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Redwall is a series of children's fantasy novels by British writer Brian Jacques, published from 1986 to 2011. [1] [2] It is also the title of the first book of the series, published in 1986, as well as the name of the abbey featured in the book, and is the name of an animated television series based on three of the novels (Redwall, Mattimeo, and Martin the Warrior), which first aired in 1999.
The Marlfoxes, backed by an army of water rats, mount a successful invasion of Redwall and steal the tapestry of the long dead hero, Martin the Warrior. The Marlfox Ziral is slain, however, and the remaining Marlfoxes swear revenge on the citizens of Redwall. Mokkan, one of the Marlfoxes, escapes with the tapestry, leaving his siblings behind.
At Redwall, Raga Bol continues to try to break into the Abbey. After an escapade of using a ladder to scale one of the windows, one sea rat manages to enter the Abbey and is about to kill Carrul when Martha suddenly lunges out of her chair and pushes him away, realising she now has the ability to stand and all she needed was will power.
Furgle recognises the disease symptoms and goes to warn Redwall. Dingeye, however, is caught by the small group lead by Dethbrush, and is beheaded with the Sword of Martin the Warrior. Dethbrush takes the Sword from Dingeye's headless carcass. Back at Redwall, a terrible disease has begun ravaging the Abbey.
Redwall is a fantasy novel by Brian Jacques. [1] Originally published in 1986, it is the first book of the Redwall series. The book was illustrated by Gary Chalk , with the British cover illustration by Pete Lyon and the US cover by Troy Howell.
The party then returns to Redwall, where they have a great feast, mainly composing of Dubble's dishes. The Abbey mourns the death of Skurpul, Ruttur, Rooter and Grabul, the moles who died saving Spingo. Nokko then hands over the last Doomwyte jewel and declares the Gonfelins as citizens of Redwall.
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The channels of these rivers and their tributaries eroded major drainage valleys that cut into the sinkhole plain as deep as 122 m (400 ft), 2/3 of the thickness of the Redwall Limestone. The corresponding drop in water table allowed the depth of karstification to exceed that of nearby paleovalleys. The basal conglomerate and sandstone unit in ...