Dissolving a solute into a solvent disrupts the solvent's ability to form an ordered crystal lattice and lowers its vapour pressure. Both effects are colligative — they depend only on how many solute particles are present, not on what the solute is. The result: the freezing point drops and the boiling point rises, both in proportion to the solute's molality.
This is exactly why salt is scattered on icy roads and why antifreeze (ethylene glycol) is added to car radiators — the dissolved particles depress the freezing point below the ambient temperature and, in the radiator's case, also raise the boiling point of the coolant.
A 3D beaker of solvent where dragging in dissolved solute particles visibly shifts the freezing point down and the boiling point up, with a live phase-change graph plotting both temperatures against concentration.
Both freezing point depression and boiling point elevation are colligative properties: ΔT scales with the van 't Hoff factor times the solvent's Kf or Kb constant times molality, regardless of what the solute actually is.
Drag in solute particles, adjust the van 't Hoff factor and ambient temperature, and switch solvents to see ice crystals form below the new freezing point or bubbles and steam appear above the new boiling point.
Camphor has such a huge cryoscopic constant (Kf ≈ 37.7 °C·kg/mol) that chemists historically used it to measure unknown molar masses just from how much its melting point dropped.