We saw in Chapter 5 that the solar system is believed to have formed from a collapsing, rotating fragment of a cloud of gas and dust some 4.6 billion years ago. This scientific theory requires that interstellar matter existed before then so that the solar system had something from which to form. Taking this reasoning one step further, if such interstellar matter exists today, perhaps star formation continues.
Matter does indeed exist between the stars. We can see a relatively small amount of it through visible light telescopes (Figure 12-2a); however, the bulk of it is too cold to be seen optically and requires the use of infrared (Figure 12-2b) and radio telescopes. We call all the matter between stars the interstellar medium, and it contains at least 10% of the observed mass in our Galaxy. Observations of the spectra of the interstellar medium reveal that it is composed of gas containing isolated atoms and molecules and tiny pieces of dust. Table 12-1 summarizes the composition of the interstellar medium.
Particle number (%) | Mass (%) | |
---|---|---|
Hydrogen (atoms and molecules) | 90 | 74 |
Helium | 9 | 25 |
Metals* | 1 | 1 |
*In astronomy, all elements except hydrogen and helium are called metals. |
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More than 170 different types of molecules have been discovered in interstellar space, some with as many as 60 molecules bonded together. Among these are molecular hydrogen (H2), carbon monoxide (CO), carbon dioxide (CO2), water (H2O), ammonia (NH3), formaldehyde (H2CO), the sugar glycoaldehyde (C2H4O2), and the 60 carbon-atom buckminsterfullerene (commonly called buckyballs). We can identify these molecules by their unique spectral emissions, just as we can identify elements from atomic spectra.
The dust found in space also has a variety of structures. Some carbon-based (that is, organic) particles out there are typically 0.005 microns (μm) across (10,000 times smaller than the diameter of a typical human hair). Among these are collections of molecules similar to those found in engine exhaust and burnt meat (Figure 12-3), called polycyclic aromatic hydrocarbons (PAHs), which are composed of only carbon and hydrogen atoms. Much larger pieces of space dust have cores of carbon or silicon compounds surrounded with mantles of ice and other materials. These grow to more than 0.30 μm in diameter (nearly 200 times smaller than the diameter of a human hair).
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Working with the knowledge that new stars form from the gas and dust of the interstellar medium, astronomers map this matter to identify places to look for young stars. When it can be seen in the visible part of the spectrum, the gas and dust in the interstellar medium glow as a result of scattered light from stars in its vicinity, as seen in Figure 12-2a. As another example, the interstellar medium is dramatically highlighted by stars in the Pleiades star cluster (Figure 12-4a) located in the constellation Taurus. The bluish haze, starlight scattered by the interstellar gas and dust, is called a reflection nebula. A nebula (plural, nebulae) is a dense region of interstellar gas and dust. Nebulae are often embedded in much larger bodies of gas and dust, called molecular clouds. The largest molecular clouds, called giant molecular clouds, contain upward of a million solar masses of matter and extend up to about 600 light-years across.
The interstellar medium is composed primarily of what kinds of things?
Astronomers identify several other types of nebulae. Most important among these are dark nebulae and emission nebulae. Dark nebulae (Figure 12-4b) are regions of interstellar gas and dust that are sufficiently dense to prevent most of the visible light from behind them from getting to us. They look like regions of empty space, whereas they are actually among the densest of interstellar nebulae. Emission nebulae are regions of interstellar gas and dust that glow from energy they receive from nearby stars, from exploding stars, and from collisions between nebulae (Figure 12-5).
While the effect of a dark nebula is an extreme case, finding more distant gas and dust in space is always difficult because the nearby interstellar medium dims, or even blocks, light from behind it. The same effect occurs on Earth where thin cloud layers in our night sky dim starlight and even prevent us from seeing the stars behind them. This darkening of light by intervening gas and dust in space is called interstellar extinction. Dark nebulae are extreme examples of interstellar extinction.
Even when we can see a star or other object at visible wavelengths through the interstellar medium, it appears redder than it actually is, a phenomenon called interstellar reddening. This effect occurs because short-wavelength starlight is scattered by dust grains more than is the long-wavelength light. (Violet is scattered most, followed by blue, green, yellow, and orange, with red scattered least.) Therefore, when we observe a star through gas and dust, we are seeing less short-wavelength light from it than we would if the interstellar medium were not there (Figure 12-6a). The more gas and dust between the objects and us, the redder the objects appear (Figure 12-6b). Interstellar reddening is different from reddening due to the Doppler shift (see Section 4-7). The Doppler shift causes all wavelengths of electromagnetic radiation to lengthen equally, whereas interstellar reddening, due to the stronger scattering of shorter wavelengths, does not change the wavelengths of the starlight we receive—only their intensities.
We have been able to discover distant stars and clouds of interstellar gas and dust whose visible light is obscured by the nearby interstellar medium because the distant objects emit radio or infrared photons that are scattered relatively little on their way to us. Likewise, we use radio and infrared telescopes to find nearby interstellar gas and dust that, as blackbodies, are too cold to emit much visible light.
Stars form from gas and dust that become Jeans unstable (see Section 5-2). Most of this matter is hydrogen in the form of molecules (rather than atoms). However, molecular hydrogen is relatively hard to detect in space. Therefore, radio astronomers often search for cold interstellar gas in the form of carbon monoxide, CO, which emits lots of photons at short radio (microwave) wavelengths of 2.6 and 1.3 mm. Calculations based on the known abundances of interstellar elements reveal that there are about 10,000 hydrogen molecules (H2) for every CO molecule in the interstellar medium. Consequently, wherever astronomers detect strong emission of CO, they deduce that an enormous amount of molecular hydrogen gas must also be present.
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In mapping the locations of CO emission, astronomers came to realize that interstellar gas and dust are often concentrated in giant molecular clouds. In some cases, these clouds appear as dark nebulae silhouetted against a glowing background light, such as Orion’s famous Horsehead Nebula (Figure 12-5). In other cases, the clouds appear as dark nebulae that obscure the background stars (Figure 12-4b). Some 6000 giant molecular clouds are estimated to exist in our Milky Way Galaxy, and have masses that range from 105 to 2 × 106 M⊙ and diameters that range from 15 to 600 light-years. The density inside each of these clouds ranges from 102 to 105 hydrogen molecules per cubic centimeter—thousands of times greater than the average density of the gas and dust dispersed throughout interstellar space, but some 1015 times less dense than the air we breathe. Having located interstellar matter, we will now consider why some of this gas and dust becomes Jeans unstable, and therefore collapses to form new stars (and planets). We explore this activity by expanding on the material in Section 5-2.
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We will see in detail in Chapter 13 that a supernova is a violent detonation that ends the life cycle of a massive star. The core of the doomed star collapses in a matter of seconds, releasing vast quantities of particles and energy that blast the star’s outer layers into space at speeds of several thousand kilometers per second.
Astronomers have found the ashes (more properly, the gas and dust) of many such dead stars scattered across the sky. These supernova remnants are another type of nebula. Supernova remnants, like the Cygnus Loop shown in Figure 12-7, have a distinctly arched appearance, as would be expected for an expanding shell of gas and dust. As it passes through the surrounding interstellar medium, the supernova remnant collides with preexisting matter, exciting the electrons in the atoms and molecules there, causing the gases to glow. If the expanding shell of a supernova remnant rams into a giant molecular cloud with sufficient speed, it can compress that cloud, making pieces of it Jeans unstable, and thus stimulating star birth in it. As we learned in Chapter 5, there is evidence that such an event happened around the time the solar system formed. For more about seeing nebulae on your own, see Guided Discovery: Observing the Nebulae.
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Distant nebulae—clusters of stars and glowing gases—are among the most impressive objects in the night sky. Binoculars and the naked eye are enough to let you “get your hands dirty” exploring them.
You can observe the Orion Nebula (M42) during winter in the northern hemisphere with the naked eye. The caption for Figure 12-2 tells you how to find the Trapezium stars in the heart of it, visible with good binoculars. More of the Orion Nebula is shown in Figure 12-17.
The North America Nebula and the Pelican Nebula in Cygnus are best spotted in autumn. Pick a dark, moonless night and use binoculars rather than a telescope. Higher magnification reveals too small a region of the sky for you to see the entirety of these vast, dim nebulae. To find them, first locate the bright star Deneb on the tail of Cygnus (using, for example, the star chart for Cygnus in this chapter, the Starry Night™ program, or the star charts at the end of the book). The North America Nebula is located 3° east of Deneb, whereas the Pelican Nebula is located 2° southeast of it. These angles are both very small, so sweep around the sky east of Deneb. If your binoculars are powerful enough, you should be able to see the outlines that give these nebulae their names.
For astronomers, the constellations of Orion and Monoceros comprise one of the most accessible regions of the sky for studying star formation and the interaction of young stars with the interstellar medium. This region of space is covered with giant molecular clouds that can be mapped with radio telescopes tuned to wavelengths emitted by carbon monoxide, as discussed in Section 12-1. Such comprehensive maps of CO emission help astronomers understand how the large-scale structure of the interstellar medium is related to the formation of stars.
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A simple collision between two interstellar clouds can also create regions that are Jeans unstable so that they collapse and form new stars. Likewise, radiation from O and B stars, which are especially bright and hot, will ionize (remove electrons from their atomic orbits) the gas that surrounds them, which then moves away and compresses the nearby interstellar medium (Figure 12-8).
As small regions of a giant molecular cloud become Jeans unstable and collapse, they become denser, preventing light from behind and inside them from escaping. These darker regions are called Bok globules (Figure 12-9a, see also the very small dark nebulae in Figure 12-8), named after astronomer Bart Bok (1906–1983), who first studied them in the 1940s. Infrared observations show compact regions of gas and dust, called dense cores, inside Bok globules. These cores are destined to become stars, as their gravity pulls their matter inward.
Often a giant molecular cloud has several hundred or even thousands of dense cores. In that case, hundreds or thousands of stars form together. Such stellar nurseries will become open clusters of stars like the Pleiades (see Figure 12-4). Open clusters are gravitationally unbound systems, meaning that the stars in them eventually drift apart. As noted in Chapter 5, it is likely that the solar system formed in an open cluster.
At first, a collapsing dense core is just a cool, dusty region thousands of times larger than our solar system. The dense core actually collapses from the inside out. The inner region falls in rapidly, leaving the outer layers of the dense core to drift in at a more leisurely rate. This process of increasing mass in the central region is called accretion, and the newly forming object at the center is called a protostar (Figure 12-9b). The formation of stars with different masses depends, in part, on the density of the interstellar medium from which it forms. Denser gas in a Bok globule can lead to a more massive star forming there, provided that the globule has enough total mass.
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Although fusion has not begun, a protostar emits energy, some of which comes from the compression and heating of its interior caused by the gravitational force from its growing mass of hot gas. However, most of the energy it releases comes from infalling gases colliding with the surface gas of the protostar. Figure 12-10 is an infrared image showing the locations of myriad protostars in and around a nebula in Centaurus.
If a dense core is not spinning, it collapses into a sphere, which ultimately becomes an isolated star. If a dense core is spinning, it collapses into a disk, which may then condense into two or three stars. Or, if the disk has a low enough mass, it may become a single star with orbiting protoplanets, as we discussed in Chapter 5.
What types of events can initiate the process of star formation?
Protostars are physically larger than the main-sequence stars into which they are evolving. A protostar of 1 M⊙, for example, has about 5 times the diameter of the Sun. Because of their large sizes, protostars emit great quantities of radiation and gas (analogous to solar wind), and they can be observed as sources of infrared radiation. At this point, they cannot be seen in visible light because they are enshrouded by their outer layer of gas and dust (see Figure 12-9b). Much matter is still slowly falling inward from the dense core’s outer shell. Eventually, the radiation and particles that flow off the protostar exert enough outward force to halt the infall of this gas and dust. As a result, mass accretion stops, and the protostar becomes a pre–main-sequence star.
Why can’t protostars be observed with visible light telescopes?
A pre–main-sequence star contracts slowly, unlike the rapid collapse of a protostar. When the temperature at its core reaches 107 K, hydrogen fusion begins. As we saw in Section 10-7, this thermonuclear process releases enormous amounts of energy. The outpouring of energy from hydrogen fusion creates enough pressure inside the pre–main-sequence star to stop its contraction. In the final stages of pre–main-sequence evolution, the outer shell of gas and dust finally dissipates (Figure 12-11; see also Figure 12-8). For the first time, the star is revealed via visible light to the outside universe.
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The more massive a pre–main-sequence star is, the more rapidly it begins hydrogen fusion in its core. For example, calculations indicate that a 5 M⊙ pre–main-sequence star starts fusing less than a million years after it first forms from a protostar, whereas a 1 M⊙ pre–main-sequence star takes a few tens of millions of years to begin fusion.
Calculations reveal that the minimum temperature required to start normal hydrogen fusion (see An Astronomer’s Toolbox 10-1: Thermonuclear Fusion) in the core of a star is 10 million K. However, pre–main-sequence stars less massive than 0.08 M⊙ do not have enough gravitational force compressing and heating their cores to ever get this hot. As a result, these small bodies contract to become planetlike orbs of hydrogen and helium, called brown dwarfs (Figure 12-12). See Guided Discovery: Extrasolar Planets and Brown Dwarfs for further discussion of these important, albeit nonstellar, bodies. To date the lowest mass star that has been observed has 0.091 M⊙. This star, part of a binary system, is only 95 times more massive and 16% larger than Jupiter.
Astrophysicists use computers and the equations of stellar structure (described in Section 10-8) to model the evolution of a pre–main-sequence star. By calculating changes in the energy that the contracting star emits, computer simulations can follow its changing position on a Hertzsprung-Russell (H-R) diagram (Figure 12-13). Keep in mind that such an evolutionary track represents changes in a star’s temperature and luminosity, not its motion in space.
Protostars transform into pre–main-sequence stars as they cross a curve called the birth line (see the blue line in Figure 12-13). A star’s exact location on this curve depends primarily on its mass and, to a much smaller extent, on the amount of metal it contains. (Recall from Section 11-6 that all elements other than hydrogen and helium are considered metals by astronomers.)
Spectroscopic observations of pre–main-sequence stars show many are vigorously ejecting gas, often in oppositely directed jets, just before they reach the main sequence. Gas-ejecting stars in spectral classes G and cooler (that is, G, K, and M) are called T Tauri Stars (Figure 12-14), after the first example discovered in the constellation of Taurus. Some astronomers propose that the onset of hydrogen fusion is preceded by vigorous chromospheric activity marked by enormous spicules (see Section 10-2) and flares (see Section 10-6) that propel the star’s outermost layers back into space. In fact, an infant star going through its T Tauri stage can lose as much as 0.4 M⊙ of matter and also shed its cocoon while still a pre–main-sequence star. In light of all this activity, it is not surprising that observations reveal T Tauri stars to be variable, meaning that they change brightness much more than, say, the Sun does today. We will discuss variable stars further in Sections 12-12 and 12-13.
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The lowest mass that an object can have and still maintain the fusion of normal hydrogen into helium, as occurs in the Sun (see An Astronomer’s Toolbox 10-1: Thermonuclear Fusion), is 0.08 M⊙, or about 75 times the mass of Jupiter. Astronomers have discovered hundreds of objects in our Galaxy with less than this mass. Like Jupiter, they are primarily composed of hydrogen and helium, with traces of other elements. Many of them are found in orbit around stars, while some are found as free-floating masses that apparently formed without ever orbiting a star. An intriguing question has arisen: What should these various objects be called?
Although normal hydrogen fusion does not occur in them, bodies with between 13 and 75 times Jupiter’s mass do fuse deuterium (a rare form of hydrogen) into helium and those with between 60 and 75 times Jupiter’s mass also fuse lithium (the element with three protons) into helium. Both of these types of fusion occur very briefly (in cosmic terms) because of the limited supplies of deuterium and lithium in any known object in space. All objects between 13 and 75 times Jupiter’s mass are called brown dwarfs. Objects with less than 13 times Jupiter’s mass that are orbiting stars are extrasolar planets or exoplanets (see Chapter 5), while free-floating bodies with less than 13 times Jupiter’s mass are often called sub-brown dwarfs. Bear in mind that these definitions are still undergoing discussion and revision in the astronomy community.
Because they emit relatively little energy compared to stars, extrasolar planets and brown dwarfs are dim and therefore very challenging to observe. Those in orbit are detected by their gravitational or eclipsing effects on the stars they orbit. The first brown dwarf was discovered in 1994. Named Gliese 229B, it is located in orbit around a star, Gliese 229A (see Figure 12-12), in the constellation Lepus, about 18 ly (6 pc) from Earth. A decade later, an extrasolar planet, 2M1207b, was observed orbiting brown dwarf 2M1207 (Figure 5-15). Hundreds more brown dwarfs have been found, along with more than a dozen sub-brown dwarfs. Many of these are found in active star-forming regions, such as the Orion Nebula (see Figure 12-17) and the Rho Ophiuchi cloud (see the accompanying figure below). Astronomers have also found more than 925 extrasolar planets. In 2002, astronomers observed clouds and storms on a brown dwarf similar to, but probably much larger than, the storms observed on the giant planets in our solar system.
Brown dwarfs of larger mass have the interesting feature that when they fuse deuterium or lithium, the helium they create moves upward, out of the core where it is formed. This helium is replaced with fresh deuterium or lithium fuel to fuse. The upward motion of the helium and downward motion of deuterium and lithium-rich hydrogen are due to convection, and, as a result of this motion, eventually all the deuterium and lithium are consumed. We say that these brown dwarfs are fully convective (for further discussion of fully convective stars, see Section 12-8). This convective behavior is different than we find in the Sun (see Chapter 10), which has a separate core, convective zone, and radiative zone that do not share atoms. Flares have been observed from brown dwarfs. By analogy to the Sun’s flares caused by magnetic fields emerging from its surface, astronomers believe that some brown dwarfs rotate and have magnetic fields.
Based on the numbers and locations of the known brown dwarfs and sub-brown dwarfs, astronomers estimate that there may be as many of these bodies in our Milky Way Galaxy as there are stars. Even in these numbers, brown dwarfs do not contribute a substantial amount of mass or gravitational force in the Galaxy because they have such small individual masses.
Which star arrives on the main sequence first, one that is 0.5 M⊙ or one that is 2 M⊙?
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How are T Tauri stars different from main-sequence stars, like the Sun?
Pre–main-sequence stars more massive than 2 M⊙ become hotter without much change in overall luminosity. The evolutionary tracks of these pre–main-sequence stars thus traverse the H-R diagram nearly horizontally, from right to left (see Figure 12-13). A star more massive than about 7 M⊙ has no pre–main-sequence phase at all. Its gravitational compression is so great that it begins to fuse hydrogen in its protostellar phase.
Until 2004, the upper limit to main-sequence stellar mass was thought to be around 120 M⊙. This number was based on calculations that show that above this mass, protostars rapidly develop extremely high fusion rates in their cores, which lead to extremely high surface temperatures—temperatures so great that their outer layers are superheated and thereby expelled into interstellar space. This expulsion, in turn, decreases their masses and their temperatures. An example of a very massive star in the process of shedding mass as it settles down onto the main sequence is the Pistol Star (Figure 12-15). One of the most luminous stars in our Galaxy, the Pistol Star may have started as a protostar with 200 M⊙. Observations reveal that every few thousand years it expels shells of gas, and it may have less than 10 M⊙ left when the expulsion of matter stops. The entire process of mass loss by very massive stars takes only a few million years.
In 2004, however, astronomers observed a main-sequence star that apparently has between 130 and 150 M⊙. In 2006, they saw the remnants of a star that must have been at least 150 M⊙. In 2010, the star R136a1, was observed to have 265 M⊙. As it has been shedding mass for some time, calculations indicate that its original mass was 320 M⊙. Clearly, our understanding of star formation is very much a work in progress.
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We can detect young open clusters of stars from the magnificent glows they create in the nebulae in which they form. Figure 12-5 and Figure 12-16 show examples of these emission nebulae. Because these nebulae are predominantly ionized hydrogen, they are also called H II regions. To see why H II regions occur, remember that the most massive pre–main-sequence stars, those of spectral types O and B, are exceptionally hot. Their surface temperatures are typically 15,000 to 35,000 K, causing them to emit vast quantities of ultraviolet radiation. This energetic radiation easily ionizes any surrounding hydrogen gas, thereby creating an H II region. Photons from an O5 star can ionize hydrogen atoms up to 30 light-years away.
H II denotes ionized hydrogen, which has no electrons in orbit that can make transitions and give off or absorb photons; therefore, how can we observe it? While some hydrogen atoms in the H II regions are being knocked apart by ultraviolet photons, some of the free protons and electrons approach each other so closely that they combine to become short-lived neutral hydrogen, H I atoms (which are soon re-ionized by ultraviolet radiation). As these new hydrogen atoms assemble, their electrons return to their ground states (n = 1). This downward cascade through each atom’s energy levels, releasing photons with each jump between levels, is what makes the nebula glow. Particularly prominent is the transition from n = 3 to n = 2, which produces Hα photons at 656 nm in the red portion of the visible spectrum (review the emission line spectrum in Figure 4-8c and d). Thus, the nebula around a newborn star cluster often shines with a distinctive reddish hue (see Figure 12-16). Nebulae that have oxygen often look green when seen with the eye through a telescope because this gas has a green emission line at 501 nm. Because the eye is more sensitive to green light than red, the dimmer oxygen emission line appears brighter in our brains than does the Hα line, which shows up well on CCD images, which usually appear red.
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An H II region is a small, bright “hot spot” in a giant molecular cloud. The collection of hot, bright O and B stars that produces the ionizing ultraviolet radiation is called an OB association. The famous Orion Nebula (Figure 12-17; see also Figure 1-4 and Figure 12-2) is an example. Four O and B stars in an open cluster called the Trapezium, at the heart of the Orion Nebula, are the primary sources of the ionizing radiation that causes the surrounding gases to glow. The Orion Nebula is embedded in a giant molecular cloud whose mass is estimated at 500,000 M⊙.
The OB association that creates an H II region also affects the rest of the giant molecular cloud in which it is imbedded (see Figure 12-17 insets). Detailed models indicate that vigorous stellar winds, along with ionizing ultraviolet radiation from these stars, carve out a cavity in the cloud. Where this outflow is supersonic, it creates a shock wave, like the sonic boom created when a whip is snapped (for example, see the shock waves shown in the right inset of Figure 12-17). The shock wave forms along the outer edge of the expanding H II region, compressing hydrogen gas as it passes and thereby stimulating a new round of star birth. As more O and B stars form, they power the expansion of the H II region still farther into the giant molecular cloud. Meanwhile, the older O and B stars left behind begin to disperse (Figure 12-18). In this way, an OB association “eats into” a giant molecular cloud, creating stars in its wake. The inset in Figure 12-18 shows star formation around a single O star.
As noted in Section 12-2, stars are often observed to form in open clusters, such as seen in the nearby Orion Nebula (see Figure 12-17). Numerous other star-forming regions have been identified, and the young open clusters in them offer astronomers a rich source of information about stars in their infancy. By measuring each star’s apparent magnitude, color, and distance, an astronomer can deduce its luminosity and surface temperature. The data for all the stars in the cluster can then be plotted on an H-R diagram, as shown for the Pleiades in Figure 12-4 or for the cluster NGC 2264 in Figure 12-19.
What are groups of high-mass stars called?
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Because all of the stars in a cluster begin forming at the same time, and stars with different masses arrive on the main sequence at different times, astronomers can use the H-R diagram to determine the age of a cluster. For example, note that the hottest stars in NGC 2264 lie on the main sequence. These hot stars have surface temperatures around 20,000 K and are extremely bright and massive. Their radiation also causes the surrounding gases to glow. Most of the stars cooler than about 10,000 K have not yet arrived at the main sequence. These less massive stars, which are in the final stages of pre–main-sequence contraction, are just now beginning to ignite thermonuclear reactions at their centers.
From the H-R diagram of a young cluster we can see which are the lowest-mass stars that have already entered the main sequence. Using this information, along with theories of stellar evolution, we can determine the cluster’s age. The cluster NGC 2264, for example, is roughly 2 million years old. In contrast, nearly all of the stars in the Pleiades (see Figure 12-4b) have completed their pre–main-sequence stage. That cluster’s age is calculated to be about 100 million years, which is how long it takes for the least massive stars to finally begin hydrogen fusion in their cores.
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Open clusters dissipate. As noted earlier, open clusters, such as the Pleiades and NGC 2264, possess barely enough mass to hold themselves together. A star moving faster than the average speed for the cluster occasionally escapes. This lowers the total gravitational force of the cluster, making it easier for other stars to leave. Observations indicate that the stars in most open clusters separate from each other and eventually mix with the rest of the stars in the Galaxy within 10–50 million years after the cluster began forming, although some open clusters last for a few hundred million years.