Answer:
Elaborative rehearsal
Explanation:
Elaborative rehearsal: In psychology, the term elaborative rehearsal is defined as a phenomenon that is responsible for encoding particular information into an individual's long-term memory with the help of brain-processing that information in depth.
It helps an individual to make an association or connection between a piece of information that he or she is trying to learn and the formerly present information in his or her memory.
It encompasses deep semantic processing of a piece of information yet to be remembered that leads to the development of durable memories and it is considered as more effective as compared to maintenance rehearsal.
In the question above, the given statement signifies the importance of elaborative rehearsal.
Answer:
Options B & D
Explanation:
Bankruptcy refers to a situation where by a people cannot pay their debts. It involves a legal process.
Option B and D are true.
Many major cities have avoided bankruptcy by being placed under the control of financial control boards by their state governments. As such it they are declared bankrupt by a court are brought under the control of independent trustees whose primary objective is to ensure that obligations to bondholders are satisfied in full.
- A: Per the federal bankruptcy code, a municipality can be declared bankrupt but not insolvent is not true because if you are declared bankrupt, it implies that you are either not paying you loan as due or have stopped paying for a while and it also means you are insolvent. A government can be bankrupt if they cannot pay their debts.
Answer:
GLACIAL DEPOSITS
Today, glacial deposits formed during the Permo-Carboniferous glaciation (about 300 million years ago) are found in Antarctica, Africa, South America, India and Australia. If the continents haven’t moved, then this would suggest an ice sheet extended from the south pole to the equator at this time - which is unlikely as the UK at this time was also close to the equator and has extensive coal and limestone deposits. If the continents of the southern hemisphere are re-assembled near the south pole, then the Permo-Carboniferous ice sheet assumes a much more reasonable size.
More evidence comes from glacial striations – scratches on the bedrock made by blocks of rock embedded in the ice as the glacier moves. These show the direction of the glacier, and suggest the ice flowed from a single central point.
