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  1. You can sort the data by time of most recent movement (4 inclusive categories) or slip rate (4 exclusive categories). For example, if you want to see the youngest and most active prehistoric faults, one would search for faults that have moved in the past 15,000 years at rates>5 mm/yr. Search Strategies. The database has two search forms.

  2. 17 gen 2020 · Reverse faults form when the hanging wall moves up. The forces creating reverse faults are compressional, pushing the sides together. They are common at convergent boundaries. Together, normal and reverse faults are called dip-slip faults, because the movement on them occurs along the dip direction -- either down or up, respectively.

  3. Faults are an important part of geology and can be categorized in various ways. This blog post offers a brief introduction to the most common type of fault. The 3 types of faults are: Normal faults; Reverse faults; Strike-slip faults; In this blog post, we will learn about these three types of faults and how they are formed.

  4. For all his faults (= in spite of his faults) he was a good father. 5 → through no fault of her/my etc own 6 crack HEG a large crack in the rocks that form the Earth’s surface the San Andreas fault 7 → generous/loyal/honest etc to a fault 8 tennis DST a mistake made when a player is serving the ball in tennis → double fault, loyal, → find fault with somebody/something シソーラス ...

  5. Faults is a 2014 dark comedy psychological thriller film written and directed by Riley Stearns in his feature film debut. The film stars Mary Elizabeth Winstead , Leland Orser , Jon Gries , Beth Grant , Chris Ellis and Lance Reddick .

  6. www.imdb.com › title › tt3021360Faults (2014) - IMDb

    Faults: Directed by Riley Stearns. With Leland Orser, Mary Elizabeth Winstead, Chris Ellis, Jon Gries. A cult deprogrammer is hired to help a couple whose daughter is under the influence of a mysterious cult.

  7. 29 ago 2018 · Types of faults include dip-slip faults, reverse dip-slip faults, strike-slip faults, and oblique-slip faults, named for their angle and their displacement. They can be inches long or extend for hundreds of miles. Where the plates crash together and move underground is the fault plane.