Answer:
dawg
Explanation: lol i ldk what you're talking about tho
Answer:
Some of the resources in the clinical area I work include
Syringes, centrifuge, test strips, autoclave, PCR(polymerase chain reaction) equipment
Explanation: There are several ways through which this equipment as highlighted are maintained and monitored some of which includes
I. Calibration: This is a procedure adopted by organisations in order to ensure that the equipment made use of in their operations five accurate results and it will also help to eliminate errors.
II. Disinfection: This is a procedure adopted by clinicians and organisations with the aim of removing or eliminating all forms of infectious agents in clinical equipment in order to make them safe for use.
III. Cleaning and drying of surfaces: This is another method of maintaining clinical equipments as it will help to prevent rusting and contamination.
IV. The use of SOPs(Standard operating procedures): This is a system that has been adopted by many organisations to ensure that all equipment are operated following best standards as described by the manufacturer and to prevent breakdowns.
The following are ways to monitor their use
I. Hourly checking through the use of checklist: The use of checklist will help to ensure effective monitoring with the aim of identifying possible faults and act to prevent breakdowns.
II. Documenting the duration of use: This is one of the very best way to effectively monitor the use of this equipment as it will help to ensure effective useage and prevent unnecessary breakdowns.
The answer is C) Pathos and ethos
Answer:
Explanation:
1. There are three main types of glacial erosion - plucking, abrasion and freeze thaw.
2. A nunatak is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They are also called glacial islands. Examples are natural pyramidal peaks.
3. A lateral moraine forms along the sides of a glacier. As the glacier scrapes along, it tears off rock and soil from both sides of its path. This material is deposited as lateral moraine at the top of the glacier's edges. Lateral moraines are usually found in matching ridges on either side of the glacier
4. These scratches, "striations," can be used to understand past ice flow. ... Over time, the glacier moves over rock and sediment, leaving striations or striae, on the rock surfaces that can reveal the direction that the glacier was flowing
5. They form in bowl-shaped depressions, also known as bedrock hollows or cirques, located on the side of, or near mountains. They characteristically form by the accumulation of snow and ice avalanching from upslope areas
