The table lists properties of a few known elements, but the states of matter and melting points are missing. Look up the element
s in this periodic table. Click an element in the table to reveal its properties. Then add the states of matter (at 20°C) and melting points you find to the table. K
State of matter:
Melting point: °C
Conductivity: good
Solubility (H2O): reacts rapidly I
State of matter:
Melting point: °C
Conductivity: very poor
Solubility (H2O): negligible Au
State of matter:
Melting point: °C
Conductivity: excellent
Solubility (H2O): none
Ge
State of matter:
Melting point: °C
Conductivity: fair
Solubility (H2O): none Ba
State of matter:
Melting point: °C
Conductivity: good
Solubility (H2O): reacts strongly Ar
State of matter:
Melting point: °C
Conductivity: none
Solubility (H2O): negligible
Cl
State of matter:
Melting point: °C
Conductivity: poor
Solubility (H2O): slight Rb
State of matter:
Melting point: °C
Conductivity: good
Solubility (H2O): reacts violently Ag
State of matter:
Melting point: °C
Conductivity: excellent
Solubility (H2O): none
Ca
State of matter:
Melting point: °C
Conductivity: good
Solubility (H2O): reacts Si
State of matter:
Melting point: °C
Conductivity: intermediate
Solubility (H2O): none Xe
State of matter:
Melting point: °C
Conductivity: very poor
Solubility (H2O):
Answer:The Earth's mantle is made up of semisolid rocks. ... The core consists of extremely hot metal layers instead of rock. Iron and nickel make up the outer section of the core, while the interior is almost entirely iron. The inner core is almost totally solid and shaped like a ball.
Respiration occurs when glucose (sugar produced during photosynthesis) combines with oxygen to produce use able cellular energy. This energy is used to fuel growth and all of the normal cellular functions.
