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 this book may be a bit more uncomfortable than Book 1. Stay with the discomfort if

iban moved into the house,?Rahim Khan said. "The pretext was that they had evicted a trespass

“But . . . but listen,” she said at last, with despair in her voice. “What can come of this? What will be the end of this?”

“I don’t know, I don’t know,” he whispered, waving off the disagreeable questions.

 nations who were said to have made too great an advance in civilization. Experience, no doubt, proves that nations, like individuals, find that intellect and learning do n

he other: namely limestone of Cumanacoa and that of Caripe. When I was on the spot the former appeared to me to hav north to 1 degree south). The latter plains, however, furnish some ledges of fragmentary rocks on the south-west of San Fernando de Atabapo, as well as on the south-east, in the lower part of the Rio Negro and the Rio Branco. I saw in the plains of Jaen de Bracamoros a sandstone which alternates with ledges of sand and conglomerate nodules of porphyry and Lydian stone. MM. Spix and Martius affirm that the banks of the Rio Negro on the south of the equator are composed of variegated sandstone; those of the Rio Branco, Jupura and Apoporis of quadersandstein; and those of the Amazon, on several points, of

lash of defiance. ‘There has been nothing said about love yet. You asked me to be your wife, and I said yes — meaning that at some remote period such a thing might be.’

She knew that the man was her slave — slave to her beauty, slave to her superior rank — and she was determined not to lessen the weight of his chain by so much as a feather.

‘Did not that promise imply something like love?’ he asked, earnestly.

‘Perhaps it implied a little gratitude for your devotion, which I have neither courted nor encouraged a little respect for your talents, your perseverance — a little admiration for your wonderful success in life. Perhaps love may follow these sentiments, naturally, easily, if you are very patient; but if you talk about our being married before next year, you will simply make me hate you.’

‘Then I will say very little, except to remind you that there is no earthly reason why we should not be married next month. October and November are the best months for Rome, and I heard you say last night you were pining to see Rome.’

‘What then — cannot Lady Kirkbank take me to Rome?’

‘And introduce you to the rowdiest people in the city,’ cried Mr. Smithson. ‘Lesbia, I adore you. It is the dream of my life to be your husband: but if you are going to spend a winter in Italy with Lady Kirkbank, I renounce my right, I surrender my hope. You will not be the wife of my dreams after that.’

‘Do you assert a right to control my life during our engagement?’

‘Some little right; above all, the privilege of choosing your friends. And that is one reason why I most fervently desire our marriage should not be delayed. You would find it difficult, impossible perhaps, to get out of Lady Kirkbank’s claws while you are single; but once my wife, that amiable old person can be made to keep her distance.’

‘Lady Kirkbank’s claws! What a horrible way in which to speak of a friend. I thought you adored Lady Kirkbank.’

‘So I do. We all adore her, but not as a guide for youth. As a specimen of the elderly female of the latter half of the nineteenth century, she is perfect. Such gush, such juvenility, such broad views, such an utter absence of starch; but as a lamp for the footsteps of girlhood — no there we must pause.’

bottom of a sea destitute of islands; it is only on the south of the Apure, between that river and the Meta, near the western bank of the Sierra, that a few hills appear, as Monte Parure, la Galera de Sinaruco and the Cerritos de San Vicente. With the exception of the fragments of tertiary strata above mentioned there is, from the equator to the parallel of 10° north (between the meridian of Sierra Nevada de Merida and the coast of Guiana), if not an absence, at least a scarcity of those petrifactions, which strikes an observer recently arrived from Europe.

[* Braunes eisenschussiges Sandstein-Conglomerat (Iron-sand of the English geologists, between the Jura limestone and green sandstone.) MM. Spix and Martius found on rocks of quadersandstein, between the Apoporis and the Japura, the same sculptures which we have pointed out from the Essequibo to the plains of Cassiquiare, and which seem to prove the migrations of a people more advanced in civilization than the Indians who now inhabit those countries.]

[* Is this wall a succession of rocks of dolomite or a dyke of quadersandstein, like the Devil’s Wall (Teufelsmauer), at the foot of the Hartz? Calcareous shelves (coral banks), either ledges of sandstone (effects of the revulsion of the waves) or volcanic eruptions, are commonly found on the borders of great plains, that is, on the shores of ancient inland seas. The Llanos of Venezuela furnish examples of such eruptions near Para(?) like Harudje (Mons Ater, Plin.) on the northern boundary of the African desert (the Sahara). Hills of sandstone rising like towers, walls and fortified castles and offering great analogy to quadersandstein, bound the American desert towards the west, on the south of Arkansas.]

The maxima of the height of the different formations diminish regularly in the country we are describing with their relative ages. These maxima, for gneiss-granite (Peak of Duida in the group of Parime, Silla de Caracas in the coast chain) are from 1300 to 1350 toises; for the limestone of Cumanacoa (summit or Cucurucho of Turimiquiri), 1050 toises; for the limestone of Caripe (mountains surrounding the table-land of the Guarda de San Augustin), 750 toises; for the sandstone alternating with the limestone of Cumanacoa (Cuchilla de Guanaguana), 550 toises; for the tertiary strata (Punta Araya), 200 toises.

The tract of country of which I am here describing the geological constitution is distinguished by the astonishing regularity observed in the direction of the strata of which the rocks of different eras are composed. I have already often pointed the attention of my readers to a geognostic law, one of the few that can be verified by precise measurements. Occupied since the year 1792 by the parallelism, or rather the loxodromism of the strata, examining the direction and inclination of the primitive and transition beds, from the coast of Genoa across the chain of the Bochetta, the plains of Lombardy, the Alps of Saint Gothard, the table-land of Swabia, the mountains of Bareuth, and the plains of Northern Germany, I was struck with the extreme frequency, if not the uniformity, of the horary directions 3 and 4 of the compass of Freiberg (direction from south-west to north-east). This research, which I thought might lead to important discoveries relating to the structure of the globe, had then such attractions for me that it was one of the most powerful incentives of my voyage to the equator. My own observations, together with those of many able geologists, convince me that there exists in no hemisphere a general and absolute uniformity of direction; but that in regions of very considerable extent, sometimes over several thousand square leagues, we observe that the direction and (though more rarely) the inclination have been determined by a system of particular forces. We discover at great distances a parallelism (loxodromism) of the strata, a direction of which the type is manifest amidst partial perturbations and which often remains the same in primitive and transition strata. A fact which must have struck Palasson and Saussure is that in general the direction of the strata, even in those which are far distant from the principal ridges, is identical with the direction of mountain chains; that is to say, with their longitudinal axis.

Venezuela is one of the countries in which the parallelism of the strata of gneiss-granite, mica-slate and clay-slate, is most strongly marked. The general direction of these strata is north 50° east, and the general inclination from 60 to 70° north-west. Thus I observed them on a length of more than a hundred leagues, in the littoral chain of Venezuela; in the stratified granite of Las Trincheras at Porto Cabello; in the gneiss of the islands of the lake of Valencia, and in the vicinity of the Villa de Cura; in the transition-slate and greenstone on the north of Parapara; in the road from La Guayra to the town of Caracas, and through all the Sierra de Avila in Cape Codera; and in the mica-slate and clay-slate of the peninsula of Araya. The same direction from north-east to south-west, and this inclination to north-west, are also manifest, although less decidedly, in the limestones of Cumanacoa at Cuchivano and between Guanaguana and Caripe. The exceptions to this general law are extremely rare in the gneiss-granite of the littoral Cordillera; it may even be affirmed that the inverse direction (from south-east to north-west) often bears with it the inclination towards south-west.

As that part of the group of the Sierra Parime over which I passed contains much more granite* than gneiss, and other rocks distinctly stratified, the direction of the layers could be observed in this group only on a small number of points; but I was often struck in this region with the continuity of the phenomenon of loxodromism. The amphibolic slates of Angostura run north 45° east, like the gneiss of Guapasoso which forms the bed of the Atabapo, and like the mica-slate of the peninsula of Araya, though there is a distance of 160 leagues between the limits of those rocks.

Fear magnifies danger. By the time Andrey Ilyitch was finishing the last course, she had firmly made up her mind to tell her husband everything and to flee from danger!

“I’ve something serious to say to you, Andrey,” she began after dinner while her husband was taking off his coat and boots to lie down for a nap.

“Well?”

Start telling the truth now, and never stop. Begin by telling the trut

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