
 
		the basisphenoid;  a process from  that border being applied to  the  external  surface  
 of the parietal.  In youth, the petrous bone enters into the formation  of  the  inner  
 wall  of  the  cranium,  and has  thus the greater  portion of  the lower border of  the  
 parietal  applied to  it.  There  is  a  small  flattened  process from the border of  the  
 parietal resting on the petrous over the  internal  auditory  foramen,  always  present  
 in young skulls.  This process plays an important part in the economy of this region  
 of  the skull, as it expands with increasing years, and  materially  contributes  to  the  
 after  exclusion  of  the  petrous  from  forming  any portion of  the inner  wall of  the  
 skull;  but  in this  it is much  assisted  by the growth of, the false petrous process of  
 the basisphenoid, by the outward growth  of  the basi-occipital  and  by  the  inward  
 and anterior strengthening of  the  basicranial margins of  the exoccipital.  In  adult  
 life,  this portion  of  the parietal  is  closely  applied to the  postauditory  process of  
 the basisphenoid, and anterior to that the border of  the bone is bent downwards and  
 articulated to the posterior division of  the wings  of  the  basisphenoid;  forming  the  
 inner  and  upper  wall  of  that portion of  the great ear-chamber, which is prolonged  
 forwards above the  pterygoid  process  of  the  squamosal.  By its  inward growth it  
 also contributes  to the division  of  this fissure  in the cranial  walls into  two parts:  
 one the foramen lacerum anterius,  defined anteriorly by the posterior division of the  
 wings of  the  basisphenoid,  externally by the  basisphenoid, posteriorly  by  the  false  
 petrous portion of the basisphenoid by the shelving petrous processes of the  parietal,  
 and superiorly by the thickened, lower border of the parietal;  the other the foramen  
 lacerum  posterius,  behind  the  two  last-mentioned  processes  which  define  its  
 anterior border, its inner margin being formed by a deep concavity lying between the  
 Grlasserian  process  of  the  basisphenoid  and  the  strong,  outward  projection of  the  
 basi-occipital which constitutes the anterior border  of  the  precondyloid  foramen  of  
 the  occipital.  The  posterior  wall  is formed  exclusively  by the extremity of  the  
 downwardly,  outwardly  and  forwardly  projecting  strong  ridge  of  the exoccipital,  
 along which  the  lateral  sinus  is placed and which also defines the posterior wall of  
 the precondyloid foramen.  Its upper wall  is  formed  entirely  by  the  thick,  lower  
 border  of  the  parietal.  The  inner  wall  of  the  bone is deeply concave, marked by  
 depressions for the  cerebral  convolutions  and  meningeal  vessels, and by numerous  
 nutrient foramina. 
 .'Frontal  (PI.  XXXIX,  figs.  1  and  2  f   mid  PI.  XL,  fig.  1).—This  bone  
 consists of  a central, vertical  or  cerebro-nasai  plate, the  anterior  surface  of  which,  
 with  the  exception  of  a  narrow  strip  down  the  middle  of  its  anterior aspect and  
 which forms the upper part  of  the  hinder  wall of  the  nares, is  covered on  either  
 side  by  the  ascending plates of  the maxillaries and partially by the upper  extremities  
 of  the  premaxillaries.  Projecting  outwards, forwards  and  downwards  like  a  
 pair of  wings from the external borders of  the vertical plate are the tempero-orbital  
 plates,  to  the  inner  surface  of which  the  ascending  plates  of  the maxillaries are  
 also applied.  The orbit is placed on the under surface of  the free  extremity  of  the  
 plate  and has  behind it  the  pit for  the  reception  of  the  zygoma.  The posterior  
 surface of  this plate constitutes the  anterior  wall  of  the  temporal  fossa.  Projecting  
 backwards,  outwards  and slightly inwards from the base of  the former there is  
 another smaller plate, the temporal, which  forms  the  internal  surface  of  the  temporal  
 fossa. 
 The cerebro-nasal plate when viewed from the cerebral surface is almost quadrangular, 
  and in  young  skulls  the  two  original halves of  the  bone can  be  detected  
 (PI. XL, fig. 1).  In that period of its history it is almost vertical, the most anterior  
 portion of  the  cerebral  lobes  being  lodged  in  two  deep  concavities  in  the  upper  
 two-thirds,  separated  from  each  other  by a moderately developed, internal, vertical  
 crest;  but in aged skulls,  the  internal  surface  of  the  frontal  has  an  upward  and  
 backward  direction  and the  concavities  for the  cerebral  lobes  are  perforated  by  
 numerous foramina.  In two skulls, I  noted a deep pit in the upper part  of  the  left  
 cerebral  fossa close  to the  well-developed,  vertical  crest,  and opposite to it on the  
 other side of  the crest a smaller pit.  These pits  are  probably  due  to  the  presence  
 on the surface of  the brain of  cystic parasites, which, pressing against the skull, produce  
 absorption of its walls (?)  In one brain the surface bore numerous cysts, which  
 in  some  cases had corresponding depressions in the skull.  In  a nearly adult female  
 skull of  which I  have made a vertical section through  the  posterior  extremities  of  
 the  frontals,  a  large  well-defined  sinus occurs on the  left  side;  while  the  corresponding  
 position  of  the  opposite  side  is  filled  up  with  finely  cancellated tissue;  
 in young skulls, however, there are no traces of  these sinuses. 
 The anterior surface of the vertical plate presents a prominent nodose-like ridge,  
 bearing on the sides of  its upper end the minute nasals.  I t  is  continuous  with  the  
 nasal septum, but has a strong twist to the left,  which  confers  on  the  right  side of  
 the  plate  a  longer  surface  than  on  the left.  The sides of  this aspect of  the plate  
 are defined by the orbitotemporal  wings, and below by the  orbitosphenoid  which is  
 invested by the alar processes of  the vomer.  At the  junction of  the orbitosphenoid  
 and parietals, in young skulls, there is an elongated  fissure  or imperfection of  ossification  
 internal  to  where the sphenoidal fissure opens on the anterior surface of  the  
 united bones.  The orbitotemporal plates differ in form, the  right having a  straight  
 anterior  margin, while  the left  is outwardly  curved in  the  upper  first-half of  its  
 extent owing to the sinistral distortion of  the skull.  They are deeply concave  from  
 above downwards and forwards; and their lower extremities, which are thin triangular  
 plates directed downwards, forwards and slightly  inwards,  are  traversed  by  the  
 optic  canals;  a  small  portion  of  their  posterior margin  constituting a part of  the  
 upper boundary of  the  pterygomaxillary  fissure.  The inner surface of  these parts  
 of  the orbitotemporal  plates presents a rather  broad but  shallow furrow, which terminates  
 in the' orbit and along which the nerves and blood vessels pass; and below it  
 are  two small grooves, along which branches of  the second or median branch of  the  
 trigeminal pass into the maxillary to appear on  the  front  aspect  of  that  bone.  At  
 the inner  end  of  the first-mentioned fissure and on the inner wall of  the canal-like  
 continuation of  the sphenoidal fissure, there is a minute orifice,  the  opening  of  the  
 orbitosphenoid  portion  of  the  optic  canal.  So  far  the  two inner branches of  the  
 fifth nerve lie in that canal, and at  this  point  two  nerves  from  the  most  external