- J C Coleman
J C Coleman - An eye sketch of the Falls of Niagara
AN EYE SKETCH of the FALLS of NIAGARA I.Weld del. Neele sculpt. London Published by J. Stockdale Piccadilly 16th. Novr. 1798. - An Old-fashioned Train of Cars
An Old-fashioned Train of Cars - View of the Horse-Shoe Fall of Niagara
VIEW of the HORSE-SHOE FALL of NIAGARA I.Weld del. Neele Scupt. Published by J. Stockdale Picadilly. - View of Bethlehem a Moravian settlement
VIEW of BETHLEHEM a Moravian settlement. I. Weld del. J. Dadley sculpt. Published Dec. 12 1798, by I. Stockdale, Picadilly. Bethlehem is the principal settlement, in North America, of the Moravians, or United Brethren. It is most agreeably situated on a rising ground, bounded on one side by the river Leheigh, which falls into the Delaware, and on the other by a creek, which has a very rapid current, and affords excellent seats for a great number of mills. The town is regularly laid out, and contains about eighty strong built stone dwelling houses and a large church. Three of the dwelling houses are very spacious buildings, and are appropriated respectively to the accommodation of the unmarried young men of the society, of the unmarried females, and of the widows. In these houses different manufactures are carried on, and the inmates of each are subject to a discipline approaching somewhat to that of a monastic institution. They eat together in a refectory; they sleep in dormitories; they attend morning and evening prayers in the chapel of the house; they work for a certain number of hours in the day; and they have stated intervals allotted to them for recreation. - View of the Falls of Niagara
View of the FALLS of Niagara J. Scott Published Dec.14 1798, by J. Stockdale - View of the Lesser Fall of Niagara
VIEW of the Lesser FALL of NIAGARA I.Weld del. J. Scott sculpt. Published Dec. 22, 1798, by J. Stockdale Picadilly. - Witsenia maura
Witsenia maura - Tulbaghia violacea
Tulbaghia violacea - Moraea iridioides
Moraea iridioides - Acokanthera spectabilis
Acokanthera spectabilis - Pachypodium succulentum
Pachypodium succulentum - Leucadendron Stokoei
Leucadendron Stokoei - Jesus with cross
- Protea abyssinica
Protea abyssinica - Part of a Telephone Exchange
- Aloe Globuligemma
Aloe Globuligemma - Stapelia Gettleffii
Stapelia Gettleffii - Bolusanthus speciosus
Bolusanthus speciosus - Senecio stapeliaeformis
Senecio stapeliaeformis - Gladiolus Rehmanni
Gladiolus Rehmanni - Orothamnus Zeyheri
Orothamnus Zeyheri - Leucadendron Stokoei
Leucadendron Stokoei - Cyrtanthus Angustifolius
- Cyrtanthus McKenii
Cyrtanthus McKenii - Arctotis Decurrens
Arctotis Decurrens - Ceropegia Meyeri
Ceropegia Meyeri - Richardia Rehmanni
Richardia Rehmanni - Streptocarpus Dunnii
Streptocarpus Dunnii - Aloe Pienaarii
Aloe Pienaarii - Freesia refracta
Freesia refracta - Clerodendron triphyllum
Clerodendron triphyllum - Nymphaea stellata
Nymphaea stellata - Sarcocaulon rigidum
Sarcocaulon rigidum - Ceropegia Rendallii
Ceropegia Rendallii - Polycheles baccata
- Gerbera Jamesoni
Gerbera Jamesoni - Cyrtanthus sanguineus
Cyrtanthus sanguineus - Crassula falcata
Cyrtanthus Angustifolius - Mimetes palustris
Mimetes palustris - Cyrtanthus rotundilobus
Cyrtanthus rotundilobus - Aloe pretoriensis
Aloe pretoriensis - Melanocetus Murrayi, 1,850–2,450 fathoms
- Richardia angustiloba
Richardia angustiloba - Haemanthus natalensis
Haemanthus natalensis - Agapanthus Umbellatus
Agapanthus Umbellatus - Cyrtanthus obliquus
Cyrtanthus obliquus - Clivia miniata
Clivia miniata - Bathynomus giganteus
- Tapping a Rubber Tree
- Bathyteuthis abyssicola
- Globigerina ooze
The Globigerina ooze is perhaps the best known of all the different deep-sea deposits. It was discovered and first described by the officers of the American Coast Survey in 1853. It is found in great abundance in the Atlantic Ocean in regions shallower than 2,200 fathoms. Deeper than this, it gradually merges into the ‘Red mud.’ It is mainly composed of the shells of Foraminifera, and of these the different species of Globigerina are the most abundant. It is probably formed partly by the shells of the dead Foraminifera that actually live on the bottom of the ocean and partly by the shells of those that live near the surface or in intermediate depths and fall to the bottom when their lives are done. So abundant are the shells of these Protozoa that nearly 95 per cent. of the Globigerina ooze is composed of carbonate of lime. The remaining five per cent. is composed of sulphate and phosphate of lime, carbonate of ammonia, the oxides of iron and manganese, and argillaceous matters. The oxides of iron and manganese are probably of meteoric origin; the argillaceous matter may be due to the trituration of lumps of pumice stone and to the deposits caused by dust storms. - Gardenia globosa
Gardenia globosa - Hypobythius calycodes
- Adenium multiflorum
Adenium multiflorum - The First Type of McCormick Reaper
- Saccopharynx ampullaceus
- Silhouettes of Grandfather and Grandmother
- Gladiolus psittacinus
Gladiolus psittacinus - Euphausia latifrons, from the surface of the sea