Deu 8:8 | KD | STEP | The Israelites were to continue mindful of this paternal discipline on the part of their God, when the Lord should bring them into the good land of Canaan. This land Moses describes in , , in contrast with the dry unfruitful desert, as a well-watered and very fruitful land, which yielded abundance of support to its inhabitants; a land of water-brooks, fountains, and floods (תּהומות, see ), which had their source (took their rise) in valleys and on mountains; a land of wheat and barley, of the vine, fig, and pomegranate, and full of oil and honey (see at ); lastly, a land “ in which thou shalt not eat (support thyself) in scarcity, and shalt not be in want of anything; a land whose stones are iron, and out of whose mountains thou hewest brass .” The stones are iron, i.e., ferruginous. This statement is confirmed by modern travellers, although the Israelites did not carry on mining, and do not appear to have obtained either iron or brass from their own land. The iron and brass of which David collected such quantities for the building of the temple ( , ), he procured from Betach and Berotai ( ), or Tibchat and Kun ( ), towns of Hadadezer, that is to say, from Syria. According to , however, the Danites brought iron-work to the market of Tyre. Not only do the springs near Tiberias contain iron ( v. Schubert , R. iii. p. 239), whilst the soil at Hasbeya and the springs in the neighbourhood are also strongly impregnated with iron ( Burckhardt , Syrien , p. 83), but in the southern mountains as well there are probably strata of iron between Jerusalem and Jericho ( Russegger , R. iii. p. 250). But Lebanon especially abounds in iron-stone; iron mines and smelting furnaces being found there in many places ( Volney, Travels; Burckhardt, p. 73; Seetzen , i. pp. 145, 187ff., 237ff.). The basalt also, which occurs in great masses in northern Canaan by the side of the limestone, from the plain of Jezreel onwards (Robinson, iii. p. 313), and is very predominant in Bashan, is a ferruginous stone. Traces of extinct copper-works are also found upon Lebanon ( Volney , Travels; Ritter’s Erdkunde , xvii. p. 1063).

‏ Deuteronomy 8:8

The Israelites were to continue mindful of this paternal discipline on the part of their God, when the Lord should bring them into the good land of Canaan. This land Moses describes in Deu 8:8, Deu 8:9, in contrast with the dry unfruitful desert, as a well-watered and very fruitful land, which yielded abundance of support to its inhabitants; a land of water-brooks, fountains, and floods (תּהומות, see Gen 1:2), which had their source (took their rise) in valleys and on mountains; a land of wheat and barley, of the vine, fig, and pomegranate, and full of oil and honey (see at Exo 3:8); lastly, a land “in which thou shalt not eat (support thyself) in scarcity, and shalt not be in want of anything; a land whose stones are iron, and out of whose mountains thou hewest brass.” The stones are iron, i.e., ferruginous. This statement is confirmed by modern travellers, although the Israelites did not carry on mining, and do not appear to have obtained either iron or brass from their own land. The iron and brass of which David collected such quantities for the building of the temple (1Ch 22:3, 1Ch 22:14), he procured from Betach and Berotai (2Sa 8:8), or Tibchat and Kun (1Ch 18:8), towns of Hadadezer, that is to say, from Syria. According to Eze 27:19, however, the Danites brought iron-work to the market of Tyre. Not only do the springs near Tiberias contain iron (v. Schubert, R. iii. p. 239), whilst the soil at Hasbeya and the springs in the neighbourhood are also strongly impregnated with iron (Burckhardt, Syrien, p. 83), but in the southern mountains as well there are probably strata of iron between Jerusalem and Jericho (Russegger, R. iii. p. 250). But Lebanon especially abounds in iron-stone; iron mines and smelting furnaces being found there in many places (Volney, Travels; Burckhardt, p. 73; Seetzen, i. pp. 145, 187ff., 237ff.). The basalt also, which occurs in great masses in northern Canaan by the side of the limestone, from the plain of Jezreel onwards (Robinson, iii. p. 313), and is very predominant in Bashan, is a ferruginous stone. Traces of extinct copper-works are also found upon Lebanon (Volney, Travels; Ritter’s Erdkunde, xvii. p. 1063).