On a passive continental margin, you can find thick sedimentary layers, wide continental shelves, and less seismic activity compared to an active continental margin.
A subduction zone would be found at an active continental margin, where one tectonic plate is being forced beneath another. This process leads to features such as deep ocean trenches, volcanic arcs, and earthquakes. In contrast, passive continental margins lack these tectonic interactions and are characterized by a relatively smooth transition from continent to ocean basin.
One structure you would find at an active continental margin that you would not find at a passive margin is a subduction zone. Subduction zones occur at active margins where tectonic plates collide, resulting in one plate being forced beneath the other. This process can lead to the formation of volcanic arcs, deep ocean trenches, and earthquakes.
At a passive continental margin, you would find a continental shelf, which is the shallow, relatively flat platform extending from the shoreline, and a continental slope, which is a steeply sloping transition zone between the continental shelf and the deep ocean floor.
In an ideal world this would be a margin that involves some element of compression, so you're looking at a compressional (orogenic) or subducting margin. Anywhere where the crust is thickened generally involves reverse, also known as thrust, faulting.
The land on the margins is often agriculturally enriched by the addition of volcanic ash. Locations in coastal areas are valuable for trade. Which explains why people are willing to live and build cities in areas that are very likely to suffer damage or destruction in the foreseeable future.
On an active continental margin, you would be likely to find an active ocean trench. This structure would generally not occur at a passive continental margin.
A subduction zone would be found at an active continental margin, where one tectonic plate is being forced beneath another. This process leads to features such as deep ocean trenches, volcanic arcs, and earthquakes. In contrast, passive continental margins lack these tectonic interactions and are characterized by a relatively smooth transition from continent to ocean basin.
One structure you would find at an active continental margin that you would not find at a passive margin is a subduction zone. Subduction zones occur at active margins where tectonic plates collide, resulting in one plate being forced beneath the other. This process can lead to the formation of volcanic arcs, deep ocean trenches, and earthquakes.
At a passive continental margin, you would find a continental shelf, which is the shallow, relatively flat platform extending from the shoreline, and a continental slope, which is a steeply sloping transition zone between the continental shelf and the deep ocean floor.
Active sentence: The park ranger could not find any endangered animals in the lorry. Passive sentence: No animals could be found in the lorry by the park ranger. HINT: Use of the word "by" is always a tip off that a sentence is passive. HINT 2: The noun that appears after "by" in any passive sentence can be flipped to the front of the sentence and made into the subject; all passive sentences can be flipped to be active sentences. It often takes thought and re-wording to switch passive to active.
For changing from passive to active voice sometimes the object is understood. In that case the object has to be mentally supplied and then formed into the subject. Thus :- 'It is said he will come' while converting from passive to active will read like this 'Men say he will come'.In passive sentences the doer of the verb is not usually given. Or if it is given then it is - by + noun, this is called the agent egThe mouse was chased by the cat.The agent becomes the subject of an active sentence eg:The catchased the mouse.If the agent is not given in the passive sentence you to find out who or what does the action to make passive into active. egThe Mona Lisa was painted in the 16th century. -- passive_________ painted the Mona Lisa in the 16th century. -- active.
This is an active sentence.To find out if this is active or passive find the verb. The verb in this sentence is 'lost'.The verbs in passive sentences have this form - be verb + past participle.So a single verb - lost - is not a passive verb phrase.Another way you can tell if a sentence is passive or active, is ask yourself who or what did the action of the verb? Who lost jobs? The answer is skilled and unskilled labourers. The phrase skilled and unskilled labourers comes before the verb so it is in the subject position - subject + verb. This will tell you this is an active sentence.In a passive sentence the subject is not given. Or if it is given it is called the agent and is put at the end of the sentence using - by + noun (phrase).This is a passive sentence:In the depression jobs were lost.Or if you want to say who lost the jobs:In the depression jobs were lost by skilled and unskilled workers.
Sentences written in active voice are clearer and more straightforward than those written in passive voice. In active voice, the subject is doing something rather than having something done to them. An example of passive voice is, "He was reading the book his cousin had written." Active voice may read, "He's reading the book his cousin wrote."
The KH-602 has active pickups but the KH-202 has passive pickups. It is possible to convert to active - either EMGs or Seymour Duncan but you would have to find somewhere to put the batteries.
The relationship between the existence of the plume influence and ocean floor topography.
You would need to find a continental rift. The best example of an active continental rift is the East African Rift.
A passive learner is one who seeks employment while sitting at home trying to find a job on Monster.com! An active learner is one who goes to the passive learner's house and uses his computer to start his own business!