YOur abdominal muscles and other stuff idk go do your homework yourself
e) mass movement
The intercarpal joints are the joints between the carpal bones of the wrist. They are plane synovial joints or gliding joints, meaning that the bones produce movement by gliding over each other.
There is no accurate data on the number of people killed by pooping each year. Typically, deaths related to pooping are rare and usually occur due to underlying health conditions or accidents. It is important to practice good hygiene and seek medical attention if any concerns arise during bowel movements.
That part is called a ligament. Ligaments are fibrous tissue that connect bones to each other at a joint and help to stabilize and support the joint during movement.
The humerus bone of the upper arm (the arm in anatomy refers only to the top part of the upper limb i.e. between the elbow and the shoulder). Like all bones it gives shape to the body and acts as an attachment site for the muscles around it. Most of the muscles that actually move the humerus are within the region called the thorax or torso. The humerus joins the thorax at the glenohumeral joint (the shoulder joint) which is a synovial joint, or freely moving joint. It is actually designeda as a ball-and-socket type of joint. At this joint there are many movements that can occur: Flexion (the arm is brought up forwards so the elbow is at shoulder height), extenstion (the reverse of flexion, so the arm is pushed backwards behing the body), Abduction (the arm is lifted up and out from the side, like flapping it); adduction (the arm is lowered back into the side of the body, like unflapping it), if all four of these are combined you get circumduction (swinging your arms around in circles, forming a cone shape); rotation (when the shoulder is turned forwards or backwards). The muscles that are found on and around the humerus are mostly for acting on the forearm, i.e. at the elbow joint. This joint is a synnovial hinge joint and as such only two movements occur here: Flexion (bending the elbow) and Extension (straightening it). Their biceps brachi (or biceps) muscle is also found around the humerus but it is not really very involved in flexion of the elbow as many would believe. It is in fact used for supination of the forearm bone, the radialis, which means it turns the radius over the ulna. When they lie parallel next to each other, this is when the palm is facing forwards. Only when the forearm is fully supinated can the biceps act to flex the elbow joint. Otherwise the braachialis, a synergist to the biceps, does most of the work.
Ligaments are the musculoskeletal structures that connect bones to each other at the joint level. They help stabilize and support the joints by encasing the joint capsule, which contains synovial fluid to lubricate the joint. Ligaments are composed of dense connective tissue, providing strength and flexibility to withstand various movements.
e) mass movement
The joints between the carpal bones in the ankles and wrists are known as Gliding Joints (a type of synovial joint). These joints work by allowing the bones to slide over each other, allowing smooth movements in multiple directions.
The joints between the carpal bones in the ankles and wrists are known as Gliding Joints (a type of synovial joint). These joints work by allowing the bones to slide over each other, allowing smooth movements in multiple directions.
A diarthrotic joint, also known as a synovial joint, is a type of joint that allows for a wide range of motion between the bones it connects. These joints are characterized by a joint cavity filled with synovial fluid, which lubricates the joint and reduces friction. Examples of diarthrotic joints include the knee, elbow, and shoulder, each allowing for various movements such as flexion, extension, and rotation. Their structure comprises articular cartilage, a joint capsule, and ligaments, contributing to both mobility and stability.
The intercarpal joints are the joints between the carpal bones of the wrist. They are plane synovial joints or gliding joints, meaning that the bones produce movement by gliding over each other.
Joint fault is an extense shear joint in basalt flows, dominantly layer-parallel and probably generated initially by the differential inertial movements inside the cooling lava flow of portions with different melt-viscosities. Their planar part is probably conditioned by the isotherms distribution, while curved segments may be related to brittle-ductile fissure propagations along their edges.
During butterfly swimming, the shoulder joint mainly moves in extension and adduction, and the elbow joint primarily moves in extension. The hip joint moves in extension and adduction, while the knee joint moves in extension and slight internal rotation. The ankle joint moves in plantarflexion and inversion.
The deltoid muscle, located on the shoulder, is responsible for arm abduction, flexion, and extension. It has three distinct parts: the anterior (front), lateral (middle), and posterior (rear) deltoids, each contributing to different movements. When the deltoid contracts, it helps raise the arm away from the body, rotate it, and stabilize the shoulder joint during various activities. Overall, the deltoid plays a crucial role in overhead movements and shoulder strength.
The ankle flexes as you place your heel down, then extends as your toes come down to the floor, repeating with each step. In coordination with the ankle flexion, the knee bends, then extends to push the lower leg forward. As the ankle and knee perform their flexion and extension, the hip joint on the same side must also flex and extend, while the spine continually 'adjusts' during the lower limbs' movements.
There is no accurate data on the number of people killed by pooping each year. Typically, deaths related to pooping are rare and usually occur due to underlying health conditions or accidents. It is important to practice good hygiene and seek medical attention if any concerns arise during bowel movements.
Tectonic movements, such as subduction, convergence, and divergence, can reshape the Earth's surface by creating mountains, valleys, and ocean basins. These movements occur at plate boundaries where plates interact and move relative to each other, altering the landscape over millions of years.