While the ark carried with Israel's host symbolized His presence in their midst, He was also known to be present in the cloud which hovered before the host and in the lightning ('esh Yahweh or " fire of Yahweh ") and the thunder (kol Yahweh or " voice of Yahweh ") which played around Mount Sinai.
Akrish, Kol Mebasser (Constantinople, 1577), and often reprinted in editions of Jehuda hal-Levv's Kuzari.
They chiefly consist of the Bhumij, Tala, Kol and Savara peoples, the Savaras being by far the most numerous, numbering 14,775.
The root kol is common to all the Teutonic nations, while in French and other Romance languages derivatives of the Latin carbo are used, e.g.
On the east the Pamir highlands are fenced off from the East Turkestan lowlands by the double border-ridge of Sarik-kol (the Sarik-kol range and the Murtagh or Kashgar range), which has its eastern foot down in the Tarim basin (4000-4500 ft.) and its western up on the Pamirs at 10,500 to 13,000 ft.
Bogdanovich, the same fossils occur in both sets of border ranges, in the Sarik-kol and in their eastward continuations, e.g.
In the western parts of the system they mostly go to feed the Kara-muren or the Cherchen-darya, while farther east they flow down into some larger self-contained basin of internal drainage, such as the Achik-kol, the two lakes Kara-kol, or the Ghaz-kol, and even yet farther east make their way, some of them into the lakes of the Tsaidam depression or become lost in its sands or in those of the Kum-tagh desert on the north, or go to feed the headstreams of the great rivers, the Hwang-ho (Yellow River) and the Yangtsze-kiang (Blue River) in the south.
Down to the shallow salt lake of Ghaz-kol or Chimen-koli (9305 ft.).
In the western part of this valley occurs the very important transverse water-divide of Gulcha-davan (14,150 ft.), which separates the basin of the Cherchen-darya that goes down into the Tarim basin from the area that drains down to the Ghaz-kol, which belongs to the Tsaidam depression.
The latter range, the Chimen-tagh, is identical in its western parts with the Piazlik-tagh and in the east must be equated with the Tsaidam chain of Przhevalsky; and it is probably continued westwards by the range which the Russian explorers call the Moscow Range or the Achik-tagh, running north of the Achik-kol and, according to Przhevalsky, connecting on the west with the Tokuz-davan.
It is possible however that the Muzluk-tagh belongs more intimately to the Chimen-tagh system, that is, to the Moscow or Achik-kol ranges.
Sven Hedin, whilst agreeing that this may possibly be the true conception, inclines to the view that the Achik-kol Range dies away towards the E., and that the Chimen-tagh and the Kalta-alaghan merge westwards into the border-ranges that lie north of the Muzluk-tagh and the Tokuzdavan.
Immediately south of the Kalta-alaghan comes a relatively deep depression, the Kum-kol valley, forming a very well-marked feature in the physical conformation of this region.
It is crossed transversely by a water-divide which separates the basin of the twin-lakes, of Kum-kol (12,700 ft.) from the basin of Tsaidam, some 3500 ft.
The floor of the valley consequently slopes away in both directions, like the Chimen valley between the Akato-tagh and the Chimen-tagh; and in so far as it slopes westwards towards the Kum kol lakes it differs from nearly all the other great latitudinal valleys that run parallel with it, because they slope generally towards the east.
Not far from the Kum-kol lakes there is a drift-sand area, though the dunes are stationary.
Farther west, lying between the Muzluk-tagh and the Arka-tagh, is the lake of Achik-kol (13940 ft.), 162 m.
With one exception, namely the climb out of the Kum-kol valley to the Arka-tagh, the first three steps are 1 This is the correct form, Arka-tagh meaning the Farther or Remoter Mountains.
When the altitudes of the intermont latitudinal valleys are compared, the significance orographically of the Chimen valley and of the Kum-kol valley is strikingly emphasized.
Kol Cr'16locrightk-vill c?
9,500 ft.) of Baron Kaulbars, the Kara-kol, and the Suzamir-tau, until it abuts upon the Talas-tau.
At Yanghi-kol (40° 52' N.
In the Talmud the voice from heaven, called Bath Kol, attested Rabbi Hillel, as he walked in Jericho, to be worthy of the holy spirit's descent and in-dwelling.
The case of the Kum-kol valley is altogether exceptional, for it lies not higher, but 680 ft.