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  • Pages
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Scientific Names on this Page

Indexed by Global Names
Book Title
Principles of geology
By
Publication Details
London, John Murray, 1837
DOI
Holding Institution
Cambridge University Library
Sponsor
JISC & NEH
Copyright & Usage
Rights:
Darwin Estate and Cambridge University Library

Copyright Status:
In copyright


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Contributed by Cambridge University Library
Annotation Not Available

top-margin annotation ⸮ Has not great force tendeny to break things smoothy, mem pane of glass with bullet


lines 8—15 score
lines 11—12 annotation
lines 14—18 score
line 15 underline "made ... upwards"
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lines 8—17 score
line 10 underline "chiefly"
line 11 underline "historical"
lines 10—11 annotation
lines 14—15 annotation ⸮ ( no doubt generally

lines 11—7 annotation ⸮⸮


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lines 4—6 double score
lines 4—5 annotation ?
line 6 underline "Pacific"
lines 10—14 annotation dip seaward
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lines 16—18 annotation ?


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lines 1—3 unmarked
top-margin annotation Why not estuary ?
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lines 2—5 score
lines 2—9 score
lines 2—8 annotation ? !
lines 3—8 annotation !!


7—figure 122 annotation (too much ?)


line 6bottom-margin annotation first origin ?
     beach ?/


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top-margin annotation [drawing]
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lines 1—3 score
lines 1—3 annotation ?


top-margin annotation [drawing]
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lines 11—2 score
bottom-margin annotation / (Azores ?)
     (Melted lava)
     / Galapagos
     ( throug volcanic rocks)


bottom-margin annotation [drawing]


[continues overleaf] lines 3—1 score
bottom-margin annotation This different from other section & like Patagonia


top-margin annotation (a very admirable specimen of descriptive geology)


bottom-margin annotation Leave out Mosaic flood? flood generally
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figure 157 annotation How far from base of escarpment does gravel extend (1 to 3 ought to be more marked) (than 3 to 4—).
from End Note 2 annotation vertically crossed 224 Capital)

figure 157 annotation show ‹elevation› «inclination» after elevation into dry land /
from Front Note 1 annotation (p.224. — Shows inclination after elevation into dry land)
from End Note 2 annotation vertically crossed 224 Capital)


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top-margin5 annotation [drawing]
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figure annotation ( very good )


figure 162 annotation Diluvius tilted /
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lines 6—8 apparently unintentional mark


top-margin annotation (Doing away anticlinal line
     / hollow ∴ chalk continuous
)
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lines 2—25 annotation transverse valleys. every Crust
     [?]frmtn [ie `formation'?] of liniar valleys
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[continues overleaf] lines 13—1 score
line 4 underline "whole mass"
whole-margin annotation incomprehensilbe to me : { it appears owing to your dread of Elevation Craters }
bottom-margin annotation ridge of unstratified rock vera causa


lines 21—1 score
bottom-margin annotation Make analogy stronger pumpin in , instead of out fluid rock /


figures score
top-margin annotation [[Is there not marine animal, case undistinguishable]]


line 3bottom-margin annotation [drawing]
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lines 9—15 score
lines 2—17 annotation Coast of Brazil
     Fresh water & other formations /


top-margin annotation I think it is an argument for prevalenc of certain ‹ord› classes at formr times, the prevalenc of orders now.— as pachyderms in Tertiary— Deer now /

line 15 score
lines 9—17 annotation ?
     do not understand
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lines 10—3 double score in pale pencil
bottom-margin annotation Galapagos plenty of reptiles
bottom-margin annotation / Distribution of animal at present day , evidenly not owg to mere circumstances: ∴ great lizards not:—


lines 2—11 score
line 1 underline "Andes"
lines 1—9 annotation Unfortunate


lines 4—7 score in pale pencil
line 4 underline in pale pencil "of slate"
lines 4—5 annotation
top-marginline 4 annotation if not composed of mny short parallel lines
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lines 20—7 score
lines 20—9 annotation very remarkable
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lines 7—9 unmarked
figure annotation X
bottom-margin annotation X vry common

figure score
figure annotation very good


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lines 1—12 score in dark pencil

lines 7—2 score in pale pencil
bottom-margin annotation arrival of fresh heated matter


lines 1—4 score
line 5bottom-margin score
line 9bottom-margin score in pale pencil
top-margin annotation good abstract
line 5bottom-margin annotation Snow — Hence Metamorphic ; not like basalt «Cordillera»

bottom-margin annotation in dark brown ink [drawing] [?]hors
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line 2 double score
line 2 annotation wrong reference


lines 4—9 score
lines 5—7 annotation ?
top-margin annotation Does any one ?


lines 3—12 score
lines 5—6 annotation St Jago

lines 14—24 score
lines 21—23 annotation !
line 22 underline "600 ... high"
lines 17—21 annotation wrong


lines 10—23 score
top-margin annotation fragments brougt up much more altered .

bottom-margin annotation in pale pencil colourng matter left dike
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top-margin annotation Wire has been known to crystallize & become brittle from frost ∴ arrangement of particles


lines 1—9 score
lines 11—26 score
lines 1—26 annotation ⸮ would not percolation destroy symmetry ?


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lines 5—8 score in pale pencil
line 6 underline in pale pencil "sponges"
top-margin annotation in pale pencil { permeation of solid coral rock by tides }

[continues overleaf] lines 6—3 score


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lines 8—13 score
lines 10—11 annotation ?
top-margin annotation is this theory or fact


[continues overleaf] lines 5—2 double score
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[continuation] 1—2 score
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lines 1—12 score
top-marginline 7 annotation contras general lowness of Tertiary formations
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lines 13—22 multiple score
line 13 underline "visible"
lines 7—23 annotation almost solely elevation ∵ rests on very hypothesisis


lines 15—8 score
lines 15—11 annotation Who ?
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lines 5—8 annotation Sir J Hersch
line 7 underline in dark pencil "infinitesimal"
lines 7—11 annotation HJS ?


lines 17—10 score
lines 17—4 annotation [drawing]
lines 10—1 score in pale pencil
lines 17—6 annotation Does it not always appear vice versâ


lines 14—15 score
top-margin annotation ⧟ beneath coast of Chili
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top-marginline 9 annotation [drawing]
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top-marginline 13 annotation [drawing]
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lines 22—20 score