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Book Title
Manual of mineralogy
By
Jameson, Robert.
Publication Details
Edinburgh, Archibald Constable & Co, 1821
Year
1821
DOI
https://doi.org/10.5962/bhl.title.49995
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
Page 4
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line 10 annotation is ths emitted from the Trap Rocks near Edinburgh
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Page 6
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line 18 annotation Is found in the oldest primitive rocks
Page 10
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lines 22—27 annotation Owes its deliquesences to the Lime & Magnesia
     Blue & Red colours are owing to the Iron
Page 11
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line 17 annotation Rock salt has never been found in Scotland
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Page 17
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line 7 annotation Sub Sulphate of Alumina
Page 20
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line 10 crossing-out "2" annotation 3
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lines 12—15 annotation γυποσ
     Mentioned by Pliny
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Page 21
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lines 1—2 annotation The purest kind
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line 10 underline "six-sided prism"
line 12 at "3" annotation ∗
lines 13—15 annotation ∗ [drawing]
⇑line 14u "flexible ... elastic"
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Page 22
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line 4 at "period" annotation ∗
line 9 annotation ∗ Mentioned by Pliny
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Page 23
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line 3 underline in pale pencil "porcelain"
lines 7—8 annotation Easily distinguished from Marble by yielding to the Nail
bottom-margin annotation Easily mistaken for Satin Spar, but can be distinguished by its softness
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Page 25
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⇑line 14 underline "Hardness ... 3.5"
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Page 28
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lines 10—11 annotation melts like Ice Before the Blowpipe
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line 36 underline "rare"
line 36 annotation very
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Page 29
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top-margin annotation All Alum is not prepared from this Mineral
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⇑line 7 annotation Always associated with Volcanic Rocks
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⇑line 6 at "Fluor" annotation ∗
bottom-margin annotation ∗ Fluor — called so from being used as a flux
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⇑line 5 underline "Tessular"
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⇑line 1 underline in pale pencil "Cleavage octahedral"
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Page 30
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lines 19—20 [    ]
lines 19—26 annotation False Topaz (& according to their respective colour are called false gems.)
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Page 31
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line 10 at "sky-blue" annotation ∗ Chlorophane
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Page 32
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line 1 annotation Phosphate of Alumina
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line 16 underline "six-sided prism"
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bottom-margin annotation Phosphate of Lime was formerly thought to belong solely to the Animal Kingdom; & after that, it was «thought to be» an animal formation
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Page 34
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⇑line 7 at "or" annotation ∗
⇑line 4 underline "Prismatic"
bottom-margin annotation ∗ First discovered in Arragon
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Page 35
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lines 6—18 annotation [drawings of crystals]
bottom-margin annotation Fragments of Arragonite will scratch Calcareous Spar.
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Page 36
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line 3 underline "Carbonate of Strontian"
⇑lines 12—6 annotation [drawing]t01 115°. 5' [drawing]
t01 - `[drawing]' erased
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Page 37
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line 2 annotation Iceland Spar
Page 38
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lines 20—21 annotation Never contains organic remains
Page 39
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top-margin annotation A block of Statuary Marble values 200 £
line 15 underline "marbles"
lines 4—11 annotation white marble equal to the Sarian is found in small pieces in Sutherland
Page 40
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⇑line 5 annotation ∗
bottom-margin annotation The Break-Water at Plymouth is composed of this rock; & therefore is much attacked by the Pholas.—
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Page 41
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top-margin annotation Sometimes this limestone contains fragments of shells such as the Nautilus &c, & gives rise to a very beautiful appearance.— it is called Fire-Marble
line 20 annotation Is supposed by some to be of volcanic origin
line 21 annotation ∗
bottom-margin annotation ∗ It is disputed whether this mineral is caused by fusion; or by fragments of a broken strata ejected by the Crater
Page 42
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line 18 annotation [drawing] ∗ [drawing]
bottom-margin annotation ∗ Is only found in very small quantities in Scotland; but is found in great plenty in England
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lines 19—21 annotation Formation of distinct concretions
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⇑line 5 annotation occurs only in Secondary rocks
Page 44
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line 4 underline "flint"
lines 1—4 annotation The Flint only occurs in «th» upper deposits
line 9 annotation The newest of the Secondary Rocks
line 11 underline "not ... Scotland"
line 20 underline "Agaric"
lines 19—21 annotation Extends from Flamborough Head down to Sidmouth    so-called because it is found emitting through rocks
     ∗
     ∗ So called from Agaric
Page 45
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lines 3—4 underline "Edinburgh"
lines 3—4 annotation in Salisbury Craigs
lines 11—12 annotation does not yield to the Nail.—
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line 31 annotation Is continually forming
Page 46
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lines 7—9 annotation generally diverging
⇑line 6 annotation ∗
Page 47
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⇑line 13 annotation ∗ Nearly all Rome is built of a compact Variety of this Mineral
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[continues overleaf] ⇑lines 8—2 annotation [drawing] Formation of the Concretions
Page 48
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⇑line 6 annotation ∗
bottom-margin annotation ∗ Easily know by its pearly lustre
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Page 49
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⇑lines 11—8 annotation ∗    So Called from Lucullus. a Romn Consul, who prized these sorts of Marble
bottom-margin annotation ∗ If the variegated specimens be immersed in weak Muriatic Acid The limestone is dissolved, but the animal matter remains.—
line 33 underline "fetid"
bottom-margin annotation Owing to Sulphurs Hydrogen
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Page 50
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line 22 annotation Owes its colours to bituminous matter
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line 26 annotation Often globular
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Page 51
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lines 19—27 annotation [drawing]
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Page 52
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bottom-margin annotation ]: It is Carb. of Lime with Alumina & Silica, met «with» in the Coal Series
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Page 54
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lines 17—23 annotation also accompanied with Copper Pyrites is called Copper Slate
     Owes its dark colour & bad smell to animal matter
Page 55
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top-margin annotation Extends for a very great distance in Europe & varies extremely in thickness
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line 5 annotation Magnesian limestone
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lines 13—14 annotation Called so from Dolumieu a celebrated French Geologist
⇑lines 13—9 annotation Is harder & heavier than limestone
⇑line 5 annotation sometimes it is slightly flexible
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⇑lines 4—3 underline "effervesces ... acids"
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Page 56
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line 7 underline "primitive"
lines 16—17 annotation ∗
     Only occurs in Secondary Rocks
bottom-margin annotation ∗ The Cathedral Walls of the City of York are built with this mineral
Page 57
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line 11 underline "flexible"
Page 58
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line 16 underline "asparagus-green"
Page 59
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lines 16—17 underline "flesh ... red"
Page 61
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line 8 underline "chlorite-slate"
Page 62
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⇑lines 12—11 underline "becomes magnetic"
Page 63
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lines 14—15 annotation The Damascus [?]Street is supposed from this mineral
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⇑line 7 underline "rose-red"
Page 70
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lines 1—3 double score
⇑lines 9—4 annotation from Dr Withering
     [drawing]
Page 71
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⇑line 14 at "Durham" annotation 2
⇑line 9 annotation 2— also in Shropshire
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Page 72
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lines 20—21 annotation Something similar to Porcelain Earth. easily distinguished by its great Sp. Grav.    is called Cawks.
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Page 74
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line 11 annotation Is of most common occurrence
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Page 77
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bottom-margin annotation Calcareous. Fluor. Heavy. Spar. often occur together
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Page 78
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lines 14—18 annotation Celestine looks like some varieties of Quartz ,but of course much «softer»
     called so because the first kind that was descovred was of a blue colour
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bottom-margin annotation ( The term Sparry is nearly synonymous to Foliated )
Page 82
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line 4 annotation ∗
bottom-margin annotation ∗ Occurs most abundantly in the upper parts of the vein
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⇑lines 2—1 underline "becomes ... globule"
Page 85
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⇑lines 4—3 underline "moss ... crusts"
Page 88
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lines 3—4 annotation has lately been met with in Brazil
     ∗
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Page 89
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top-margin annotation ∗ Have not I a specimen of this in my Cabinet?
bottom-margin annotation (Nearly all these Lead Spars are daily forming: thus Spades &c have been found coated with Carb: of Lead)
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Page 98
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line 17 annotation Carb: of Copper
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Page 101
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⇑line 12 underline "fibrous"
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Page 106
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line 4 annotation to shine
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line 14 annotation Arceniate of Copper
line 20 underline "emerald-green"
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bottom-margin annotation ∗ By a late Analysis appears to be Phosphate of Uranium
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Page 107
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line 7 annotation ∗    Phosphate of Uranium
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Page 108
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lines 5—9 crossing-out "Oxide ... 2.0"
Page 114
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lines 4—7 annotation [drawing]
Page 115
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line 17 annotation Phospate of Iron    X    Vivianite
bottom-margin annotation X [drawing]
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Page 118
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line 1 underline "even splendent"
line 2 underline "Writes ... soils"
bottom-margin annotation Occurs in isolated irregular pieces in different strata.—
Page 119
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line 5 annotation Talc is derived from a Saxon word meaning Tallow
line 12 underline "flexible"
line 13 underline "= ... 1.5"
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line 18 annotation χλωροσ
line 25 underline "dark ... green"
line 26 underline "dark ... green"
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Page 120
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lines 9—14 annotation Nearly always contains Magnetic Iron Ore
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Page 121
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lines 4—9 annotation often accompanies & is intermixed with Shock-crystal
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⇑line 10 at "colour" annotation dark Copperish
Page 122
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line 14 annotation in Calton Hill. Arthur Seat, Pentland Hills
     when heated changes into a red which is used as a pigment
⇑line 14 underline "greenish-white"
⇑line 14 annotation pearly
⇑line 5 underline "flexible ... elastic"
⇑line 4u "very greasy"
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Page 123
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top-margin annotation Crayons are prepared from produced Talc mixed with the various colouring matters
line 17 annotation The Chines ornament their walls with ground Talc
bottom-margin annotation (Rouge is made by extracting the colouring matter from Saffron by Carb. of Potash praecipitated by Acetic Ac. ‹then› sediment is well mixed up with powdered Talc.)
Page 124
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lines 2—3 annotation made into Culinary Vessels
lines 12—13 annotation Used for coating Furnaces in Norway
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Page 126
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line 5 annotation & in th [?]Brithen Shropshire
Page 127
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line 10 underline "elastic"
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lines 14—15 annotation Case 2nd. of th Museum begins here
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⇑line 3 underline "Elastic"
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Page 128
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lines 18—21 annotation occurs sometimes associated with Volcanic Rocks
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⇑line 5 annotation ∗    from its scaly structure
⇑line 3 underline "peach ... red"
bottom-margin annotation very beautiful
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Page 129
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line 5 annotation rather unfrequent
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⇑line 9 annotation X Foliated Structure
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Page 130
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line 7 annotation lustre inclining to Metallic
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Page 131
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line 3 underline "colour green"
⇑line 9 annotation ∗
bottom-margin annotation ∗ looks like Bronze
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Page 132
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line 15 underline "serpentine"
⇑line 6 at "shining" annotation Copper colour
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Page 133
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line 12 underline "Island of Skye"
line 16 annotation occurs as a constituent of Greenstone
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Page 134
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line 16 underline "prismatic"
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Page 135
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line 11 underline "iron"
line 11 annotation colouring matter
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⇑lines 2—1 double score
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Page 136
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lines 20—24 annotation Called so from a Dutch officer who first discovered it in the Cape of Good Hope
⇑line 6 annotation X
bottom-margin annotation X generally botryoidal & internally diverging
Page 138
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line 17 underline "secondary ... rocks"
⇑lines 8—7 annotation rests upon Calcareous Spar in drusy Cavities
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Page 139
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⇑line 6 underline "Boracic Acid"
Page 141
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line 5 underline "gr. ... 2.5"
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line 6 underline "Trapezoidal"
line 12 underline "and grey"
lines 6—10 annotation named white Garnet generally assuming the form of Garnets
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Page 142
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line 2 underline "secondary ... lavas"
line 2 annotation ∗
lines 4—6 annotation ∗ The lava generally contains a good deal of Soda. whereas the leucite contains only Potash
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line 22 underline "Soda"
Page 143
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⇑lines 4—2 annotation The crystals are generally twin placed Cross-wise
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Page 147
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line 12 underline "scopiform ... stellular"
line 16 underline "pearly"
lines 12—15 annotation [drawing]
Page 148
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line 12 underline "natron"
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bottom-margin annotation Zeolites (Supposed to be formed by infiltration)
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Page 153
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line 4 annotation Wavellite. Appendix II P333.
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line 9 underline "Fels"
line 9 annotation Signifies a Rock
Page 154
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line 23 underline "Oblique ... prism"
line 13 annotation from the mountain Adula
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Page 156
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line 6 annotation appears to have suffered heat
⇑line 13 annotation One of the most abundant minerals in the crust of the earth
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bottom-margin annotation in pale pencil 08 [×] 65 [=] 520    18 [×] 65 [=] 1170
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Page 157
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line 9 underline "potash"
⇑lines 12—11 annotation contains Soda not like the other Felspars, Potash
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bottom-margin annotation Potash was first detected in the Mineral Kingdom in th Lepidolite
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Page 158
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lines 1—2 double score
line 16 annotation || this perhaps ought to be a distinct species
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Page 159
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line 3 at "Hills" annotation Salisbury Craigs
line 4 at "felspar" annotation ∗    the white variety
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line 16 underline "slaty"
⇑line 9 underline "natron"
Page 160
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line 1 underline "Bass rock"
lines 2—5 annotation Braid Hills
     Pentland Hills
     There must be some 100000x tons of Soda in this rock
⇑line 11 annotation is met with in the centre of solid granite & deep in mines.—
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Page 161
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⇑line 9 annotation For the process of making Porcelain see Jameson's System.
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Page 165
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line 3 annotation from shining
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lines 8—9 annotation The green colour in the secondary rocks of Edinburgh is caused by augite
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⇑line 15 underline "green"/ ⇑lines 3—2 annotation colours owing    {
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Page 167
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lines 11—12 annotation from Coccus a grain
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Page 170
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⇑line 11 underline "Hornblende"
⇑lines 11—7 annotation blended in other rocks
     Refers to its toughness
     contains much less Magnesia than Augite
Page 171
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line 17 underline "Oxide of Iron"
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Page 172
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line 6 underline "Basaltic"
lines 6—7 annotation from occurring in Basalt
line 8 underline "velvet ... black"
line 20 annotation Arthurs Seat
⇑line 10 underline "Asbestous"
⇑line 8 underline "green"
Page 174
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lines 2—3 annotation from a mountain in [?]Semlya land
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⇑line 13 underline "white"
⇑line 8 underline "pearly"
⇑lines 13—10 annotation [drawing]
Page 175
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⇑lines 15—14 annotation is composed of very minute crystals of White Hornblende
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Page 176
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line 4 annotation mountain [?]leather
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line 12 annotation Hornblende
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⇑line 7 underline "Rigid"
Page 177
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⇑line 5 underline "green"
⇑line 7 annotation from Pistachio — green
Page 178
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⇑line 8 underline "large ... distinct"
Page 180
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⇑line 17 underline "smalt-blue"
Page 181
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line 4 annotation Lapis Lazuli. App:II P.317. —
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line 10 annotation from Andalusia in Spain
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Page 182
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lines 6—7 annotation might perhaps used as a substitute for Emery
     from Saussure.
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lines 18—21 annotation Case 3.rd of the Museum, begins here. —
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Page 183
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line 9 annotation ∗    Spinel Ruby
top-margin annotation ∗ Spinel occurs by far most beautifully near Equator
bottom-margin annotation ∗ The most beautiful specimens was in possession of [?]Josephine
line 12 annotation [drawing]
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⇑line 14 underline "Chromic Acid"
⇑line 14 annotation Colouring matter
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⇑line 6 at "Asia—" annotation The most beautiful specimens
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bottom-margin annotation (many gems are composed of Alumina)
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Page 184
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⇑line 10 underline "Hardness= 9.0"
⇑line 5 annotation is highly crystallized Alumina
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Page 185
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line 9 underline "Alumina"
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⇑line 13 underline "Oriental Ruby"
⇑lines 7—6 annotation must be distinguished from the Spinel
     is an uncrystallized Sapphire
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Page 186
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line 3 annotation Chiefly composed of Alumina
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lines 10—12 annotation may be supposed to connect Emery & Sapphire
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Page 187
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line 12 underline "Silica"
Page 188
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line 2 underline "adamantine ... transparent"
line 3 underline "semitransparent"
line 6 underline "pure carbon"
top-margin annotation I think it not impossible that some time Diamond will be found to be a vegetable secretion
Page 189
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line 15 at "Flouric acid" annotation ∗
bottom-margin annotation ∗ Said by some to have been the universal solvent
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Page 190
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⇑line 11 annotation ∗
bottom-margin annotation ∗ when polishing on the wheel it flies into pieces which the true Emerald does not
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Page 191
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⇑lines 9—8 score
⇑line 8 underline "Chrome"
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Page 192
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line 10 annotation ∗
bottom-margin annotation ∗ Beryl is well described by Pliny
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Page 193
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lines 3—9 annotation is an old Saxon word expressing the disagreealbe sound, caused by the friction of two pieces of Quartz
Page 194
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lines 14—18 annotation ∗
     [drawing]
bottom-margin annotation ∗ It is Silica coloured with Iron & Manganese
Page 195
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line 11 annotation in its upper part
lines 15—19 annotation [drawing]
⇑lines 4—3 annotation very rare in Secondary & Tertiary rocks
bottom-margin annotation ∗ in Specimens from Dauphigny have one very large acuminating plane the 5 others being almost evanescent
Page 196
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top-margin annotation sometimes encrusted & interspersed with Chlorite
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line 8 underline "Cairngorm stones"
line 10 annotation are distinguished from Topaz by inferior Sp. Grav. & Hardness
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line 12 annotation ∗
line 18 annotation never occurs crystallized
line 26 annotation Silica coloured by Manganese
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⇑line 10 annotation ∗
⇑lines 5—4 annotation [drawing]
bottom-margin annotation ∗ When kept in dry places, exposed to the light, looses in a few years «looses» its colour
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Page 197
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top-margin annotation X The massive variety is easily distinguished «from all other minerals» by its superior hardness
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lines 4—5 annotation A flexible variety occurs in Arthurs Seat
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line 21 annotation from its light green colour.—
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Page 198
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⇑line 11 annotation ∗
bottom-margin annotation ∗ Common Quartz impregnated with Iron
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Page 200
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line 2 annotation wood petrified with Hornstone
bottom-margin annotation (The Tick tree in Calcutta has been known to form a strong Mineral , like Woodstone)
Page 201
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line 8 underline "greyish-black"
line 8 annotation owing to Bituminous matter
line 12 annotation is often traversed by veins of white Quartz
line 18 annotation That variety which is free from veins is used for touchstone
line 17 annotation ∗
bottom-margin annotation ∗ by comparing the streak of the pure gold, with that of the specimen assaying
Page 202
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top-margin annotation is of rare occurrence in Scotland owing to the scarceness of Chalk
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lines 10—13 annotation The base of pudding ‹f› stone is quartz; the concretions flint
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line 13 annotation from Calcedon in Asia Minor
line 16 annotation X
line 18 underline "blue"
lines 18—21 annotation where blue is called Sapphirine by the Jewellers
bottom-margin annotation X The dendritic variety is called Mocha Stone from a place in India or from a German word signifying moss, this appearance is owing to Iron & Manganese
Page 203
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line 2 annotation X
top-margin annotation X is mentioned by Pliny as a different mineral
line 4 underline "apple-green"
line 4 annotation owing to Nickel
⇑line 8 annotation from its colour
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Page 204
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line 14 underline "green"
lines 14—16 annotation The green colour is owing to Green earth
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⇑line 9 annotation origin of name disputed
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⇑line 5 underline "Egyptian"
⇑line 5 annotation ∗
bottom-margin annotation ∗ mentioned by Dr. Clarke as occurring near Cairo in great plenty
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Page 206
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line 2 annotation X
top-margin annotation x Clay long exposed to heat
lines 14—15 annotation is Quartz combined with Alumina
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⇑line 4 annotation X
bottom-margin annotation X some varieties are called Eye-Stones
     [drawings]
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Page 207
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bottom-margin annotation (All these Romboidal quartz when heated & thrown into water, splits in direction of its cleavage)
Page 208
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⇑line 5 annotation is daily forming
Page 210
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line 6 annotation (minute portions have been found in Scotland
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⇑lines 6—5 annotation has lately been found in Mexico & Faroe Islands
Page 212
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⇑lines 13—10 annotation distinguished from Jasper by superior lustre
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Page 213
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line 10 annotation in New-Holland
line 18 annotation from Menil, a hill near Paris
Page 214
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⇑lines 11—10 annotation from Obsidian a Roman
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Page 215
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lines 5—8 score
lines 5—8 annotation Colouring matter
     & Carbonaceous matter
line 16 annotation often with imbedded portions of Pearl-stone
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⇑line 16 annotation X    from its resinous appearance
bottom-margin annotation X black colour owing to Carbonaceous matter
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Page 216
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line 3 annotation in Arran
Page 218
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line 7 annotation the crystals resemble the head of an axe
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Page 219
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⇑line 10 underline "Iron"
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⇑line 3 annotation ∗
bottom-margin annotation ∗ Is Chrysolite in a less perfect form. .
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Page 220
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top-margin annotation Meteoric Iron often contains a mineral like Chrysolite or Olivine —
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line 12 annotation near Edinburgh — Arthur Seat
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line 13 annotation Borate of Magnesia
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⇑lines 8—7 double score
⇑line 1 at "imbedded" annotation always
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Page 221
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line 15 underline "red"
line 15 annotation Bubulite
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bottom-margin annotation (Boracic Acid is found in Salisbury Craigs)
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Page 222
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line 11 annotation occasionally contains a little Boracic Acid
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line 18 annotation from a village in Saxony.
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Page 224
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⇑line 8 annotation signifying a Gooseberry
Page 225
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line 19 annotation from μελασ niger
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Page 226
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line 2 annotation ∗
top-margin annotation ∗ From the different colours it undergoes under the blowpipe
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Page 227
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top-margin annotation «Many of the» Carbuncles of the ancients are garnets: the origin of the name— signifying its shining in the dark is erroneous, this word sometimes refers to th Ruby & Sapphire
Page 228
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lines 6—7 annotation from its beautiful red colour
line 18 underline "Acid of Chrome"
line 24 annotation is called the Bohemian Garnet.
Page 230
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⇑line 12 underline "Zirconia"
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Page 232
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⇑line 5 annotation ∗
bottom-margin annotation ∗ not unlike Hyacinth ,distinguishes from yielding to the knife
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Page 234
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line 9 annotation from oxide of Titanium
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Page 236
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line 22 annotation Oxide of Copper
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Page 238
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⇑line 4 annotation Oxide of Tin
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Page 240
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bottom-margin annotation Distinguished from Tin Ore by its streaks being of reddish «brown» colour; Tin ore having a yellow «grey» colour
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Page 243
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line 1 annotation ∗
top-margin annotation Streaks yellowish
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⇑line 4 annotation (Streaks a distinguishing character)
bottom-margin annotation Occurs in Magnesian rocks. such as Talc & Serpentine. —
Page 244
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lines 5—6 underline "Streak black"
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line 10 underline "Magnetic"
lines 9—10 annotation The magnetic property only occurs in rocks near the surface.—
⇑line 6 annotation when pure, affords 70 per cent of Iron
Page 245
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line 10 annotation in Salisbury Craigs
lines 14—15 underline "Streak ... brown"
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⇑line 9 underline "tarnished"
⇑line 4 underline "splendent"
Page 246
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top-margin annotation (The Magnetic Iron Ore occurs in greater plenty in the North, The Specular in the South)
lines 17—19 annotation occurs in plates in the crevices of Volcanic Rocks. as. Vesuvius
line 19 annotation ∗
bottom-margin annotation ∗ distinguished from Mica, by the rigidity of the Plates
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Page 248
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⇑line 17 underline "botryoidal"
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Page 250
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line 18 annotation ∗    Hydrate of Iron
line 21 underline "yellowish-brown"
bottom-margin annotation ∗ Makes better Steell than the two former varieties
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Page 251
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line 13 underline "Water"
Page 254
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lines 7—8 annotation ∗
     is daily forming in boggy places
bottom-margin annotation ∗ Is well adapted for making cast-Iron
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Page 263
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⇑line 9 annotation Occurs in newer formations than the last. —
Page 266
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line 2 underline "dendritic"
top-margin annotation formed of crystals; in this mineral, by cubes
line 13 annotation because when struck gives out sparkes
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line 19 annotation Arsenuent of Nickel
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Page 273
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line 2 annotation X
top-margin annotation X decays more rapidly than th other varieties
Page 274
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line 18 underline "magnetic"
Page 275
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line 10 underline "brass"
top-margin annotation does not afford sparks with steel
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Page 280
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line 2 annotation X continues to be formed by aqueous means
Page 289
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⇑line 11 underline "specular-splendent"
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Page 294
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⇑line 2 annotation associated with Native Arsenic
Page 295
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⇑line 9 annotation along with compact Gypsum
Page 296
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top-margin annotation Every time volcano emits sulphur, mostly in form of Vapour. —
Page 298
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top-margin annotation (all the insects inclosed in amber are extinct.) & different from those now alive
Page 299
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⇑line 13 annotation Pitchford & Coal-Brook Dale
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Page 300
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top-margin annotation The walls of Babylon were cemented by melted Mineral pitch
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line 6 underline "splendent"
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line 19 annotation Mineral Caoutchouck
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Page 301
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line 18 annotation the remains of ancient trees.—
Page 302
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line 10 annotation but must be mixed with some connecting matter
Page 303
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line 31 annotation common Coal
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Page 304
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line 5 annotation the most common variety
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bottom-margin annotation Is of older formation than the Browne.— (was formed before Mammalia Aves Amphibia but there existed fishes & shells)
Page 305
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lines 8—9 underline "metallic lustre"
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⇑line 4 annotation X
bottom-margin annotation X little Bituminous matter
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Page 307
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bottom-margin annotation The Browne coals when burnt emit a very bad smell
     The Glanc Coals never contain vegetables were formed before vegetables existed
Page 317
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lines 14—19 annotation Iron Pyrites is often disseminated in it, & then is mistaken for Gold.
line 23 annotation ∗ Lapis Lazulis has been met with in Vesuvius
bottom-margin annotation Origin disputed, whether formed, or merely broken fragments.—
Page 333
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lines 6—7 annotation [drawing]
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Page 337
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line 22 underline "Compound"
line 22 annotation not homogeneous
Page 338
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⇑line 4—bottom-margin annotation [drawing]
bottom-margin annotation a basis including crystals
Page 339
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lines 5—11 annotation [drawing]
     a basis containing cavities or other foreign substances of an amygdaloidal form
⇑lines 10—4 annotation vid: the secondary rocks of Arthur Seat
     [drawing]
⇑line 9 annotation ∗
bottom-margin annotation ∗ the grains joined without basis or cement.—
Page 340
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lines 19—20 underline "slaty ... large"
lines 10—20 annotation [drawing]
     A Slaty B Granular
⇑line 11 underline "Granular"
⇑lines 12—11 annotation of rarer occurrence
     Base granular
⇑line 6 underline "Slaty"
⇑line 6 annotation Base slaty
Page 341
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lines 2—5 annotation [drawing]
line 11 annotation of frequent occurrence in th Calton Hill
bottom-margin annotation [drawing]
Page 342
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⇑line 3 annotation ∗
bottom-margin annotation ∗ [drawings] ∗
Page 344
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bottom-margin annotation (Hydrogen & Nitrogen are emitted in greater quantities in some Volcanic countries)
Page 346
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lines 16—26 annotation [drawings] Hornblende
     Felspar
     Syenite
bottom-margin annotation in pale pencil (Felspar is distinguished from Quartz by its inferior hardness, yielding to knife)
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Page 361
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line 15 annotation These four rocks, generally occur in the order here placed
     minute scales of Mica
Page 365
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⇑line 13 annotation according to the formation, so is the state of crystallization
Page 369
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⇑line 9 annotation so called from its resemblance to the colouring of Serpents —
Page 370
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top-margin annotation a mixture of Marble with Serpentine is called Verde Antique.—
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bottom-margin annotation Magnesia occurs in the greatest quantity in the newer Primitive Rocks, as Serpentine
Page 371
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⇑line 10 annotation perhaps ought to be considered a variety of [?]pormilica Greenstone
Page 377
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lines 5—10 annotation is clayslate with imbedded fragments
     [drawing]
Page 382
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bottom-margin annotation 1 Old Red Sandstone
     2 Mountain Limestone
     3 Bed Conglomerate
     4 Magnesia Limestone
     5 New Red Sandstone
     6 Shell Limestone
     7 3rd Sandstone formation
     8 Oolite
     [continues on page 383] 9 (Sand Clay Marl.) Chalk Marl
     10 Chalk formation
Page 383
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line 10 annotation 1
Page 384
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bottom-margin annotation It is disputed that this rock is of the primitive series
Page 385
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⇑line 3 underline "a ... streak"
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Page 386
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line 4 underline "a dull streak"
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line 17 annotation ∗
bottom-margin annotation ∗ Sometimes contains Iron Pyrites, which from its decomposing entirely unfits for building
Page 387
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line 10 underline "Trap"
line 10 annotation X
top-margin annotation X The Trap in this formation is composed of Augite & Felspar
Page 390
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⇑line 5 annotation 2
Page 392
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⇑line 8 annotation 7
Page 394
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line 1 annotation 9
line 15 annotation 3
Page 396
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line 13 annotation 7
Page 398
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line 5 annotation 9
⇑line 2 annotation 10
Page 399
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line 13 annotation 11
Page 402
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bottom-margin apparently unintentional mark
Page 405
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line 3 annotation an earthy greenstone
Page 410
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bottom-margin annotation (These rocks generally occur in the old Red Sandstone also in Mountain Limestone sometimes in still newer rocks)
Page 411
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line 17 annotation Tertiary Rocks
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Page 412
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⇑line 13 annotation also contains Pudding stone & Browne Coal
Page 413
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line 9 annotation ∗ The London Clay is of this formation
line 10 (    )
line 10 crossing-out "3"
line 10 annotation ∗ 2
bottom-margin annotation ∗ Iron Pyrites, Sulphate of Lime & Iron occurs in this mineral. also sometimes Amber & Browne clay also various seeds of tropical [continues on page 414] plants. also Crocodiles &c &c & Cocoa Nuts fishes..
⇑line 16 (    )
⇑line 16 at "4" annotation 3
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Page 414
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line 7 (    )
line 7 annotation 3 x
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line 19 (    )
line 19 annotation 4
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Page 415
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line 11 (    )
line 11 annotation 5
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lines 11—13 annotation of considerable importance in the arts; for making millstones
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⇑line 11 underline "fresh-water shells"
Page 417
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line 10 (    )
line 10 annotation 5
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Page 418
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⇑line 12 annotation X
bottom-margin annotation X The only Human Fossil Skeleton known was found in this rock
Page 420
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lines 3—12 annotation Beds of this mineral occur in the Meadows & Coates Crescent in Edinburgh
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⇑lines 10—9 annotation differs from Potters Clay in containing Sand
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Page 421
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line 19 annotation [drawing]
lines 24—25 score
lines 24—25 annotation now disputed
Page 423
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line 10 annotation ∗
bottom-margin annotation ∗ Occurs only the more Northern countries never being found in the Tropics
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Page 424
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line 15 at "lakes" annotation their variability being diminished
⇑line 6 (    )
⇑line 6 annotation 6
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Page 425
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⇑line 9 annotation swims on Water
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Page 426
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lines 18—23 annotation [drawing]
     a b c d
     the order of their position
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⇑line 10 annotation ∗
bottom-margin annotation ∗ has often been mistaken for red Pumice Stone
⇑line 4 annotation X
bottom-margin annotation X formed by the attrition of different minerals
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Page 428
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lines 4—5 annotation appears to have been sublimed
line 16 score [`bookmark']
Page 440
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bottom-margin annotation The lead mines in Flintshire Shropshire are situated chiefly in Mountain Limestone
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Page 444
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lines 16—17 annotation are mentioned by many of the older writers viz Herodotus observed them in Aegypt also Ovid remarks them.
Page 445
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lines 2—3 annotation Quadrumana none have yet been found—
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Page 446
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line 2 annotation X
bottom-margin annotation Bears are of rare occurrence in alluvial strata
Page 447
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⇑lines 11—9 annotation Another species has been found Europe simultaneous with the Elephant Tapir Rhinoceros
Page 452
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lines 1—5 annotation this is the animal that the Indians belief that the Gods destroyed to prevent the destruction of the Human race.
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bottom-margin annotation 6 distinguished from the Mammoth by tubercular teeth—
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Page 455
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top-margin annotation The Owl & Buzzard
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⇑line 12 annotation one, have been generally found in the tertiary formation of Paris
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Page 456
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line 7 annotation in the Isle of Sheppy
Page 458
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bottom-margin annotation The teeth of Sharks are found in great plenty in the Limestones of Malta
Page 460
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line 11 annotation X
bottom-margin annotation X ‹All› Nearly all insects which are found in this mineral are now extinct, except as some say the common Ant . —
lines 20—21 annotation Mr Witham has in his collection a specimen of Amber containing a small skeleton probably a reptile .—
⇑line 4 annotation In one collection in France there is 3560 specimens and nearly 5000 have been described.—
Page 461
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top-margin annotation All the Fossil shells are now extinct . —
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Page 466
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bottom-margin annotation Fossil organic remains are those included in any formation; sometimes, they are scarcely «altered but» generally a portion of the animal «matter» is extracted— often the whole substance is removed & merely a cast remains sometimes it percolated with some Fossil matter & then it is named petrified. —
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`List of Jameson's works, page [2]'; in pale pencil
lines 7—11 double score
bottom-margin annotation [drawing]
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`List of Jameson's works, page [3]'; bottom right torn away
much of page annotation in pale pencil [drawings]
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`List of Jameson's works, page [4]'; bottom left torn away; in pale pencil
much of page annotation [drawings]
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