Final answer:
The initial radioactive element in the 1.3 billion-year-old pegmatite was U-238, with less than half remaining due to decay. Daughter nuclides, including Ra-226, Rn-222, and Po-210, contribute to the measured radioactivity of 4.2 mR/hr, indicating potential health risks from prolonged exposure to the site's radiation.
Step-by-step explanation:
When we are dealing with a pegmatite that has a measured age of 1.3 billion years and contains uranium-bearing microlite, it's reasonable to start with the assumption that the original radioactive element was U-238. Given that the half-life of U-238 is 4.5 × 10⁹ years, and the pegmatite is 1.3 billion years old, we can calculate that approximately less than half of the original U-238 remains, because the pegmatite has not yet reached its first half-life.
Regarding the exposure danger to humans, the measured radioactivity of 4.2 mR/hr indicates that the site has a significant level of radiation, which can pose health risks with prolonged exposure. Radiation safety protocols must be utilized to minimize exposure, such as limiting time spent near the site, using shielding, and employing personal protective equipment.