Research online and find a case where physical evidence played an important role in solving the crime. What role did the physical evidence found in crime scene play in solving the crime?

Ted Bundy left the teeth marks on the victim of Chi Omega's murder. This evidence was presented at the court and the match was found between the mark and Bundy's teeth. He was convinced for all the crimes, even though previous witness reports were often dismissed.

Explanation:

In the historic case of serial killer Ted Bundy, the physical evidence was crucial that determined his connection to the crime.

While there was already evidence from testimonies that Bundy can be connected to the various murders that he committed, including evidence of women who saw him leave with the weapon, the physical evidence was crucial at the end.

There were bite marks on one of the victim’s body, and the court insisted to compare those to the casting of Bundy’s teeth. He protested first, probably knowing there will be the match. As suspected, the mark proved to be complementary with the cast of Bundy’s teeth, and a forensic odontologist confirmed the match. Bundy’s teeth were chipped and misaligned, just like the ones that left the mark on the body. This was the only physical evidence found at the scene and it proved to be the crucial one. Bundy was convicted of the murders and crimes he committed.

We can see how crucial physical evidence here is, as Bundy was suspected before for various crimes, even turned in by his girlfriend - his name, car, and appearance matched the records given by the victims and witnesses. However, they were often dismissed by the police and attributed to the emotions and shock. Yet, with this kind of hard physical evidence, it was finally determined Ted Bundy was the one who attacked and murdered the women.

answer; i believe that the correct answer to the above question is; (tariff)

the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)