüthige Volk seine Lebenstage am Baue dieser Monumente verzehren musste. So entstanden wahrscheinlich die Pyramiden und Obelisken Aegyptens. Nur in den ältesten Zeiten wurden sie gebauet: denn die spätere Zeit und jede Nation, die ein nützliches Gewerbe treiben lernte, bauete keine Pyramiden mehr. Weit gefehlt also, dass Pyramiden ein Kennzeichen von der Glückseligkeit und Aufklärung des alten Aegyptens seyn sollten, sind sie ein unwidersprechliches Denkmal von dem Aberglauben und der Gedankenlosigkeit sowohl der Armen, die da baueten, als der Ehrgeizigen, die den Bau befahlen.’ Herder's Ideen zur Geschichte, vol. iii. pp. 103, 104: see also p. 293, and some admirable remarks in Volney's Voyage en Egypte, vol. i. pp. 240, 241. Even M. Bunsen, notwithstanding his admiration, says of one of the pyramids, ‘the misery of the people, already grievously oppressed, was aggravated by the construction of this gigantic building… The bones of the oppressors of the people who for two whole generations harassed hundreds of thousands from day to day,’ &c. Bunsen's Egypt, vol. ii. p. 176, a learned and enthusiastic work.

163

Καὶ τοῦτο ἐκόμιζον μὲν ἐπ᾽ ἔτεα τρία διοχίλιοι δὲ οἱ οσετετάχατο ᾰνδρες ἀγωγέες. Herodot. book ii. chap. clxxv. vol. i. p. 897. On the enormous weight of the stones which the Egyptians sometimes carried, see Bunsen's Egypt, vol. i. p. 379; and as to the machines employed, and the use of inclined roads for the transit, see Vyse on the Pyramids, vol. i. p. 197, vol. iii. pp. 14, 38.

164

Wilkinson's Ancient Egyptians, vol. i. p. 70: but this learned writer is unwilling to believe a statement so adverse to his favourite Egyptians. It is likely enough that there is some exaggeration; still no one can dispute the fact of an enormous and unprincipled waste of human life.

165

Τριάκοντα μὲν γὰρ καὶ ἒξ μυριάδες ἀνὃρῶν, ὥς φασι, ταῖς τῶν ἔργων λειτουργίαισμα τέλος ἔσχε μόγις ἐτῶν εἴκοσι διελθόντων Diod. Sic. Bibliothec. Hist. book i. ch. lxiii. vol. i. p. 188.

166

‘When compared with other parts of the New World, Mexico and Peru may be considered as polished states.’ History of America, book vii. in Robertson's Works, p. 904. See, to the same effect, Journal of Geograph. Society, vol. v. p. 355.

167

Compare Squier's Central America, vol. i. pp. 34, 244, 358, 421, vol. ii. p. 307, with Journal of Geograph. Society, vol. iii. p. 59, vol. viii. pp. 319, 323.

168

Mr. Squier (Central America, vol. ii. p. 68); who explored Nicaragua, says of the statues, ‘the material, in every case, is a black basalt, of great hardness, which, with the best of modern tools, can only be cut with difficulty.’ Mr. Stephens (Central America, vol. ii. p. 355) found at Palenque ‘elegant specimens of art and models for study.’ See also vol. iii. pp. 276, 389, 406, vol. iv. p. 293. Of the paintings at Chichen he says (vol. iv. p. 311), ‘they exhibit a freedom of touch which could only be the result of discipline and training under masters.’ At Copan (vol. i. p. 151), ‘it would be impossible, with the best instruments of modern times, to cut stones more perfectly.’ And at Uxmal (vol. ii. p. 431), ‘throughout, the laying and polishing of the stones are as perfect as under the rules of the best modern masonry.’ Our knowledge of Central America is almost entirely derived from these two writers; and although the work of Mr. Stephens is much the more minute, Mr. Squier says (vol. ii. p. 306), what I believe is quite true, that until the appearance of his own book in 1853, the monuments in Nicaragua were entirely unknown. Short descriptions of the remains in Guatemala and Yucatan will be found in Larenaudière's Mexique et Guatemala, pp. 308–327, and in Journal of Geograph. Society, vol. iii. pp. 60–63.

169

See the remarks on Yucatan in Prichard's Physical History of Mankind, vol. v. p. 348: ‘a great and industrious, though perhaps, as the writer above cited (Gallatin) observes, an enslaved population. Splendid temples and palaces attest the power of the priests and nobles, while as usual no trace remains of the huts in which dwelt the mass of the nation.’

170

Dr. M'Culloh (Researches concerning the Aboriginal History of America, pp. 272–340) has collected from the Spanish writers some meagre statements respecting the early condition of Central America; but of its social state and history, properly so called, nothing is known; nor is it even certain to what family of nations the inhabitants belonged, though a recent author can find ‘la civilisation guatemalienne ou misteco-zapotèque et mayaquiche vivante pour nous encore dans les ruines de Mitla et de Palenque.’ Mexique et Guatemala, par Larenaudière, p. 8, Paris, 1843. Dr. Prichard, too, refers the ruins in Central America to ‘the Mayan race:’ see Prichard on Ethnology, in Report of British Association for 1847, p. 252. But the evidence for these and similar statements is very unsatisfactory.

171

Respecting the connection between the vegetable productions of a country and its geognostic peculiarities, little is yet known; but the reader may compare Meyen's Geography of Plants, p. 64, with Reports on Botany by the Ray Society, 1846, pp. 70, 71. The chemical laws of soil are much better understood, and have a direct practical bearing on the use of manures. See Turner's Chemistry, vol. ii. pp. 1310–1314; Brande's Chemistry, vol. i. p. 691, vol. ii. pp. 1867–1869; Balfour's Botany, pp. 116–122; Liebig and Kopp's Reports, vol. ii. pp. 315, 328, vol. iii. p. 463, vol. iv. pp. 438, 442, 446.

172

As to the influence of heat and moisture on the geographical distribution of plants, see Henslow's Botany, pp. 295–300, and Balfour's Botany, pp. 560–563. Meyen (Geog. of Plants, p. 263) says, ‘I, therefore, after allowing for local circumstances, bring the vegetation of islands also under the law of nature, according to which the number of species constantly increases with increasing heat and corresponding humidity.’ On the effect of temperature alone, compare a note in Erman's Siberia, vol. i. pp. 64, 65, with Reports on Botany by the Ray Society, pp. 339, 340. In the latter work, it is supposed that heat is the most important of all single agents; and though this is probably true, still the influence of humidity is immense. I may mention as an instance of this, that it has been recently ascertained that the oxygen used by seeds during germination, is not always taken from the air, but is obtained by decomposing water. See the curious experiments of Edwards and Colin in Lindley's Botany, vol. ii. pp. 261, 262, London, 1848; and on the direct nourishment which water supplies to vegetables, see Burdache's great work, Traité de Physiologie, vol. ix. pp. 254, 398.

173

There is a difference between the watersheds of the eastern and western ranges, which explains this in part, but not entirely; and even if the explanation were more satisfactory than it is, it is too proximate to the phenomenon to have much scientific value, and must itself be referred to higher geological considerations.

174

Of this irrigation some idea may be formed from an estimate that the Amazon drains an area of 2,500,000 square miles; that its mouth is 96 miles wide; and that it is navigable 2,200 miles from its mouth. Somerville's Physical Geography, vol. i. p. 423. Indeed, it is said in an essay on the Hydrography of South America (Journal of Geograph. Society, vol. ii. p. 250), that ‘with the exception of one short portage of three miles, water flows, and is for the most part navigable, between Buenos Ayres, in 35° south latitude, to the mouth of the Orinoco, in nearly 9° north.’ See also on this river-system, vol. v. p. 93, vol. x. p. 267. In regard to North America, Mr. Rogers (Geology of North America, p. 8, Brit. Assoc. for 1834) says, ‘the area drained by the Mississippi and all its tributaries is computed at 1,099,000 square miles.’ Compare Richardson's Arctic Expedition, vol. ii. p. 164.

175

The Oregon, or Columbia as it is sometimes called, forms a remarkable botanical line, which is the boundary of the Californian flora. See Reports on Botany by the Ray Society, p. 113.

176

For proof that the mean temperature of the western coast of North America is higher than that of the eastern coast, see Journal of Geograph. Society, vol. ix. p. 380, vol. xi. pp. 168, 216; Humboldt, la Nouvelle Espagne, vol. i. pp. 42, 336; Richardson's Arctic Expedition, vol. ii. pp. 214, 218, 219, 259, 260. This is well illustrated by the botanical fact, that on the west coast the Coniferæ grow as high as 68° or 70° north latitude; while on the east their northern limit is 60°. See an Essay on the Morphology of the Coniferæ, in Reports on Botany by the Ray Society, p. 8, which should be compared with Forry on the Climate of the United States and its Endemic Influences, New York, 1842, p. 89.

177

‘Writers on climate have remarked that the eastern coasts of continents in the northern hemisphere have a lower mean temperature than the western coasts.’ Richardson on North American Zoology, p. 129, Brit. Assoc. for 1836: see also Report for 1841, Sections, p. 28; Davis's China, vol. iii. pp. 140, 141; Journal of Geograph. Society, vol. xxii. p. 176.

178

The little that is known of the early state of the North-American tribes has been brought together by Dr. M'Culloh in his learned work, Researches concerning America, pp. 119–146. He says, p. 121, that they ‘lived together without laws and civil regulations.’ In that part of the world, the population has probably never been fixed; and we now know that the inhabitants of the north-east of Asia have at different times passed over to the north-west of America, as in the case of the Tschuktschi, who are found in both continents. Indeed, Dobell was so struck by the similarity between the North-American tribes and some he met with nearly as far west as Tomsk, that he believed their origin to be the same. See Dobell's Travels in Kamtschatka and Siberia, 1830, vol. ii. p. 112. And on this question of intercourse between the two continents, compare Crantz's History of Greenland, vol. i. pp. 259, 260, with Richardson's Arctic Expedition, vol. i. pp. 362, 363, and Prichard's Physical History of Mankind, vol. iv. pp. 458, 463, vol. v. pp. 371, 378.

179

From general physical considerations, we should suppose a relation between amount of rain and extent of coast; and in Europe, where alone we have extensive meteorological records, the connexion has been proved statistically. ‘If the quantity of rain that falls in different parts of Europe is measured, it is found to be less, other things being equal, as we recede from the sea-shore.’ Kaemtz's Meteorology, 1845, p. 139. Compare pp. 91, 94. Hence, no doubt, the greater rarity of rain as we advance north from Mexico. ‘Au nord du 20°, surtout depuis les 22° au 30° de latitude, les pluies, que ne durent que pendant les mois de juin, de juillet, d'août et de septembre, sont peu fréquentes dans l'intérieur du pays.’ Humboldt, la Nouvelle Espagne, vol. i. p. 46.

180

‘The difference between the climates of the east and west coasts of continents and islands, has also been observed in the southern hemisphere but here the west coasts are colder than the east, while in the northern hemisphere the east coasts are the colder.’ Meyen's Geography of Plants, 1846, p. 24.

181

Mr. Darwin, who has written one of the most valuable works ever published on South America, was struck by this superiority of the eastern coast; and he mentions that ‘fruits which ripen well and are very abundant, such as the grape and fig, in latitude 41° on the east coast, succeed very poorly in a lower latitude on the opposite side of the continent.’ Darwin's Journal of Researches, Lond. 1840, p. 268. Compare Meyen's Geog. of Plants, pp. 25, 188. So that the proposition of Daniell (Meteorological Essays, p. 104, sec. xiv.) is expressed too generally, and should be confined to continents north of the equator.

182

The trade-winds sometimes reach the thirtieth parallel. See Daniell's Meteorological Essays, p. 469. Dr. Traill (Physical Geography, Edin. 1838, p. 200), says, ‘they extend to about 30° on each side of the equator:’ but I believe they are rarely found so high; though Robertson is certainly wrong in supposing that they are peculiar to the tropics; History of America, book iv. in Robertson's Works, p. 781.

183

‘In the northern hemisphere the trade-wind blows from the north-east, and in the southern from the south-east.’ Meyen's Geog. of Plants, p. 42. Compare Walsh's Brazil, vol. i. p. 112, vol. ii. p. 494; and on the ‘tropical east-wind’ of the Gulf of Mexico, see Forry's Climate of the United States, p. 206. Dr. Forry says that it has given to the growth of the trees ‘an inclination from the sea.’