Question: Which of the inner planets is most large and dense?
About the article "Solar System", section "Earth".

Candidate passages:
The four inner or terrestrial planets have dense, rocky compositions, few or no moons, and no ring systems.
They are composed largely of refractory minerals, such as the silicates, which form their crusts and mantles, and metals such as iron and nickel, which form their cores.
Three of the four inner planets (Venus, Earth and Mars) have atmospheres substantial enough to generate weather; all have impact craters and tectonic surface features such as rift valleys and volcanoes.
The term "inner planet" should not be confused with "inferior planet", which designates those planets that are closer to the Sun than Earth is (i.e.
Mercury and Venus). 
In the warmer inner Solar System, planetesimals formed from rocks and metals cooked billions of years ago in the cores of massive stars.
These elements constituted only 0.6% of the material in the solar nebula.
That is why the terrestrial planets could not grow very large and could not exert large pull on hydrogen and helium gas.
Also, the faster collisions among particles close to the Sun were more destructive on average.
Even if the terrestrial planets had had hydrogen and helium, the Sun would have heated the gases and caused them to escape.
Hence, solar terrestrial planets such as Mercury, Venus, Earth, and Mars are dense small worlds composed mostly from 2% of heavier elements contained in the solar nebula. 
Since the 1990s, astronomers have discovered numerous extrasolar planets (planets that orbit stars other than the Sun).
Many of these planets have masses of order that of Jupiter and so some presumably could resemble Yavin.
No extrasolar planetary satellites have yet been discovered because such objects are extremely difficult to detect with current technology.
However, both Jupiter and Saturn have large satellites, and Saturn's satellite Titan is enshrouded in a dense atmosphere, so it is quite conceivable that some gas giant extrasolar planets which orbit in their stars' habitable zones could have satellites that could have life or be habitable.
One of the most intriguing extrasolar planets is HD 28185 b, which orbits in its star's habitable zone in a circular orbit.
However, such planets are currently predicted to be white, with water clouds needed.
Another such planet is 55 Cancri f. 
The four inner or terrestrial planets have dense, rocky compositions, few or no moons, and no ring systems.
They are composed largely of minerals with high melting points, such as the silicates which form their solid crusts and semi-liquid mantles, and metals such as iron and nickel, which form their cores. 
The original core of the Nice model is a triplet of papers published in the general science journal "Nature" in 2005 by an international collaboration of scientists: R. Gomes, Hal Levison, Alessandro Morbidelli and Kleomenis Tsiganis.
In these publications, the four authors proposed that after the dissipation of the gas and dust of the primordial Solar System disk, the four giant planets (Jupiter, Saturn, Uranus and Neptune) were originally found on near-circular orbits between ~5.5 and ~17 astronomical units (AU), much more closely spaced and more compact than in the present.
A large, dense disk of small, rock and ice planetesimals, their total about 35 Earth masses, extended from the orbit of the outermost giant planet to some 35 AU.
Scientists understand so little about the formation of Uranus and Neptune that Levison states, "...the possibilities concerning the formation of Uranus and Neptune are almost endless."
However, it is suggested that this planetary system evolved in the following manner.
Planetesimals at the disk's inner edge occasionally pass through gravitational encounters with the outermost giant planet, which change the planetesimals' orbits.
The planets scatter inwards the majority of the small icy bodies that they encounter, exchanging angular momentum with the scattered objects so that the planets move outwards in response, preserving the angular momentum of the system.
These planetesimals then similarly scatter off the next planet they encounter, successively moving the orbits of Uranus, Neptune, and Saturn outwards.
Despite the minute movement each exchange of momentum can produce, cumulatively these planetesimal encounters shift (migrate) the orbits of the planets by significant amounts.
This process continues until the planetesimals interact with the innermost and most massive giant planet, Jupiter, whose immense gravity sends them into highly elliptical orbits or even ejects them outright from the Solar System.
This, in contrast, causes Jupiter to move slightly inward.
The low rate of orbital encounters governs the rate at which planetesimals are lost from the disk, and the corresponding rate of migration.
After several hundreds of millions of years of slow, gradual migration, Jupiter and Saturn, the two inmost giant planets, cross their mutual 1:2 mean-motion resonance.
This resonance increases their orbital eccentricities, destabilizing the entire planetary system.
The arrangement of the giant planets alters quickly and dramatically.
Jupiter shifts Saturn out towards its present position, and this relocation causes mutual gravitational encounters between Saturn and the two ice giants, which propel Neptune and Uranus onto much more eccentric orbits.
These ice giants then plough into the planetesimal disk, scattering tens of thousands of planetesimals from their formerly stable orbits in the outer Solar System.
This disruption almost entirely scatters the primordial disk, removing 99% of its mass, a scenario which explains the modern-day absence of a dense trans-Neptunian population.
Some of the planetesimals are thrown into the inner Solar System, producing a sudden influx of impacts on the terrestrial planets: the Late Heavy Bombardment.
Eventually, the giant planets reach their current orbital semi-major axes, and dynamical friction with the remaining planetesimal disc damps their eccentricities and makes the orbits of Uranus and Neptune circular again.
In some 50% of the initial models of Tsiganis "et al"., Neptune and Uranus also exchange places about a billion years (20%) into the life of the Solar System.
However, the results only correspond to an even mass distribution in the protoplanetary disk, and match the masses of the planets, if the switch did take place.