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What was trajans title?

The Roman Emperor.. .. since I guess you mean the Emperor who built the Wall in Britain..


What 3 areas that were added to the roman empire by the end of trajans reign?

Dacia, Nabataea, Arabia.


Are the three types of faults normal faults backward faults and slip faults?

No. Your terminology is close but not quite right. The three main types of faults are normal faults, reverse faults, and strike-slip faults. Strike-slip faults may also be called transform faults.


What were Florence Nightingale's largest faults?

Some of Flo's largest faults were stubbornness, selfishness, and lack of concern in others' well-being


What kind fault lines are there?

There are 6 types of fault lines. Strike-slip faults, dip-slip faults, oblique- slip faults, listric faults, ring faults, and synthetic and antithetic faults.


What are some common wood faults?

cupping, twisting, splitting and knots.


How faults are made?

Faults are created when tectonic plates are stretching or compressing. There are two types of faults which are normal and reverse faults.


How do you write rhyming poem about faults?

Think about some facts you know about faults, and then put them into a sentence. Then, change the words that need to be rhyming words and you should have a poem!


How are earths faults different from your faults?

Your faults are flaws in your personality. Earth's faults are cracks in the ground along which blocks of rock move.


How are are earths faults different from your faults?

Your faults are flaws in your personality. Earth's faults are cracks in the ground along which blocks of rock move.


How are earth's faults different from your faults?

Your faults are flaws in your personality. Earth's faults are cracks in the ground along which blocks of rock move.


What are the three major types of faults are normal reverse and syncline.?

The three major types of faults are normal faults, reverse faults, and strike-slip faults. Synclines are not faults but rather geological structures that describe the folding of rock layers.