This specific monitoring location is about 650 m up the Abeja channel from the previous location. Here bedrock forces any streamflow to the surface. There is also a spring at this location from which water originates during relatively wetter periods
Sort of a mini canyon with outcrops of the parent bedrock rising on both sides of the channel.
Puertocito-Rock Outcrop Complex
Ephemeral flows during storm events. Underlying bedrock forces water to surface through here.
Juniper and Falugia lining wash. Juniper and creosote on hillslopes.