relative URLs - definição. O que é relative URLs. Significado, conceito
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O que (quem) é relative URLs - definição

DETERMINING THE RELATIVE ORDER OF PAST EVENTS
Relative dating methods; Relative age; Relative ages
  • volcanic dyke]] (cutting through A, B & C); E – even younger rock strata (overlying C & D); F – [[normal fault]] (cutting through A, B, C & E).
  • Multiple melt inclusions in an olivine crystal. Individual inclusions are oval or round in shape and consist of clear glass, together with a small round vapor bubble and in some cases a small square spinel crystal. The black arrow points to one good example, but there are several others. The occurrence of multiple inclusions within a single crystal is relatively common
  • Schematic representation of the principle of lateral continuity
  • The [[Permian]] through [[Jurassic]] [[stratigraphy]] of the [[Colorado Plateau]] area of southeastern [[Utah]] is a great example of Original Horizontality and the Law of Superposition, two important ideas used in relative dating. These strata make up much of the famous prominent rock formations in widely spaced protected areas such as [[Capitol Reef National Park]] and [[Canyonlands National Park]]. From top to bottom: Rounded tan domes of the [[Navajo Sandstone]], layered red [[Kayenta Formation]], cliff-forming, vertically jointed, red [[Wingate Sandstone]], slope-forming, purplish [[Chinle Formation]], layered, lighter-red [[Moenkopi Formation]], and white, layered [[Cutler Formation]] sandstone. Photo from [[Glen Canyon National Recreation Area]], Utah.

Relative velocity         
  • Relative motion man on train
  • Relative velocities between two particles in classical mechanics
VELOCITY OF AN OBJECT OR OBSERVER B IN THE REST FRAME OF ANOTHER OBJECT OR OBSERVER A
Relative motion; Relative speed
The relative velocity \vec{v}_{B\mid A} (also \vec{v}_{BA} or \vec{v}_{B \operatorname{rel} A}) is the velocity of an object or observer B in the rest frame of another object or observer A.
Relative risk         
  • Risk Ratio vs Odds Ratio
IN STATISTICS AND EPIDEMIOLOGY
Relative Risk; Relative risks; Relative chance; Relative probability; Risk ratio; Adjusted relative risk
The relative risk (RR) or risk ratio is the ratio of the probability of an outcome in an exposed group to the probability of an outcome in an unexposed group. Together with risk difference and odds ratio, relative risk measures the association between the exposure and the outcome.
Relative change and difference         
TECHNIQUES USED TO COMPARE TWO QUANTITIES
Percent error; % difference; Percent Difference; %difference; %ch; Relative difference; Percentage change; Percent change; Relative percent difference; Percentage increase; Relative change; Percent difference; Δ%; %CH; Percentage difference; Percent discrepancy; Log point; Log change
In any quantitative science, the terms relative change and relative difference are used to compare two quantities while taking into account the "sizes" of the things being compared. The comparison is expressed as a ratio and is a unitless number.

Wikipédia

Relative dating

Relative dating is the science of determining the relative order of past events (i.e., the age of an object in comparison to another), without necessarily determining their absolute age (i.e., estimated age). In geology, rock or superficial deposits, fossils and lithologies can be used to correlate one stratigraphic column with another. Prior to the discovery of radiometric dating in the early 20th century, which provided a means of absolute dating, archaeologists and geologists used relative dating to determine ages of materials. Though relative dating can only determine the sequential order in which a series of events occurred, not when they occurred, it remains a useful technique. Relative dating by biostratigraphy is the preferred method in paleontology and is, in some respects, more accurate. The Law of Superposition, which states that older layers will be deeper in a site than more recent layers, was the summary outcome of 'relative dating' as observed in geology from the 17th century to the early 20th century.