Papers On the Geology of New Mexico
Papers On the Geology of New Mexico
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This we suppose to be the upper limit of the exposed cretaceous for the series follow- ing dipping to the south east is part of the Tertiary section given above.
The fault mentioned is that of the Isleta mesa monocline and may be traced for many miles north and south. A similar fault occurs about three miles west of San Ignatio. To the west of thjs the lower part of the series is visible and rises in the higher hills to the Punta de la Mesa sandstpne but to the east of it the lignitic series oc...cupies the entire area. The fauna of the sand above the lignite is abundantly illustrated beyond and seems to be closely allied to the Punta de la Mesa if not iden- tical with it. It is a marine fauna and of Fox Hills age. Thus our first impression and the prevailing opinion of geologists who have seen these lignites that they are Laramie is overthrown.
The leaves also, of which a large collection may be made, are not identifiable with familiar Laramie species. This same se- quence is detected east of the Sandia mountains but we are pre- pared to find this series followed by fresh- water or brackish Laramie at that place when sufficient exploration is possible.
What to read after Papers On the Geology of New Mexico?
You can find similar books in the "Read Also" column, or choose other free books by Clarence Luther Herrick, D. W. Johnson, Denison University to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
This we suppose to be the upper limit of the exposed cretaceous for the series follow- ing dipping to the south east is part of the Tertiary section given above.
The fault mentioned is that of the Isleta mesa monocline and may be traced for many miles north and south. A similar fault occurs about three miles west of San Ignatio. To the west of thjs the lower part of the series is visible and rises in the higher hills to the Punta de la Mesa sandstpne but to the east of it the lignitic series oc...cupies the entire area. The fauna of the sand above the lignite is abundantly illustrated beyond and seems to be closely allied to the Punta de la Mesa if not iden- tical with it. It is a marine fauna and of Fox Hills age. Thus our first impression and the prevailing opinion of geologists who have seen these lignites that they are Laramie is overthrown.
The leaves also, of which a large collection may be made, are not identifiable with familiar Laramie species. This same se- quence is detected east of the Sandia mountains but we are pre- pared to find this series followed by fresh- water or brackish Laramie at that place when sufficient exploration is possible.
What to read after Papers On the Geology of New Mexico?
You can find similar books in the "Read Also" column, or choose other free books by Clarence Luther Herrick, D. W. Johnson, Denison University to read onlineMoreLess
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