Answer: <span>A. The hungry housecat killed the small, grey mouse last Tuesday and left it on the doorstep.</span>
<span>With active voice the subject, in this case the housecat is doing the action. So with this sentence, the cat killed the mouse and then left it on the doorstep.</span>
<span>Passive voice sentences usually use the word was like in three of the four examples you gave. </span>
<span>In example B the following wording was used: was left, was killed (that is passive voice).</span>
<span>Example C: was left</span>
<span>Example D: was killed</span>
<span>While example C and D start off using active voice (the hungry housecat killed) it finishes using passive voice. The tenses should remain the same throughout the sentence. </span>
<span>Hopefully this helped and good luck</span>
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Answer: it proves not everyone has the resilience to overcome challenging situations.
Answer:
- It has iambic pentameter.
Explanation:
Blank verse is elucidated as the literary device that involves a regular iambic pentameter(consists of five iambic feet(an unstressed or short syllable followed by a stressed or long syllable)).
In the given excerpt from Robert Frost's 'Mending Wall', <u>the use of 'iambic pentameter'(five metrical feet') makes it fall in the category of blank verse and helps the poet to create the desired rhythm and mood to convey the intended message effectively</u> ('remove the barriers(walls) that prevent socialization or human interaction) to the audience<u>.</u> The poet feels that 'walls are not good for humans as it promotes isolation and segregation.
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
