Temblor Formation

{{Short description|Geologic formation in California}}

{{Infobox rockunit

| name = Temblor Formation

| image =

| caption =

| type = Geologic formation

| age = Late Oligocene-Mid Miocene
~{{fossil range|28|11.6}}

| period = Miocene

| prilithology = Shale, sandstone

| otherlithology =

| namedfor = Temblor Ranch, McKittrick district, Kern County

| namedby = Anderson

| year_ts = 1905

| region = Western San Joaquin Valley,
Kern County, California

| country = United States

| coordinates =

| unitof =

| subunits = Agua Sandstone Member, Buttonbed Sandstone Member, Carneros Sandstone Member, Cymric Shale Member, Devilwater Siltstone, Gould Shale, Media Shale Member, Round Mountain Silt, Santos Shale Member, Wygal Sandstone Member

| underlies = Monterey Formation

| overlies =

| thickness =

| extent =

| area =

| map =

| map_caption =

}}

The Temblor Formation is a geologic formation in California. It preserves fossils dating back from the Late Oligocene to the Middle Miocene of the Neogene period. It is notable for the famous Sharktooth Hill deposit (otherwise known as Ernst Quarry).{{cite web |title=Vast Bed of Ancient Bones and Shark Teeth Explained |url=https://www.livescience.com/3656-vast-bed-ancient-bones-shark-teeth-explained.html |website=LiveScience |date=9 June 2009 |publisher=By Charles Q. Choi}}

Fossils

= Vertebrates =

== Cartilagenous fishes ==

=== Sharks ===

File:Isurus planus teeth.png

{{div col}}

{{div col end}}

=== Rays and skates ===

= Reptiles =

= Birds =

File:Hypohippus.jpg

File:Paleoparadoxia BW.jpg

= Mammals =

See also

{{Portal|California|Geology|Paleontology}}

References

{{reflist}}