The university, founded in 1869, built mainly of basalt, has schools of arts, medicine, chemistry and mineralogy.
Two days' journey beyond Rakka, where the Euphrates breaks through the basalt dike of el-IIamme, are two admirably preserved ruins, built of gypsum and basalt, that on the Mesopotamian side called Zelebiya (Chanuga), and that on the Syrian, much the finer of the two, Halebiya or Zenobiya, the ancient Zenobia.
Large areas are overlain with trachyte, basalt, obsidian, tuff and pumice.
Is perhaps the fine spring north of the village, a shallow pool of good water full of small fish, rising between black basalt boulders: or more probably the copious `Ain Jalud.
In most cases the eruptions appear to be of Pliocene or later date, but in the extreme north some of the basalt seems to belong to the Miocene period.
It is a basalt stele inscribed in hieroglyphic, demotic and Greek with a decree of the priests assembled at Memphis in favour of Ptolemy V.
In later days, in the time of the Sargonid kings of Akkad or the monarchs of Ur, stones such is granite, basalt, diorite and dolerite were probably brought from the Sinaitic peninsula, if not from the western desert of Egypt, if the Red Sea coast is to be identified, as seems very probable, with Magan, " the place to which ships went," the land whence the Babylonians got some of their first stones for sculpture and architecture.
The objects found in these researches are in the museum, the most notable being a great basalt bull, probably once an object of cult in the Serapeum.
Besides huge masses of old schists and sandstones, the range contains extensive limestone, marble, diorite, basalt and porphyry formations, while granite prevails on its southern slopes.
This iron is considered by several of the first authorities"on the subject to be of meteoric origin,' but no evidence hitherto given seems to prove decisively that it cannot be telluric. That the nodules found were lying on gneissic rock, with no basaltic rocks in the neighbourhood, does not prove that the iron may not originate from basalt, for the nodules may have been transported by the glaciers, like other erratic blocks, and will stand erosion much longer than the basalt, which may long ago have disappeared.
This iron seems, however, in several respects to be unlike the celebrated large nodules of iron found by Nordenskiold at Ovifak, but appears to resemble much more closely the softer kind of iron nodules found by Steenstrup in the basalt;' it stands exposure to the air equally well, and has similar Widmannstaten figures very sharp, as is to be expected in such a large mass.
Nigdeh; basalt drum or altar with incised inscription.
Inscribed basalt bowl found at Babylon) and fragments of ware painted with dark ornament on light body-clay, or in polychrome on a cream-white slip, or black burnished, found on N.
Such rocks as basalt, diorite and trachyte are comparatively rare.
The church of Preshute, largely rebuilt, but preserving its Norman pillars, has a curious piscina, and a black basalt font of great size dating from 1100-1150, in which according to a very old tradition King John was baptized.
In alluvial deposits the richest ground is usually found in contact with the "bed rock"; and, when the overlying cover of gravel is very thick, or, as sometimes happens, when the older gravel is covered with a flow of basalt, regular mining by shafts and levels, as in what are known as tunnel-claims, may be required to reach the auriferous ground.
The hills west of the town consist of horizontal strata of sandstone covered with irregular pieces of basalt and the top of the hill on which the observatory stood was made level by taking away the basalt.
The Nile at the Ripon Falls leaps over a basalt dike.
The rocks on the verge of the Kisumu province of East Africa are mainly volcanic (basalt, tuff, lava, kenyte).
In the Eastern province the rocks are mainly quartz, gneiss and granite, with sandstone in Busoga, basalt round Mt Elgon, slate (Busoga) and iron- g stone (Busoga and Bukedi).
In the Rudolf province there and are the basalt, lava, tuff and kenyte of the volcanic mineralogy.
The Nahuatl lapidaries had at hand many varieties of workable and beautiful stone - onyx, marble, limestone, quartz and quartz crystal, granite, syenite, basalt, trachyte, rhyolite, diorite and obsidian, the best of material prepared for them by nature; while the Mayas had only limestone, and hard, tenacious rock with which to work it, and timber for burning lime.
His idol was a huge block of basalt (still thought to be preserved in Mexico), on one side of which he is sculptured in hideous form, adorned with the feathers of the humming-bird.
Many of the oceanic islets are composed of coral limestone, which in this way becomes phosphatized; others are igneous, consisting of trachyte or basalt, and these rocks are also phosphatized on their surfaces but are not so valuable, inasmuch as the presence of iron or alumina in any quantity renders them unsuited for the preppration of artificial manures.
The soil, of decomposed basalt, is wonderfully fertile.
NEUENAHR, a spa of Germany, in the Prussian Rhine province, situated at the foot of a basalt peak, in the pleasant valley of the Ahr, io m.
Dr Bunge found Bolshoy to consist of granite protruding from beneath non-fossiliferous deposits; while the promontory of Svyatoy Nos Qonsists of basalt hills, 1400 ft.
GIANT'S CAUSEWAY, a promontory of columnar basalt, situated on the north coast of county Antrim, Ireland.
The volcanic fissures that allowed of the upwelling of basalt are represented by numerous dykes, many cutting the earlier lava-flows as well as all the beds below them.
The glens of Antrim are deep notches cut by seaward-running streams through the basalt scarp, their floors being formed of Triassic or older rocks.
In the Hauran 22.16 is shown by a basalt door (British Museum), and perhaps elsewhere in Syria (25).
On the north-west are several conical hills of basalt, which are surrounded by oases of fertile soil.
In the Miocene period andesites of various kinds were erupted, while at the close of the Pliocene began the great eruptions of basalt which reached their maximum in Quaternary times and continue to the present day.'
Teanaway basalt 4000
The sapphire occurs also in Europe, being found in the Iserweise of Bohemia and in the basalt of the Rhine valley and of Le-Puy-en-Velay in France, but the European stones have no interest as gems.
With the exception of the coral and a small amount of calcareous sandstone, the rocks are entirely volcanic and range from basalt to trachyte, but are mainly basalt.
Broad), continued westwards after a marshy break by the volcanic Tell Kokab (basalt, about 1300 ft.), and then the `Abd al-`Aziz range (limestone), veering upwards towards its western end as if to meet the Tektek promontory from the north.
They include colossal figures of Aesculapius and Bacchus, and the lower half of a seated Egyptian divinity in black basalt, bearing the cartouche of Tethmosis (Thothmes) I.
The town is still surrounded by the masonry walls of black basalt which give it the name of Kara or Black Amid; they are well built and imposing on the west facing the open country, but almost in ruins where they overlook the river.
Augite-andesite predominates, but basalt and rhyolite also occur.
Long, has a seaward slope of 300 ft., and is protected by rows of piles and basalt blocks.
13, Plate I I., the sequence of the basalt, shale and melaphyre is clearly visible on the sides of the pit; and fig.
Figure 9, Plate I., shows the top of the De Beers' crater with basalt overlying the shale.
The bulk of the mountain consists of andesite, but porphyry, obsidian, trachyte, basalt, and.
It is formed of basalt, trachyte and phonolite, and the soil is very fertile.
Thousands of feet of basalt have been worn away from many parts of its surface; deep and wide valleys have been carved out of it; and so enormously has it been wasted, that it has been almost entirely stripped from wide tracts which it formerly covered and where only scattered outliers remain to prove that it once existed.
Where lava has been piled up in successive nearly horizontal sheets, with occasional layers of tuff or other softer rock between them, it offers conditions peculiarly favourable for the formation of escarpments, as in the wide basalt plateaus of the Inner Hebrides.
These rocks form a prominent feature underneath the basalt terraces of the east side of Skye, Raasay and Eigg.
Rocks belonging to the Cretaceous system at one time covered considerable areas on both sides of the Highlands, but they have been entirely stripped off the eastern side, while on the western they have been reduced to a few fragmentary patches, which have survived because of the overlying sheets of basalt that have protected them.
Their existence under the basalt outlier of Ben Iadain in Morven, at a height of 1600 ft.