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3 See Labbé, Veteres glossae verborum juris quae passim in Basilicisreperiuntur (1606); Otto, Thesaurus juris Romani, iii. (1697);Stephens, Thesaurus linguae Graecae, viii. (1825).
In 1659 Henry (1639-1660), a brother of Charles II., wasformally created duke of Gloucester, a title which he had bornesince infancy. This prince, sharing the exile of the Stuarts, hadincensed his mother, Queen Henrietta Maria, by his firm adherenceto the Protestant religion, and had fought among theSpaniards at Dunkirk in 1658. Having returned to Englandwith Charles II., he died unmarried in London on the 13th ofSeptember 1660. The next duke was William (1689-1700),son of the princess Anne, who was, after his mother, the heir tothe English throne, and who was declared duke of Gloucester byhis uncle, William III., in 1689, but no patent for this creationwas ever passed. William died on the 30th of July 1700, andagain the title became extinct.
Glyptodonts constitute a family, the Glyptodontidae,whose position is next to thearmadillos (Dasypodidae); the group beingrepresented by a number of generic types.The Pleistocene forms, whose remains occurabundantly in the silt of the Buenos Airespampas, are by far the largest, the skull andtail-sheath in some instances having a lengthof from 12 to 16 ft. In Glyptodon (withwhich Schistopleurum is identical) the tail-sheathconsists of a series of coronet-likerings, gradually diminishing in diameter frombase to tip. Daedicurus, in which the tail-sheathis in the form of a huge solid club, isthe largest member of the family, in Panochthusand Sclerocalyptus (Hoplophorus) thetail-sheath consists basally of a small numberof smooth rings, and terminally of a tube.In some specimens of these genera the hornyshields covering the bony scutes of the carapacehave been preserved, and since theforamina, which often pierce the latter, stopshort of the former, it is evident that thesewere for the passage of blood-vessels andnot receptacles for bristles. In the earlyPleistocene epoch, when South Americabecame connected with North America, some of the glyptodontsfound their way into the latter continent. Among these northernforms some from Texas and Florida have been referred toGlyptodon. One large species from Texas has, however, beenmade the type of a separate genus, under the name of Glyptotheriumtexanum. In some respects it shows affinity with Panochthus,although in the simple structure of the tail-sheath itrecalls the undermentioned Propalaeohoplophorus. All the aboveare of Pleistocene and perhaps Pliocene age, but in the Santa Cruzbeds of Patagonia there occur the two curious genera Propalaeohoplophorusand Peltephilus, the former of which is a primitive andgeneralized type of glyptodont, while the latter seems to comenearer to the armadillos. Both are represented by species of comparativelysmall size. In Propalaeohoplophorus the scutes of thecarapace, which are less deeply sculptured than in the larger glyptodonts,are arranged in distinct transverse rows, in three of whichthey partially overlap near the border of the carapace after thefashion of the armadillos. The skull and limb-bones exhibit severalfeatures met with in the latter, and the vertebrae of the back are notwelded into a continuous tube. There are eight pairs of teeth, thefirst four of which are simpler than the rest, and may perhaps thereforebe regarded as premolars. More remarkable is Peltephilus, onaccount of the fact that the teeth, which are simple, with a chevron-shapedsection, form a continuous series from the front of the jawbackwards, the number of pairs being seven. Accordingly, amodification of the character, even of the true Edentata, as givenin the earlier article, is rendered necessary. The head bears a pairof horn-like scutes, and the scutes of the carapace and tail, whichare loosely opposed or slightly overlapping, form a number of transverserows.
In every country where the lowest and oldest rocks have come tothe surface and been exposed by the long continued action of denudationin stripping away the overlying formations, gneisses are found ingreat abundance and of many different kinds. They are in fact thetypical rocks of the Archean (Lewisian, Laurentian, &c.) series.In the Alps, Harz, Scotland, Norway and Sweden, Canada, SouthAmerica, Peninsular India, Himalayas (to mention only a fewlocalities) they occupy wide areas and exhibit a rich diversity oftypes. From this it has been inferred that they are of great geologicalage, and in fact this can be definitely proved in many cases, for theoldest known fossiliferous formations may be seen to rest unconformablyon these gneisses and are made up of their débris. It wasfor a long time believed that they represented the primitive crust ofthe earth, and while this is no longer generally taught there arestill geologists who hold that these gneisses are necessarily of pre-Cambrianage. Others, while admitting the general truth of thishypothesis, consider that there are localities in which typical gneissescan be shown to penetrate into rocks which may be as recent as theTertiary period, or to pass into these rocks so gradually and in sucha way as to make it certain that the gneisses are merely alteredstates of comparatively recent sedimentary or igneous rocks. Muchcontroversy has arisen on these points; but this is certain, thatgneisses are far the most common among Archean rocks, and wheretheir age is not known the presumption is strong that they are atleast pre-Cambrian.
In the Mandaean speculations the Seven are introduced withthe Babylonian names of the planets. The connexion of theSeven with the planets is also clearly established by the expositionsof Celsus and Origen (Contra Celsum, vi. 22 seq.) and similarlyby the above-quoted passage in the Pistis-Sophia, where thearchontes, who are here mentioned as five, are identified withthe five planets (excluding the sun and moon). This collectivegrouping of the seven (five) planetary divinities is derived fromthe late Babylonian religion, which can definitely be indicatedas the home of these ideas (Zimmern, Keilinschriften in demalten Testament, ii. p. 620 seq.; cf. particularly Diodorus ii. 30).And if in the old sources it is only the first beginnings of thisdevelopment that can be traced, we must assume that at a later155period the Babylonian religion centred in the adoration of theseven planetary deities. Very instructive in this connexionis the later (Arabian) account of the religion of the MesopotamianSabaeans. The religion of the Sabaeans, evidently a lateroffshoot from the stock of the old Babylonian religion, actuallyconsists in the cult of the seven planets (cf. the great work ofDaniel Chwolsohn, Die Ssabier u. der Ssabismus). But thisreference to Babylonian religion does not solve the problemwhich is here in question. For in the Babylonian religion theplanetary constellations are reckoned as the supreme deities.And here the question arises, how it came about that in theGnostic systems the Seven appear as subordinate, half-daemonicpowers, or even completely as powers of darkness. This canonly be explained on the assumption that some religion hostileto, and stronger than the Babylonian, has superimposed itselfupon this, and has degraded its principal deities into daemons.Which religion can this have been? We are at first inclined tothink of Christianity itself, but it is certainly most improbablethat at the time of the rise of Christianity the Babylonian teachingabout the seven planet-deities governing the world should haveplayed so great a part throughout all Syria, Asia Minor andEgypt, that the most varying sections of syncretic Christianityshould over and over again adopt this doctrine and work it upinto their system. It is far more probable that the combinationwhich we meet with in Gnosticism is older than Christianity,and was found already in existence by Christianity and its sects.We must also reject the theory that this degradation of theplanetary deities into daemons is due to the influence of Hebrewmonotheism, for almost all the Gnostic sects take up a definitelyhostile attitude towards the Jewish religion, and almost alwaysthe highest divinity among the Seven is actually the creator-Godof the Old Testament. There remains, then, only one religionwhich can be used as an explanation, namely the Persian, whichin fact fulfils all the necessary conditions. The Persian religionwas at an early period brought into contact with the Babylonian,through the triumphant progress of Persian culture towardsthe West; at the time of Alexander the Great it was already theprevailing religion in the Babylonian plain (cf. F. Cumont,Textes et monuments rel. aux mystères de Mithra, i. 5, 8-10, 14,223 seq., 233). It was characterized by a main belief, tendingtowards monotheism, in the Light-deity Ahuramazda and hissatellites, who appeared in contrast with him as powers of thenature of angels.
As regards wild goats other than the representatives of Caprahircus, the members of the ibex-group are noticed under Ibex,while another distinctive type receives mention under Markhor.The ibex are connected with the wild goat by means of Capranubiana, in which the front edge of the horns is thinner than ineither the European C. ibex or the Asiatic C. sibirica; whilethe Spanish C. pyrenaica shows how the ibex-type of horn maypass into the spirally twisted one distinctive of the markhor,C. falconeri. In the article Ibex mention is made of the Caucasusibex, or tur, C. caucasica, as an aberrant member of that group,but beside this animal the Caucasus is the home of another veryremarkable goat, or tur, known as C. pallasi. In this ruminant,which is of a dark-brown colour, the relatively smooth blackhorns diverge outwards in a manner resembling those of thebharal among the sheep rather than in goat-fashion; and, infact, this tur, which has only a very short beard, is so bharal-likethat it is commonly called by sportsmen the Caucasian bharal.It is one of the species which render it so difficult to give a precisedefinition of either sheep or goats.
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