The flame and the flood stream free download

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There was more foolery yet, if I could remember it. Farewell, both. He was quick mettle when he went to school. This rudeness is a sauce to his good wit, Which gives men stomach to digest his words With better appetite. For this time I will leave you: To-morrow, if you please to speak with me, I will come home to you; or, if you will, Come home to me, and I will wait for you.

Thunder and lightning. Why are you breathless? O Cicero, I have seen tempests, when the scolding winds Have rived the knotty oaks, and I have seen The ambitious ocean swell and rage and foam, To be exalted with the threatening clouds: But never till to-night, never till now, Did I go through a tempest dropping fire.

Either there is a civil strife in heaven, Or else the world, too saucy with the gods, Incenses them to send destruction. And yesterday the bird of night did sit Even at noon-day upon the market-place, Hooting and shrieking. Come Caesar to the Capitol to-morrow? Cassius, what night is this! It is the part of men to fear and tremble, When the most mighty gods by tokens send Such dreadful heralds to astonish us.

You look pale and gaze And put on fear and cast yourself in wonder, To see the strange impatience of the heavens: But if you would consider the true cause Why all these fires, why all these gliding ghosts, Why birds and beasts from quality and kind, Why old men fool and children calculate, Why all these things change from their ordinance Their natures and preformed faculties To monstrous quality,—why, you shall find That heaven hath infused them with these spirits, To make them instruments of fear and warning Unto some monstrous state.

Now could I, Casca, name to thee a man Most like this dreadful night, That thunders, lightens, opens graves, and roars As doth the lion in the Capitol, A man no mightier than thyself or me In personal action, yet prodigious grown And fearful, as these strange eruptions are.

CASSIUS I know where I will wear this dagger then; Cassius from bondage will deliver Cassius: Therein, ye gods, you make the weak most strong; Therein, ye gods, you tyrants do defeat: Nor stony tower, nor walls of beaten brass, Nor airless dungeon, nor strong links of iron, Can be retentive to the strength of spirit; But life, being weary of these worldly bars, Never lacks power to dismiss itself.

If I know this, know all the world besides, That part of tyranny that I do bear I can shake off at pleasure. Poor man! I know he would not be a wolf, But that he sees the Romans are but sheep: He were no lion, were not Romans hinds. Those that with haste will make a mighty fire Begin it with weak straws: what trash is Rome, What rubbish and what offal, when it serves For the base matter to illuminate So vile a thing as Caesar!

But, O grief, Where hast thou led me? I perhaps speak this Before a willing bondman; then I know My answer must be made. Hold, my hand: Be factious for redress of all these griefs, And I will set this foot of mine as far As who goes farthest.

Metellus Cimber? What a fearful night is this! Is Decius Brutus and Trebonius there? Well, I will hie, And so bestow these papers as you bade me. Let us go, For it is after midnight; and ere day We will awake him and be sure of him. I cannot, by the progress of the stars, Give guess how near to day. Lucius, I say! I would it were my fault to sleep so soundly. When, Lucius, when? It is the bright day that brings forth the adder; And that craves wary walking.

Crown him? He then unto the ladder turns his back, Looks in the clouds, scorning the base degrees By which he did ascend. So Caesar may. Then, lest he may, prevent. Is not to-morrow, boy, the ides of March? Speak, strike, redress! What, Rome? O Rome, I make thee promise: If the redress will follow, thou receivest Thy full petition at the hand of Brutus! Go to the gate; somebody knocks.

Between the acting of a dreadful thing And the first motion, all the interim is Like a phantasma, or a hideous dream: The Genius and the mortal instruments Are then in council; and the state of man, Like to a little kingdom, suffers then The nature of an insurrection. O conspiracy, Shamest thou to show thy dangerous brow by night, When evils are most free?

O, then by day Where wilt thou find a cavern dark enough To mask thy monstrous visage? Seek none, conspiracy; Hide it in smiles and affability: For if thou path, thy native semblance on, Not Erebus itself were dim enough To hide thee from prevention.

Know I these men that come along with you? This is Trebonius. What watchful cares do interpose themselves Betwixt your eyes and night? Here, as I point my sword, the sun arises, Which is a great way growing on the south, Weighing the youthful season of the year.

Some two months hence up higher toward the north He first presents his fire; and the high east Stands, as the Capitol, directly here. But if these, As I am sure they do, bear fire enough To kindle cowards and to steel with valour The melting spirits of women, then, countrymen, What need we any spur but our own cause, To prick us to redress?

I think he will stand very strong with us. But, alas, Caesar must bleed for it! And, friends, disperse yourselves; but all remember What you have said, and show yourselves true Romans. BRUTUS Good gentlemen, look fresh and merrily; Let not our looks put on our purposes, But bear it as our Roman actors do, With untired spirits and formal constancy: And so good morrow to you every one.

Fast asleep? It is not for your health thus to commit Your weak condition to the raw cold morning. Dear my lord, Make me acquainted with your cause of grief. Good Portia, go to bed. What, is Brutus sick, And will he steal out of his wholesome bed, To dare the vile contagion of the night And tempt the rheumy and unpurged air To add unto his sickness? No, my Brutus; You have some sick offence within your mind, Which, by the right and virtue of my place, I ought to know of: and, upon my knees, I charm you, by my once-commended beauty, By all your vows of love and that great vow Which did incorporate and make us one, That you unfold to me, yourself, your half, Why you are heavy, and what men to-night Have had to resort to you: for here have been Some six or seven, who did hide their faces Even from darkness.

Within the bond of marriage, tell me, Brutus, Is it excepted I should know no secrets That appertain to you? Am I yourself But, as it were, in sort or limitation, To keep with you at meals, comfort your bed, And talk to you sometimes?

Dwell I but in the suburbs Of your good pleasure? Knocking within Hark, hark! All my engagements I will construe to thee, All the charactery of my sad brows: Leave me with haste. Boy, stand aside. Caius Ligarius! Would you were not sick! Soul of Rome!

Brave son, derived from honourable loins! Thou, like an exorcist, hast conjured up My mortified spirit. Now bid me run, And I will strive with things impossible; Yea, get the better of them. What it is, my Caius, I shall unfold to thee, as we are going To whom it must be done. Enter a Servant Servant My lord? Servant I will, my lord. You shall not stir out of your house to-day. There is one within, Besides the things that we have heard and seen, Recounts most horrid sights seen by the watch.

O Caesar! Yet Caesar shall go forth; for these predictions Are to the world in general as to Caesar. Of all the wonders that I yet have heard. It seems to me most strange that men should fear; Seeing that death, a necessary end, Will come when it will come. Re-enter Servant What say the augurers? Servant They would not have you to stir forth to-day.

Plucking the entrails of an offering forth, They could not find a heart within the beast. Do not go forth to-day: call it my fear That keeps you in the house, and not your own. Decius, go tell them Caesar will not come. If you shall send them word you will not come, Their minds may change.

Pardon me, Caesar; for my dear dear love To our proceeding bids me tell you this; And reason to my love is liable. I am ashamed I did yield to them. Give me my robe, for I will go. Good morrow, Casca. Good morrow, Antony. Now, Cinna: now, Metellus: what, Trebonius! There is but one mind in all these men, and it is bent against Caesar. If thou beest not immortal, look about you: security gives way to conspiracy. The mighty gods defend thee! My heart laments that virtue cannot live Out of the teeth of emulation.

If thou read this, O Caesar, thou mayst live; If not, the Fates with traitors do contrive. How hard it is for women to keep counsel!

Art thou here yet? Run to the Capitol, and nothing else? And so return to you, and nothing else? Hark, boy! Soothsayer At mine own house, good lady. Soothsayer About the ninth hour, lady. Soothsayer Madam, not yet: I go to take my stand, To see him pass on to the Capitol. Soothsayer That I have, lady: if it will please Caesar To be so good to Caesar as to hear me, I shall beseech him to befriend himself. Soothsayer None that I know will be, much that I fear may chance.

Good morrow to you. Ay me, how weak a thing The heart of woman is! O Brutus, The heavens speed thee in thine enterprise! Sure, the boy heard me: Brutus hath a suit That Caesar will not grant. O, I grow faint. Run, Lucius, and commend me to my lord; Say I am merry: come to me again, And bring me word what he doth say to thee. Exeunt severally. Soothsayer Ay, Caesar; but not gone. Come to the Capitol.

Sediment accumulation consistently occurs whenever discharge rises more than 8, m3 s21 over a few days. These rapid-rise years also correspond to peak discharges. However, there are four slow-rise years with maximum discharges above that threshold, although these events are not recorded in our cores. Beni flood-plain topographic surveys indicate that flood-plain inundation begins when discharges exceed 6, m3 s21, a value exceeded annually However, distal flood plains do not exhibit chronic accumulation.

Sedimentation is episodic in several specific ways: 1 events correspond only to large, rapid-rise floods; 2 neighbouring cores within 1 km typically record the same event, but there is little synchrony between locations tens of kilometres apart; and 3 at any specific location, sediment accumulates only during some floods, with a hiatus of decades typically separating sediment pulses 20—80 cm in thickness.

The environment of depo- sition is low energy and silt rich. Suspended sediment in the Beni river is dominated by fine silts, whereas the bed is composed of sand13,24, so source material for flood-plain sedimentation is derived from high in the water column. Inundation of the entire flood plain by sediment-laden water slowly decanted over levees during annual floods—the local mechanism that constructs the levees—would result in chronic, thin, synchronous sediment accumulation.

Instead, the thick episodic deposits are probably relatively small crevasse splays; delta-shaped deposits formed during levee failure. The banks are composed of loamy deposits susceptible to incision of Figure 2 Unsupported Pb activity profiles circles and clay abundance crosses from representative flood-plain cores.

Increases within the top 10 cm represent meteoric fallout. The meteoric cap is incomplete. X-radiographs depict fine laminations throughout the upper core, with minor Figure 3 Spatial distribution of Beni flood-plain accumulation rates, averaged for five cross-bedding below 80 cm depth. The cap date is X-radiographs do not resolve the lower bound of accumulation events, rates are conservative. Owing to depict fine laminations throughout the core. These examples portray typical episodic rapid channel migration across the flood plain, many of the core sites lay farther from the accumulation events, without chronic sedimentation.

Nearby sites along flood-plain river during the most recent recorded deposition—concurrent river distances were transects record similar events, a characteristic result that suggests that such sediment measured from images Landsat or aerial bracketing the recorded date of each packages blanket regions hundreds to thousands of metres in width and length.

Projected across the flood plains of the Beni foreland basin18, this disintegrations per minute. The lower threshold shows both the minimum rapid flood rise about STI is the average sea surface temperature anomaly in the eastern equatorial Pacific 8, m3 s21 associated with flood-plain accumulation and the mean annual sediment —80 W, 4 N—4 S from November to February the early rainy season months for flux about Mt.

The upper threshold represents the minimum discharge associated Bolivia; temperatures are derived from a standard century-scale oceanographic record Floodwater, decanted sediment storage, exchange and geomorphic complexity. Because from high in the water column, would diverge into the densely sediment supply, transport, deposition and exchange within these vegetated flood plain, depositing an extensive lens of fine sediment major Andean tributaries are orchestrated by extreme climate, such within this low-energy environment.

A failure is more likely when the surrounding flood plain is relatively Received 27 March; accepted 15 August ; doi Conversely, a 1. Kesel, R. An approximation of the sediment budget of the lower high flood plain is typically inundated by sediment-free water28 Mississippi River prior to major human modification. Earth Surf. Landforms 17, — from: 1 local rainfall and tributaries; 2 river water that enters the Aslan, A. Evolution of the Holocene Mississippi River floodplain, Ferriday, Louisiana: traverses the inundated forest; and 3 water that slowly decants insights of the origin of fine-grained floodplains.

Nicholas, A. Investigating spatial patterns of medium-term overbank over bank, depositing its sediment as it crosses the vegetated levees. Hence, only a rapid-rise flood can engender the 4. He, Q. Use of fallout Pb measurements to investigate longer-term rates and critical elevation differential between water in the channel and in the patterns of overbank sediment deposition on the floodplains of lowland rivers.

Landforms 21, — Goodbred, S. Floodplain processes in the Bengal Basin and the storage of Ganges- Crevasse splays, triggered by large, rapid-rise ENSO floods, Brahmaputra river sediment: an accretion study using Cs and Pb geochronology. Mertes, L. Rates of flood-plain sedimentation on the central Amazon River.

Geology 22, — lation across the Bolivian Llanos lowland plains , building strati- Howard, A. Wiley and Sons, Chichester, UK, Pizzuto, J. Sediment diffusion during overbank flows. Sedimentology 34, — James, C.

Sediment transfer to overbank sections. Amazonian lowland Fig. Dunne, T. Exchanges of sediment between variation of sediment supply and transport resulting from the the floodplain and channel of the Amazon River in Brazil.

Allison, M. Importance of flood-plain sedimentation for climate. However, annual water discharge is relatively constant and river sediment budgets and terrigenous input to the oceans: Insights from the Brahmaputra-Jamuna River.

Geology 26, — Aalto, R. Application of fallout Pb geochronology to river-floodplain systems. Pre-Keyed 4K Assets. Overlays can be colored in a variety of ways, polished for a reflective sheen, or customized with stencils and stamps. Upload your logo and wait for the result. Find the best Fire Overlay stock photos for your project. You may like these posts Show more. You can easily add them to your footage by changing blending modes such as Add or Screen.

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