A pathologic fracture occurs when a weakened bone breaks under normal strain.
A fracture zone formed when a layer of rock breaks under strain and moves is called a "fault." Faults are characterized by the displacement of rock on either side of the fracture, which can occur due to tectonic forces. There are various types of faults, including normal, reverse, and strike-slip faults, each defined by the direction of movement.
When rock bends until it breaks, this process is called "faulting." It occurs due to stress in the Earth's crust, where the accumulated strain exceeds the rock's strength, resulting in a fracture. The movement along the fault line can cause earthquakes and is a key aspect of tectonic activity.
The normal strain is a deformation caused by normal forces such as Tension or Compression that act perpendicular to the cross-sectional area, while the shear strain is a deformation obtained from forces acting parallel or tangential to the cross-sectional area.
The strain theory is a state of deviation from bond angle of a normal tetrahedral angle.
The three types of strain are tensile strain, compressive strain, and shear strain. Tensile strain occurs when an object is stretched, compressive strain occurs when an object is compressed, and shear strain occurs when two parts of an object slide past each other in opposite directions.
The type of strain that results when rock responds to stress by permanently deforming without breaking is known as ductile strain. This occurs when rocks are subjected to high temperatures and pressures, allowing them to bend or flow rather than fracture. Ductile deformation is typically observed in deeper crustal levels where conditions promote such behavior. This contrasts with brittle strain, where rocks break or fracture under stress.
A strain is an overstretched or "pulled" or torn muscle. a sprain is an overstretched or torn ligament (holds bones together at a joint), and a fracture is a crack, chip, break or crush of a bone.
A fracture of a material refers to the separation or breaking of the material into two or more pieces due to applied stress or strain that exceeds its strength. This can occur in various forms, such as brittle fracture, where the material breaks without significant deformation, or ductile fracture, which involves considerable deformation before failure. The nature of the fracture can provide insights into the material's properties and the conditions that led to its failure. Understanding fractures is crucial in fields like engineering, materials science, and structural design to prevent catastrophic failures.
Fracture point
Straining your eyes can lead to discomfort and symptoms such as dryness, fatigue, headaches, and blurred vision. This often occurs due to prolonged periods of focusing on screens or other close-up tasks without adequate breaks. Over time, frequent eye strain may contribute to more serious vision problems if not addressed. Taking regular breaks and ensuring proper lighting and ergonomics can help alleviate eye strain.
The material has to stretch (strain) first before it breaks. For ductile materials, when stretch reaches a certain point it permanently deforms (yield) and continues to carry load until it then breaks as load increases. For brittle materials like glass which do not permanently deform thay simply break without yield.
Strain aging could be described as " normal wear and tear " or the fatigue that is experienced under normal conditions, whereas Dynamic strain would be an out of the normal range stress condition like a one time over stress condition where the sum of much strain aging is experienced in one " dynamic" occurrence.