āĻ āĻ¨ā§āĻ¸āĻ¨ā§āĻ§āĻžāĻ¨ āĻāĻ°ā§āĻ¨
āĻ āĻāĻŋāĻ§āĻžāĻ¨ā§āĻ° āĻāĻžāĻˇāĻž āĻ¨āĻŋāĻ°ā§āĻŦāĻžāĻāĻ¨ āĻāĻ°ā§āĻ¨
āĻāĻĒāĻ¨āĻžāĻ° āĻāĻžāĻˇāĻž āĻ¨āĻŋāĻ°ā§āĻŦāĻžāĻāĻ¨ āĻāĻ°ā§āĻ¨
Bedrock
01
āĻāĻŋāĻ¤ā§āĻ¤āĻŋ, āĻāĻ§āĻžāĻ°
principles from which other truths can be derived
02
āĻŽā§āĻ˛āĻŋāĻ āĻļāĻŋāĻ˛āĻž, āĻļāĻŋāĻ˛āĻžāĻ° āĻāĻŋāĻ¤ā§āĻ¤āĻŋ
solid rock beneath surface materials, forming the Earth's crust foundation
āĻāĻĻāĻžāĻšāĻ°āĻŖ
Geologists drilled into the bedrock to collect samples and analyze the composition of the Earth's crust.
āĻā§āĻ¤āĻ¤ā§āĻ¤ā§āĻŦāĻŦāĻŋāĻĻāĻ°āĻž āĻĒā§āĻĨāĻŋāĻŦā§āĻ° āĻā§āĻ¤ā§āĻŦāĻā§āĻ° āĻāĻ āĻ¨ āĻŦāĻŋāĻļā§āĻ˛ā§āĻˇāĻŖ āĻāĻŦāĻ āĻ¨āĻŽā§āĻ¨āĻž āĻ¸āĻāĻā§āĻ°āĻš āĻāĻ°āĻžāĻ° āĻāĻ¨ā§āĻ¯ āĻŦā§āĻĄāĻ°āĻ-āĻ āĻĄā§āĻ°āĻŋāĻ˛ āĻāĻ°ā§āĻāĻŋāĻ˛ā§āĻ¨āĨ¤
āĻ¨āĻŋāĻāĻāĻŦāĻ°ā§āĻ¤ā§ āĻļāĻŦā§āĻĻ
