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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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sedimentary<br />

sedimentary Referring to rock that has been<br />

formed by deposition <strong>and</strong> consolidation of preexisting<br />

material. Divided into types: clastic<br />

— consilidation (typically under water) of<br />

fine “s<strong>and</strong>” particles; carbonate — including<br />

oolitic limestones, which are consolidated diatom<br />

shells; organic — coal, which formed from<br />

compressed organic material; <strong>and</strong> evaporite —<br />

rock salt, gypsum. Only sedimentary stones<br />

contain fossils, since they form in ways that will<br />

preserve the structure of organic material.<br />

sedimentary basin In geophysics, a region<br />

in which the Earth’s surface has subsided <strong>and</strong><br />

has been covered by sediments. One mechanism<br />

for subsidence is thermal subsidence: the<br />

lithosphere cools <strong>and</strong> thickens, <strong>and</strong> due to the<br />

increased density of the cooler rocks the lithosphere<br />

sinks. A typical thickness of a sedimentary<br />

basin is a few kilometers but some basins<br />

have a thickness of 10 km or more. Subsidence<br />

is often impeded by the rigidity of the elastic<br />

lithosphere <strong>and</strong> the resulting flexure of the lithosphere<br />

results in near circular or linear basins<br />

with a radius or width of about 200 km.<br />

sediment budget See s<strong>and</strong> budget.<br />

sediment load The amount of sediment being<br />

transported by moving water. Consists of bed<br />

load, suspended load, <strong>and</strong> wash load.<br />

sediment sink A place or process that results<br />

in sediment removal from a beach or littoral system.<br />

A submarine canyon might serve as a sediment<br />

sink, <strong>and</strong> s<strong>and</strong> mining provides another<br />

example.<br />

sediment source The opposite of a s<strong>and</strong> sink;<br />

a source of s<strong>and</strong> for the littoral system or beach.<br />

Cliffs that back a beach, or a river might serve<br />

as sediment sources.<br />

sediment transport The movement of sediment<br />

due to the action of wind or water.<br />

seeing The phenomenon of time dependent<br />

refraction in the Earth’s atmosphere which<br />

moves stellar images around, <strong>and</strong> often breaks<br />

them into multiple subimages. For groundbased<br />

telescope, seeing is the dominant factor<br />

© 2001 by CRC Press LLC<br />

414<br />

limiting resolution. Seeing arises principally in<br />

the air within 50 m of the telescope. Seeing is<br />

reported in seconds of arc, as the size of the apparent<br />

disk of a point source (star). The best<br />

Earth-based sites have seeing of the order of 2<br />

arcseconds. Active optics in telescopes can reduce<br />

the effects of seeing by factors of up to<br />

10, thereby allowing ground-based observations<br />

closer to the diffraction limit.<br />

seiche A stationary water wave usually<br />

caused by strong winds, changes in barometric<br />

pressure, or seismic activity. It is found in lakes,<br />

semi-enclosed bodies of water, <strong>and</strong> in areas of<br />

the open ocean. The period, T ,ofaseiche in<br />

an enclosed rectangular body of water is usually<br />

represented by the formula 2L<br />

√ gd , where L is the<br />

length, d is the average depth of the body of water,<br />

<strong>and</strong> g is the acceleration of gravity. Typical<br />

periods range from a few minutes in small lakes<br />

to a few hours in gulfs.<br />

seismic coupling factor A parameter used<br />

almost exclusively for subduction zone thrust<br />

faults. It is defined as the ratio of the long-term<br />

average rate of fault slip taking place during subduction<br />

earthquakes to the rate of plate convergence<br />

for a given fault area.<br />

seismic gap First, a region that has a potential<br />

to cause large earthquakes, but where large<br />

earthquakes have not occurred for a long time<br />

(seismic gap of a first kind). Second, a region<br />

where seismicity of usual small earthquakes decreases<br />

drastically for some time (seismic gap<br />

of a second kind). The latter sometimes precedes<br />

a forthcoming large earthquake. Seismic<br />

gaps of the first <strong>and</strong> second kinds could be important<br />

clues for long-term prediction of large<br />

earthquakes.<br />

seismic intensity Numerical values which<br />

represent the intensity of earthquake motion at<br />

a point, divided into several classes. Seismic<br />

intensity is determined mainly based on degree<br />

of shaking that the human body feels, also referring<br />

to shaking of surrounding materials, degree<br />

of damage, <strong>and</strong> phenomena associated with<br />

the earthquake. Seismic intensity scales such as<br />

MM, MSK, <strong>and</strong> JMA seismic intensity scales,<br />

which are appropriate to each country, are used.

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