At its core, (from Greek gē ‘earth’ and -logia ‘study of’) is the study of the solid Earth. However, Geology 1 breaks this into two broad sub-disciplines:
Silicates are built around the silicon-oxygen tetrahedron (one silicon atom bonded to four oxygen atoms). The most common silicates you must know: geology 1
The cornerstone of geological thought, introduced by James Hutton in the 18th century, is . Often summarized as "the present is the key to the past," this principle posits that the geological processes we observe today—such as erosion by rivers, volcanic eruptions, and sediment deposition—have operated in the same way and at roughly the same rates throughout Earth's history. At its core, (from Greek gē ‘earth’ and
That shift in perspective is the true goal of . The rocks are speaking. Now, you are learning to listen. Often summarized as "the present is the key