Answer:
cords in walkway , horseplay, not locking and tagging out broke machines, tools not put away in proper place
Answer:
(b)- zone of hypertrophy
Explanation:
Hypertrophic cells synthesize alkaline phosphatase by calcifying the surrounding area; prevent the diffusion of substances, this causes chondrocyte death; therefore, the matrix degrades and the lagoons converge, then the blood vessels proliferate in the collarete to vascularize the cavity. The primitive periodic cells migrate to the vascular borders to become osteoprogenitor cells which are attached to the cartilaginous spicules leaving the degradation of the calcified cartilage, then they become osteoblasts. The combination of cartilage and bone matrix forms a mixed spicule.
Endochondral bone growth begins in the second trimester of fetal life and goes to adulthood, in it there is presence of epiphyseal cartilage.
The epiphyseal cartilage has several areas including:
<u>Hypertrophy zone</u>: it is composed of large chondrocytes that accumulate glycogen. The matrix is compressed between the hypertrophied cartilaginous columns.
The process is called OXIDATIVE PHOSPHORYLATION.
Oxidative phosphorylation is the process by which a free phosphate ion is added to ADP in order to produce ATP. This process take place in the mitochondrion and is a major source of energy for anaerobic organisms. The free phosphate ion is usually transferred from NADH or FADH2.<span />
The answer to the given question above would be the second option. If a<span>n ultrasound tech is trying to identify an object, </span>the machine is not functioning well and is not sending out the sound wave, the statement that best describes this situation is that the sound wave will not be made, so there will be no echo received. Hope this helps.
In a dried up lake bed, it is expected for rock salt and evaporite minerals to be observed.
Rock salt, or halite, is the mineral form of sodium chloride ("NaCl" or table salt). Evaporite is a general term for water-soluble mineral sediments that form from the concentration and crystallization of the "mineral-containing (aqueous) solution," mostly by evaporation. They are considered as sedimentary rocks.
Lakes are freshwater bodies and thus usually form non-marine evaporites while oceans and seas form marine evaporites. Nonmarine evaporites include blödite<span>, </span>borax<span>, </span>epsomite<span>, </span>gaylussite<span>, </span>glauberite<span>, </span>mirabilite<span>, </span>thenardit, trona, and also halite, gypsum, and anhydrite (which are more commonly found in oceans and seas).