Perhaps loyal to a fault—in the sense that he kept around people like Donald Rumsfeld around longer than he should have.
Our nation is going so soft, and it's clearly President Obama's fault.
He is the captain of the ship, and he has publicly stated that this was his fault and his administration failed.
“I realized these rude people were encroaching upon my personal life—my own fault, mind you—for opening the door,” he said.
Hagel was not accusing Israel of being at fault for the "sickening slaughter."
Moreover, the saddest of precisians could find no fault with the conduct of the shop.
The probability was that she had no one to blame but herself—if fault there was.
It wasn't his fault, and he wouldn't take the blame; he was only going by orders all the time.
Why, it would be simply monstrous if your career were spoilt through no fault of your own.
She is sold for no fault, but simply because her owner must have money.
late 13c., faute, "deficiency," from Old French faute (12c.) "opening, gap; failure, flaw, blemish; lack, deficiency," from Vulgar Latin *fallita "a shortcoming, falling," noun use of fem. past participle, from Latin falsus "deceptive, feigned, spurious," past participle of fallere "deceive, disappoint" (see fail).
The -l- was restored 16c., probably in imitation of Latin, but was not pronounced till 18c. Sense of "physical defect" is from early 14c.; that of "moral culpability" is first recorded late 14c. Geological sense is from 1796. The use in tennis (c.1600) is closer to the etymological sense.
late 14c., Scottish, "be deficient;" see fault (n.). Meaning "find fault with" is from mid-15c. Related: Faulted; faulter; faulting.
A fracture in a rock formation along which there has been movement of the blocks of rock on either side of the plane of fracture. Faults are caused by plate-tectonic forces. See more at normal fault, reverse fault, strike-slip fault, thrust fault, transform fault. See Note at earthquake.
Our Living Language : Bedrock, the solid rock just below the soil, is often cracked along surfaces known as planes. Cracks can extend up to hundreds of kilometers in length. When tensional and compressional stresses cause rocks separated by a crack to move past each other, the crack is known as a fault. Faults can be horizontal, vertical, or oblique. The movement can occur in the sudden jerks known as earthquakes. Normal faults, or tensional faults, occur when the rocks above the fault plane move down relative to the rocks below it, pulling the rocks apart. Where there is compression and folding, such as in mountainous regions, the rocks above the plane move upward relative to the rocks below the plane; these are called reverse faults. Strike-slip faults occur when shearing stress causes rocks on either side of the crack to slide parallel to the fault plane between them. Transform faults are strike-slip faults in which the crack is part of a boundary between two tectonic plates. A well-known example is the San Andreas Fault in California. Geologists use sightings of displaced outcroppings to infer the presence of faults, and they study faults to learn the history of the forces that have acted on rocks.