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These sediments are cemented by permafrost and have accumulated periodically over the last 200, 000 years.
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These and sediments
These channels are the main transport pathway for sediments to the deep sea where they form sedimentary deposits.
These sediments are deposited on the rock unit that is going down.
These are the primary inhabitants of salt lakes, inland seas, and evaporating ponds of seawater, such as the deap salterns, where they tint the water column and sediments bright colors.
These sediments then provide an anaerobic environment which protects from further degradation.
These sediments accumulated to form a sedimentary basin, and make up the island's bedrock.
These represent periods where no new sediments were laid down, or when earlier sedimentary layers raised above sea level and eroded away.
These sediments later deposit in the slower lower reaches of the river, elevating the river bed and creating the famous " river above ground ".
These sediments have been dated through Chandronian NALMA
These deposits are located within a mid-depth zone around 300 – 500 m thick in the sediments ( the gas hydrate stability zone, or GHSZ ) where they coexist with methane dissolved in the fresh, not salt, pore-waters.
These were formed by accumulated sediments brought down by the rivers Aude, Orb and Hérault.
These sediments were laid down in the late ( upper ) Paleozoic era, in the Carboniferous period, in deltaic conditions.
These extremely fine-grained sediments are the result of the erosion of soft clay-rich rocks along the Milk River basin in southern Alberta.
These sediments move towards larger and more sizable waterways through a natural process that moves water towards oceans.
These indicator minerals are generally sought in stream sediments in modern alluvial material.
These sediments are poorly consolidated to unconsolidated mixtures of sand, silt, clay, and gravel derived from older rock in the adjacent mountains.
These fluid inclusions provide direct information about the composition of the fluid and the pressure-temperature conditions that existed during diagenesis of the sediments.
These sediments are the cells that are shed by the autopsy and biopsy specimen during processing.
These form a small component of marine sediments, and are known as microfossils from as far back as the early Cretaceous.
These included increasing relative buoyancy in soft sediments by developing spines on the shell, gaining the ability to swim, and in a few cases, adopting predatory habits.
These sediments combined to form what we today call the Furnace Creek Formation.
These plants are terrestrial in origin and are essential to the stability of the salt marsh in trapping and binding sediments.
These sediments extended far to the west of the river itself, accumulating in a shallow basin below the Sierra de Cucapá.
These " sediments " are tightly linked to the type of currents, depth, and the type of water ( salinity, pH, etc.
These sediments often contain the footprints of humans and animals ( most commonly aurochs ) from that period.
These burrows can be very large, over a meter long in sediments that show good preservation, e. g. Jurassic rocks of the Yorkshire Coast ( eastern United Kingdom ), but the width is usually only up to 2 cm, restricted by the size of the organisms producing it.
These and are
These are just another couple of characters to roll.
These men are not callous.
These things are important to almost all Persians and perhaps most important to the most ordinary.
These are traversed by another line of vaults, and thus rooms, arched on all four sides, are formed.
These songs ( practically all Persian music, for that matter ) are limited to a range of two octaves.
These are not, however, differences in federal structure.
These my grandmother left in their places ( they are still there, more persistent and longer-lived than the generations of man ) and planted others like them, that flourished without careful tending.
These are like the initial ways in which the world forces itself upon the self and thrusts the self into decision and choice.
These are suggestive of Selma Lagerlof.
These assumptions lead to an organization with one man at the top, six directly under him, six under each of these, and so on until there are six levels of personnel.
These ways are absolutely irreconcilable because they offer two different recipes for man's redemption from chaos.
These responses are explicable in terms of characteristics inherent in the crisis.
These discoveries are of present interest chiefly to the scientific community ; ;
These are personality factors ; ;
These are, if the research is done with subtlety and skill, researchable topics, but the research is missing.
These moments are historical events in the lives of individual authors with which the student of comparative literature must be frequently concerned.
These lives are in themselves outside of the moral order and are unburdened with moral responsibility.
These conceptions and the manner in which they were transposed into poetry or engendered by poetic form are intrinsic to western life from the time of Aeschylus to that of Shakespeare.
These biographical analogies are obvious, and far too much time has been spent speculating on their possible implications.
These women whose organization grew out of the old suffrage movement are dedicated to Thomas Jefferson's dictum that one must cherish the people's spirit but `` Keep alive their attention ''.
These are, of course, the same people whose support he has only now rejected to seek the independent vote.
These are New York, Pennsylvania, Michigan, Maryland, Missouri, New Jersey, Illinois and Minnesota.
These men are spenders.
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