2 A deadly conflict with the Ammonites was provoked by a gross insult to friendly ambassadors of Israel; 3 and this war, of which we have pretty full details in 2 Sam.
26-3 r, assumed unexpected dimensions when the Ammonites procured the aid of their Aramean neighbours.
If his reason for taking refuge in Ishbaal's capital Mahanaim is not obvious, it is even more remarkable that he should have been received kindly by the Ammonites whom he had previously decimated.
Hence we find them taking part with Ammonites and Midianites (Judg.
AMMONITES, or the "children of Ammon," a people of east Palestine who, like the Moabites, traced their origin to Lot, the nephew of the patriarch Abraham, and must have been regarded, therefore, as closely related to the Israelites and Edomites.
Both the Ammonites and Moabites are sometimes spoken of under the common name of the children of Lot (Deut.
According to the traditions, the original territory of the two tribes was the country lying immediately on the east of the Dead Sea, and of the lower half of the Jordan, having the Jabbok for its northern boundary; and of this tract the Ammonites laid claim to the northern portion between the Arnon and the Jabbok, out of which they had expelled the Zamzummim (Judg.
By this invasion, as the Moabites were driven to the south of the Arnon, which formed their northern boundary from that time, so the Ammonites were driven out of Gilead across the upper waters of the Jabbok where it flows from south to north, which henceforth continued to be their western boundary (Num.
The other limits of the Ammonitis, or country of the Ammonites ('Aï¿½ï¿½av7res x pa, 2 Mac. iv.
The metropolis of the Ammonites (Deut.
With the neighbouring tribes, the Ammonites helped the Babylonian monarch Nebuchadrezzar against Jehoiakim (2 Kings xxiY.
7) - leads an army of Israel and Judah to deliver Jabesh-Gilead from the Ammonites, and is now recognized as king.
Mesozoic rocks are represented by slates containing Ammoniles and Monotis, evidently of Triassic age, rocks containing Ammonites Bucklandi of Liassic age, a series of beds rich in plants of Jurassic age, and beds of Cretaceous age containing Trigonia and many other fossils.
4447), and a fresh separation from the heathen (Moabites and Ammonites, xiii.
Invasions followed by Chaldeans, Syrians, Moabites and Ammonites, per 1 2 Kings xxiv.
Their fossils include belemnites, ammonites, scaphites and marine saurians, such as Cimoliosaurus.
At Portrush, the Lower Lias is seen on the shore, crowded with ammonites, but silicified and metamorphosed by invading dolerite.
3) it is stated that the prohibition against intermarriage with the Moabites, Ammonites, Egyptians and Edomites, though given in the Bible, only applied for a certain number of generations and did not apply at all to their daughters, but, it is added, "Bastards and Nethinim are prohibited (to marry Israelites), and this prohibition is perpetual and applies both to males and females."
He showed that from each individual shell of an ammonite the entire ancestral series may be reconstructed, and that, while the earlier shell-whorls retain the characters of the adults of preceding members of the series, a shell in its own adult stage adds a new character, which in turn becomes the pre-adult character of the types which will succeed it; finally, that this comparison between the revolutions of the life of an individual and the life of the entire order of ammonites is wonderfully harmonious and precise.
In 1869 Wilhelm Heinrich Waagen (1841-1900) entered the field with the study of Ammonites subradiatus.
Cephalopod molluscs have been traced back to the straight-shelled nautiloids of the genus Volborthella, while true ammonites have been found in the inferior Permian of the Continent and by American palaeontologists in the true coal measures.
Among the ammonites of the Jurassic and Cretaceous periods types occur which in their external appearance so closely resemble each other that they could be taken for members of a single series, and not infrequently have been taken for species of the same genus and even for the same species; but their early stages of development and, in fact, their entire individual history prove them to be distinct and not infrequently to belong to widely separated genetic series.
Hyatt (1883) observed of the ammonites that each group originated suddenly and spread out with great rapidity.
In his history of the Arietidae Hyatt points out that toward the close of the Cretaceous this entire group of ammonites appears to have been affected with some malady; the unrolled forms multiply, the septa are simplified, the ornamentation becomes heavy, thick, and finally disappears in the adult; the entire group ends by dying out and leaving no descendants.
Among the ammonites the loss of power to coil the shell is one feature of racial old age, and in others old age is accompanied by closer coiling and loss of surface ornamentation, such as spines, ribs, spirals; while in other forms an arresting of variability precedes extinction.
Whereas among many ammonites and gastropods smooth ness of the shell, following upon an ornamental youthful Condition, is generally a symptom of decline, among many other invertebrates and vertebrates, as C. E.
Holofernes now inquires of the chiefs who are with him about the Israelites,and is answered by Achior the leader of the Ammonites, who enters upon a long historical narrative showing the Israelites to be invincible except when they have offended God.
Crystalline rocks crop out at several capes; Cretaceous limestones, containing an abundant and specific fauna of gigantic ammonites, occur at Dui on the west coast, and Tertiary conglomerates, sandstones, marls and clays, folded by subsequent upheavals, in many parts of the island.
The Upper Cretaceous is represented by limestones with bands of chert, and contains Ammonites, Baculites, Hippurites and other fossils.
Menelaus, the brother of Simon the Benjamite, had bought the high-priesthood over the head of Jason, who fled into the country of the Ammonites, in 172 B.C. (2 Macc. iv.
Few or no extinct types are to be found in these older strata - there is nothing among the plants equivalent to the unmistakably extinct Ammonites, Belemnites, and a hundred other groups, and we only meet with constant variations in the same genus or family, these variations having seldom any obvious relation to phylogeny.
Among these we may include not only the Israelites or tribes which afterwards became Israelitish, but the Moabites, Ammonites and Edomites.
In the seas, bony fish and crab-like decapods increased in numbers and variety, while pelecypods and gasteropods took the prominent place previously occupied by ammonites and belemnites, and, leaving behind such forms as Rudistes, Inoceramus, &c., they gradually developed in the direction of the modern regional groups.
Lot is saved and becomes the ancestor of the Moabites and Ammonites, who are thus closely related to the descendants of Abraham (note xix.
Westward of and above these strata, the Middle and Upper Jurassic formations are found (Lias, Lower Oolite, Oxfordian, &c.), with well-marked and numerous fossils (Ammonites, Nerinaea, Natica, Astarte, Rhynchonella, Echinodermata, &c.); then the Cretaceous rocks, both these and the Jurassic series being largely developed, the Cretaceous fossils including Nautilus, Belemnites, Ostrea, Gryphaea, &c., and some very large Ammonites (Pachydiscus).
Xxxv., 12) " the reproach of Moab and the revilings of the Ammonites," and the Lord of Hosts, the God of Israel, swears by his life that both shall be destroyed for their hostility towards his people, and the remnant of his nation shall possess their territory (vv.
The Jurassic beds are marine and contain numerous Ammonites, but the beds which are referred to the Neocomian include a series of sandstones and shales with remains of plants.
49); apparently the site of the camp of the Israelites when about to attack the Ammonites under Jephthah's leadership (Judges x.
The fossils from the Rhaetic beds belong to the Avicula contorta zone, those from the Lias to the Ammonites angulatus zone, while the blocks of limestone with chert contain Inoceramus, Cretaceous foraminifera and other organisms. The materials yielding these fossils are embedded in a course volcanic agglomerate which gives rise to crags and is pierced by acid and basic igneous ricks.