FREE BOOKS

Author's List




PREV.   NEXT  
|<   282   283   284   285   286   287   288   289   290   291   292   293   294   295   296   297   298   299   300   301   302   303   304   305   306  
307   308   309   310   311   312   313   314   315   316   317   318   319   320   321   322   323   324   325   326   327   328   329   330   331   >>   >|  
electors, succeeded in obtaining the see of Winchester for Aymer. The appointment was in every way unsuitable. Aymer was illiterate, ignorant of the English language, and wholly secular in his mode of life. Upon his head was concentrated the whole of the popular indignation against the foreign favourites; and he seems to have deserved this unenviable distinction. At the parliament of Oxford (1258) he and his brothers repudiated the new constitution prepared by the barons. He was pursued to Winchester, besieged in Wolvesey castle, and finally compelled to surrender and leave the kingdom. He had never been consecrated; accordingly in 1259 the chapter of Winchester proceeded to a new election. Aymer, however, gained the support of the pope; he was on his way back to England when he was overtaken by a fatal illness at Paris. See W. Stubbs' _Constitutional History_, vol. ii. (1896); G. W. Prothero's _Simon de Montfort_ (1877); W. H. Blaauw's _Barons' War_ (1871). AYMESTRY LIMESTONE, an inconstant limestone which occurs locally in the Ludlow series of Silurian rocks, between the Upper and Lower Ludlow shales. It derives its name from Aymestry in Herefordshire, where it may be seen on both sides of the river Lugg. It is well developed in the neighbourhood of Ludlow (it is sometimes called the Ludlow limestone) and occupies a similar position in the Ludlow shales at Woolhope, [v.03 p.0074] the Abberley Hills, May Hill and the Malvern Hills. In lithological character it varies greatly; in one place it is a dark grey, somewhat crystalline limestone, elsewhere it passes into a flaggy, earthy or shaly condition, or even into a mere layer of nodules. When well developed it may reach 50 ft. in thickness in beds of from 1 to 5 ft.; in this condition it naturally forms a conspicuous feature in the landscape because it stands out by its superior hardness from the soft shales above and below. The most common fossil is _Pentamerus Knightii_, which is extremely abundant in places. Other brachiopods, corals and trilobites are present, and are similar to those found in the Wenlock limestone. (See SILURIAN.) AYR, a royal, municipal and police burgh and seaport, and county town of Ayrshire, Scotland, at the mouth of the river Ayr, 41-1/2 m. S.S.W. of Glasgow by the Glasgow & South-Western railway. Pop. (1891) 24,944; (1901) 29,101. It is situated on a fine bay and its beautiful sands attract thousands of summer visitors. Ayr proper lies o
PREV.   NEXT  
|<   282   283   284   285   286   287   288   289   290   291   292   293   294   295   296   297   298   299   300   301   302   303   304   305   306  
307   308   309   310   311   312   313   314   315   316   317   318   319   320   321   322   323   324   325   326   327   328   329   330   331   >>   >|  



Top keywords:

Ludlow

 
limestone
 
shales
 

Winchester

 
condition
 
developed
 

Glasgow

 

similar

 

conspicuous

 

nodules


thickness

 

naturally

 
Malvern
 

lithological

 
Abberley
 

Woolhope

 

character

 
varies
 

crystalline

 

passes


flaggy

 

greatly

 

feature

 

earthy

 

Western

 
railway
 

county

 

seaport

 
Ayrshire
 

Scotland


attract

 

thousands

 

summer

 

visitors

 
beautiful
 

situated

 

police

 

position

 

common

 
fossil

Knightii
 
Pentamerus
 

proper

 

stands

 

superior

 

hardness

 

extremely

 

abundant

 
Wenlock
 

SILURIAN