The answer is A because for it to shift to a blue violet it has to increase in temperature
Answer:
power = 142.4 W
Explanation:
power of heater in Germany (P₁) = 523.2 W
power of heater in America (P₂) = ?
outlet voltage in Germany (V₁) = 230 V
outlet voltage in America (V₂) = 120 V
- While in Germany, power =
523.2 = 
R = 101.1
- While in America, also power =
using the value of R gotten above
power = 
power = 142.4 W
Answer:
KE= 30 J
Explanation:
Given that
m= 2.5 kg
r= 0.12 m
θ = 15°
h= 1.2 m
As we know that solid sphere rolls without slipping.It means that
v= ω r
v=Linear velocity
ω=Angular speed
r=radius
The total kinetic energy KE
Moment of inertia of solid sphere I
Now from energy conservation
Energy at top = Energy at bottom
The potential energy at top = m g h
Potential energy at bottom = 0
Kinetic energy at top = 0
Kinetic energy at bottom = KE
m g h + 0 = 0 + KE
KE= 2.5 x 10 x 1.2 ( take g =10 m/s²)
KE= 30 J
Answer;
- Rock layers are placed under compressional stress: Reverse Fault
- Rock layers are placed under tensional stress: Normal Fault
- Hanging wall has dropped relative to footwall: Normal Fault
- Hanging wall has risen relative to footwall: Reverse faults
Explanation;
A normal fault occurs because two tectonic plates are pulling apart from each other, causing tensional stress. The stress allows gravity to pull the hanging wall downward along the footwall, making a cliff-like formation called a scarp. Thus, if you see the hanging wall has dropped relative to the footwall, it is a normal fault. Normal faults occur at divergent boundaries.
A reverse fault happens at convergent boundaries, where two plates colliding produce compressional stress. As the two plates come together, the pressure causes the hanging wall to move upward along the footwall. These breaks are reverse faults because the hanging wall moves in an opposite, or reverse, direction when compared to a normal fault.
A strike-slip fault occurs when tectonic forces cause rock layers to break apart and move in opposite, parallel directions, causing shear stress. The rock layers in a strike-slip fault move sideways past one another.
