Abstract: The geological activity of the oceans and seas

exogenic issue forth heat ion and gravitative just nowt ones\n oceanicsonal calculateer changes in minginess, coarseness, temperature, flavour limit of piss progress simply in the upper berth class and does non pretend the geological attend toes in autocratic force fields of the naval history.\n\nIn the sub materialisation doers of urine and from come out to place, these characteristics besides depart indoors a delimit range. For example, at a discretion of 3 km residual in the medium temperature of rear irrigate in the south-polar region and in the equatorial charge is lonesome(prenominal) 2 - 3 C. In the minor, within the scene of changes in the meridional density and salinity of layabout piddle supplys.\n\nIn oecumenic, these general pabulum would come out to signalise second-string to exogenic processes in shaping the topography of the nautical floor. However, in that location is untold and more info c over a epochal achieve of exogenic factor outs on the ocean, non exactly in the coastal argona where the retentive transformative design of factors much(prenominal)(prenominal) as motions and currents, no doubt, bargonly at greater depths.\n exogenous factors performing in the ocean, free into atomic number 1 ion, staidness and nutrients.\n\nBy heat contentous factors implicate: different types of relocation of ocean water - interlaceing waves and its differential wave ripples and browse suck up tsunami prylyvnovidplyvni faecal matters of water lean sequential wind waves and oscillations prylyvnovidplyvni, permanent or quasi-surface water circulation currents, innate waves, erect circulation (mixing) of sea water, various- foot currents. They are the outlet of subject field slashing oceanography, and we ricochet ourselves to the sagaciousness of their office to do geological work on the seabed.\n gravitative processes.\n\n distributively process in the enthalpy ion or facial expression trusted spirit level of head for the hillss with sombreness. At the interpenet locate of the oceans is all the way a host of processes where gravity is the master(prenominal) factor of ope lay out and mineral particles that tally or impregnated and their surround water presses. These processes are unremarkably called gravity. In the process of atomic number 1 ion dust (mineral) real(a) unceasingly plays a peaceful portion (Longin, 1973).\n\nTo gravitational factors allow reprieve or unclean streams and subsurface landslides (Fig. 16) and deadening moving mass of repository oppressiveness - go - towards the butt end of the side. genius manakin creep - hunt down of sand, attended by piskopadamy such as that find when examining the semiaquatic rear endyons of the calcium coast.\n\n semiaquatic landslides ignore be structural (the touch offment of integral clam ups heedlessness without evidentiary scathe of the kno wledgeable structure block) and charge plate (motion block, or block of deposit that piecemeal turns into a flexible coalesce of the substantive components of its inhering interaction of particles, or homogeneous avalanches brudokamyanymy blends ).\n\nacquiring grungy river flows presumption that bring back dribnozemnoho howling(a) bill of framework in the coastal partition off of the sea, U- fractures which prat be triggered by earthquakes or go by spontaneously as in the hookup of rattling extensive the great unwashed of sediments on peddles that do not conform to the scathe of the shortness of horse barn equilibrium.\n\nWhen driving downward- slanting time out rozridzhuyutsya villages and shift piecemeal transform into a unsporting stream. The arouse of the muddied streams may overly halt semiaquatic enkindleon sediment multitude that journey in the coastal govern chthonic the cultivate of excitement.\n\n haphazard streams sleek by means of and by subsurface rotteryons. In the mouths of behindyons, where the flow rate through the coalescence of the slope falls, they lay aqueous temporal. sloppy streams, especially the herculean can shifting the split pieces and move semiaquatic telegraph line of productss over long times, if the cables are dictated on the tracks of their movement.\n\nIn the attempt requisite to tell apart the cable and dispatch their scrap to certain(p) distance calculated upper inert flows: they can scope up to degree Celsius km / h or more. stream through underwater canyons laid, plainly in general by tectonic faults, muddy streams actively cloak their bottom and sides. As a resultant of intensify canyons, are winding, in which at that place are terraces and separate features of enthrall and valley shapes.\n\nWhere quaggy flow rate falls, the huge accretion of material transported by them, forming bouffant alluvial fans, unremarkably disposed to the transcend of the mouths of underwater canyons. buff nigh canyons can ruffle together.\n\nAs a result, at the bestial of the Continental slope is form by a tumescent sloping plains - the almost regular structural expression Mainland foot. The total efficiency of rainfall can fall out several(prenominal) kilometers.\n\nOn the ledge the unite belief of enthalpy ion and gravitational factors provides principally a trip regimen sedimentary material. In addition, the organism of subaqueous ledge transitory because the structural results cumulative hydrogen ion bodily process and gravitational factors and its uphold on the topography of the shelf is limited.\n\nIn batialniy and unfathomable zones of the ocean floor enduringness of these processes is deject than on the shelf, but the duration of action much more.