Don Elkins

Ra (Spirit)

James Allen McCarty

Carla Rueckert

Who are the ancient astronauts? Why did they first come to Earth? Why are they returning now? What part did they play in building the great monuments of antiquity? What part did they play in the formation of present and earlier civilizations? With what other beings do we share our universe? And where does the Earth fit into the cosmic scheme of things? Almost twenty years of experimental work with telepathy led to the "breakthrough" contact recorded in this book. The Ra Material is an account not only of the events leading up to this contact, but of over 200 pages of verbatim transcripts of each and every conversation!

An Ancient Astronaut Speaks

The Ra Material

Carla L. Rueckert

"I am Ra. We came to your peoples to enunciate the Law of One. We wished to impress upon those who wished to learn of unity that in unity all paradoxes are resolved; all that is broken is healed; all that is forgotten is brought to light." For thousands of years those of Ra have sought to teach the Law of One to seekers of truth on Earth who wished to learn of the unity or oneness of all things. This basic law of all creation is buried deep within each of our hearts because we really are one in love and in light, the building blocks of the universe. We are all manifestations of the One Infinite Creator. We are the Creator. We are not learning this law for the first time but are remembering it yet again as all mystics have taught throughout Earth's history. Our journey of self-realization is the discovery or remembrance of this essential truth, our essential identity. A waking up, as some have called it, within an illusion of separation. Don Elkins and Carla L. Rueckert worked together for 12 years to perfect the channeling process and receive philosophical inspiration and guidance from extraterrestrial sources. When Jim McCarty joined them in 1980 they began to receive a new and unique type of channeling contact from those of Ra. Through this contact, Ra shared information to help seekers of truth deepen their awareness and acceptance of self and other, and to help Earth move into the emerging fourth density of love and understanding. This book is the transcript from the recording of that conversation between the Questioner and Ra. Through questions & answers, the metaphysical blueprint of spiritual evolution is explored, from the microcosm to the macrocosm, from the particulars of life on this planet to the life of the cosmos, to the possibilities of healing, transformation, and self-realization for spiritual seekers and wanderers. * * * * * * * * * The Ra Contact: Teaching the Law of One Volume 1 contains Ra contact sessions 1-56. As with all L/L Research material, this book can be read for free in PDF form on L/L's archive website.

The Ra Contact: Teaching the Law of One:

Personal MaterialÐFragments Omitted from the First Four Books (Law of One)

The Law of One Book V

Eutrophication of surface waters not only impacts the environment but also water treatment processes, the most significant of which is from the effects of algae. During peak algal growth in many southern U.S. reservoirs, inflows that bring nutrients are at an annual minimum, and phosphorus released from bed-sediments is trapped in the hypolimnion. Littoral areas, described as the most productive zone of the lake, may be a possible source of phosphorus that fuels algal growth in the reservoir. I studied an isolated shallow cove in the War Eagle Creek arm of Beaver Lake in Northwest Arkansas to measure, quantify, and model the dynamics and transport of nutrients in littoral zones. A summary of the research problem, the statement of purpose, and associated hypothesis are provided in Chapter 1. Chapter 2 provides an overview of eutrophication as it relates to drinking water treatment, reservoirs, and zones within reservoirs. Also reviewed is the relationship of phosphorus (P) to reservoir eutrophication, internal loading as a source of P, and P cycling and transport within a reservoir. In Chapter 3, I present my study of sediment cores, temperature profiles, and dissolved oxygen (DO) profiles of the cove to determine the redox condition of the water overlying the bed-sediments and the associated sediment P release rates. Phosphorus release rates from bed-sediment incubations were as high as 2.02 mg m-2 d-1 under aerobic conditions and 4.05 mg m-2 d-1 under anaerobic. Variability in bottom DO concentrations of the littoral zone likely contribute to a cycling of aerobic and anaerobic conditions by changing the redox state at the sediment-water interface. When compared to whole-lake P release averages conducted for Beaver Lake, eutrophic coves were a disproportionate source of P within the reservoir, producing 6.5 times more P per unit area. Chapter 4 describes a study of how sediment P release and algal growth in littoral areas are connected. Sediment composition, equilibrium P concentration (EPCo), and aerobic P release rates were characterized for several sites within the cove. Core aerobic P release rates and EPCo both confirmed the release of P under aerobic conditions; however, it appears that algal demand sustained low dissolved P concentrations in the waters of the cove. This created a nutrient cycle where algae impose a nutrient gradient favoring the release of P by keeping concentrations of the waters overlying sediments below the EPCo. Chapter 5 describes a model developed to simulate thermoconvective flow and transport mechanisms between littoral and pelagic zones. Diurnal fluctuation in flow for surface and bottom waters indicated water moves in and out of the cove on a daily timestep. Overall, the general direction of flow was in along the bottom of the cove, and out along the top. The model and in situ P concentrations revealed that P is transported from bottom waters as they enter the cove to surface waters as they leave the cove. This process applied to all littoral areas of the reservoir would result in a major P transport mechanism to surface waters in late summer. Chapter 6 provides a synthesis of the three studies. Unique processes of the littoral zone make it a disproportionate source of P within a reservoir. P loads brought into the littoral zone along the bottom and P released out of littoral sediments are then available for transport out of the surface of the littoral zone. This P would then be available to be used by algae and replenish P losses in the epilimnion which occur through sedimentation. Our model and sampling indicate that late summer blooms of algae in Beaver Lake are likely fueled in part by P transport out of the littoral zone. The fundamental contribution of this research is the recognition of littoral areas as a significant source of internal P loading to fuel algal growth in reservoirs.

A Study of a Eutrophic Littoral Cove on Beaver Lake in Northwest Arkansas

The Release, Transport, and Utilization of Phosphorus from Bed-sediments

In Book Two of The Law of One, the nature of each of the densities or dimensions of this octave of creation is explored in detail with special emphasis given to how evolution for our third density to the fourth density is accomplished. The relationship between the densities of creation and the energy centers of the body is investigated so that each experience can be used as catalyst for growth to balance and crystallize the energy centers of chakras of the student of evolution. Wanderers, sexual energy transfers, the physics of Dewey B. Larson, Polarization in consciousness, ritual magic, and the nature and function of the Higher Self are all explored as they are related to the Law of One. Book Two contains Sessions #27 through #50.

James Allen McCarty

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